<?xml version="1.0" encoding="UTF-8"?><!DOCTYPE article  PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd"><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" dtd-version="3.0" xml:lang="en" article-type="research article"><front><journal-meta><journal-id journal-id-type="publisher-id">OJS</journal-id><journal-title-group><journal-title>Open Journal of Statistics</journal-title></journal-title-group><issn pub-type="epub">2161-718X</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/ojs.2016.66091</article-id><article-id pub-id-type="publisher-id">OJS-72899</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Physics&amp;Mathematics</subject></subj-group></article-categories><title-group><article-title>
 
 
  Comparison of Two Time Series Decomposition Methods: Least Squares and Buys-Ballot Methods
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>I.</surname><given-names>S. Iwueze</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>E.</surname><given-names>C. Nwogu</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>V.</surname><given-names>U. Nlebedim</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>J.</surname><given-names>C. Imoh</given-names></name><xref ref-type="aff" rid="aff2"><sup>2</sup></xref></contrib></contrib-group><aff id="aff2"><addr-line>Dept of Maths/Statistics, Imo State Polytechnic, Umuagwo, Nigeria</addr-line></aff><aff id="aff1"><addr-line>Department of Statistics, Federal University of Technology, Owerri, Nigeria</addr-line></aff><pub-date pub-type="epub"><day>14</day><month>11</month><year>2016</year></pub-date><volume>06</volume><issue>06</issue><fpage>1123</fpage><lpage>1137</lpage><history><date date-type="received"><day>August</day>	<month>20,</month>	<year>2016</year></date><date date-type="rev-recd"><day>Accepted:</day>	<month>December</month>	<year>18,</year>	</date><date date-type="accepted"><day>December</day>	<month>21,</month>	<year>2016</year></date></history><permissions><copyright-statement>&#169; Copyright  2014 by authors and Scientific Research Publishing Inc. </copyright-statement><copyright-year>2014</copyright-year><license><license-p>This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/</license-p></license></permissions><abstract><p>
 
 
  This paper discusses comparison of two time series decomposition methods: The Least Squares Estimation (LSE) and Buys-Ballot Estimation (BBE) methods. As noted by Iwueze and Nwogu (2014), there exists a research gap for the choice of appropriate model for decomposition and detection of presence of seasonal effect in a series model. Estimates of trend parameters and seasonal indices are all that are needed to fill the research gap. However, these estimates are obtainable through the Least Squares Estimation (LSE) and Buys-Ballot Estimation (BBE) methods. Hence, there is need to compare estimates of the two methods and recommend. The comparison of the two methods is done using the Accuracy Measures (Mean Error (ME)), Mean Square Error (MSE), the Mean Absolute Error (MAE), and the Mean Absolute Percentage Error (MAPE). The results from simulated series show that for the additive model; the summary statistics (ME, MSE and MAE) for the two estimation methods and for all the selected trending curves are equal in all the simulations both in magnitude and direction. For the multiplicative model, results show that when a series is dominated by trend, the estimates of the parameters by both methods become less precise and differ more widely from each other. However, if conditions for successful transformation (using the logarithmic transform in linearizing the multiplicative model to additive model) are met, both of them give similar results.
 
</p></abstract><kwd-group><kwd>Decomposition Models</kwd><kwd> Least Squares Estimates</kwd><kwd> Buys-Ballot Estimates</kwd><kwd> Accuracy  Measures</kwd><kwd> Successful Transformation</kwd><kwd> Trending Curves</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>The two major goals of time series analysis are 1) identification of the nature of the phenomenon represented by the sequence of observations and 2) forecasting (predicting future values of the time series variable). Identification of the pattern and choice of model in time series data is critical to facilitate forecasting. Thus, these two goals of time series analysis require that the pattern of observed time series data is identified and described. Two patterns that may be present are trend and seasonality.</p><p>The trend represents a general systematic linear or (most often) nonlinear component that changes over time and does not repeat or at least does not repeat within the time range captured by data. As long as the trend is monotonous (consistently increasing or decreasing) the identification of trend component is not very difficult. Trend analysis (methods for estimating the trend parameters) can be done by three important methods; 1) smoothing [<xref ref-type="bibr" rid="scirp.72899-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.72899-ref2">2</xref>] [<xref ref-type="bibr" rid="scirp.72899-ref3">3</xref>] [<xref ref-type="bibr" rid="scirp.72899-ref4">4</xref>] [<xref ref-type="bibr" rid="scirp.72899-ref5">5</xref>] 2) fitting a mathematical function [<xref ref-type="bibr" rid="scirp.72899-ref6">6</xref>] [<xref ref-type="bibr" rid="scirp.72899-ref7">7</xref>] and 3) differencing to make the series stationary in the ARIMA methodology [<xref ref-type="bibr" rid="scirp.72899-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.72899-ref8">8</xref>] [<xref ref-type="bibr" rid="scirp.72899-ref9">9</xref>] . Tests for trend are given in Kendall and Ord [<xref ref-type="bibr" rid="scirp.72899-ref7">7</xref>] . Correlation analysis can also be used to assess trend. If a time series contains a trend, then the values of the autocorrelations will not come to zero except for very large values of the lag [<xref ref-type="bibr" rid="scirp.72899-ref6">6</xref>] .</p><p>Many time series exhibit a variation which repeats itself in systematic intervals over time and this behaviour is known as seasonal dependency (seasonality). By seasonality, we mean periodic fluctuations. It is formally defined as correlational dependency of order k between each ith element of the series and the (i − k)th element [<xref ref-type="bibr" rid="scirp.72899-ref10">10</xref>] and measured by autocorrelation (a correlation between <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x2.png" xlink:type="simple"/></inline-formula> and<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x3.png" xlink:type="simple"/></inline-formula>); k is usually called the lag. Seasonality can be visually identified in the series as a pattern that repeats every k elements. The following graphical techniques can be used to detect seasonality: 1) A run sequence plot [<xref ref-type="bibr" rid="scirp.72899-ref11">11</xref>] , 2) A seasonal sub-series plot [<xref ref-type="bibr" rid="scirp.72899-ref12">12</xref>] , 3) Multiple box plots [<xref ref-type="bibr" rid="scirp.72899-ref11">11</xref>] and 4) the autocorrelation plot [<xref ref-type="bibr" rid="scirp.72899-ref1">1</xref>] . Both the seasonal sub-series plot and the box plot assume that the seasonal periods are known. In most cases, the seasonal periods are easy to find (4 for quarterly data, 12 for monthly data etc). If there is significant seasonality, the autocorrelation plot should show spikes at multiples of lags equal to the period, the seasonal lag (for quarterly data, we would expect to see significant spikes at lag 4, 8, 12, 16, and so on). Davey and Flores [<xref ref-type="bibr" rid="scirp.72899-ref13">13</xref>] proposed a method which adds statistical tests of seasonal indexes for the multiplicative model that helps identify seasonality with greater confidence. Tests for seasonality are also given in Kendall and Ord [<xref ref-type="bibr" rid="scirp.72899-ref7">7</xref>] .</p><p>In time series analysis, it is assumed that the data consist of a systematic pattern and random noise (error). The systematic pattern consists of the: trend (denoted as<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x4.png" xlink:type="simple"/></inline-formula>), seasonal (denoted as<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x5.png" xlink:type="simple"/></inline-formula>) and cyclical (denoted as<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x6.png" xlink:type="simple"/></inline-formula>) components. The random noise is the error or irregular component (denoted as <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x7.png" xlink:type="simple"/></inline-formula> or<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x8.png" xlink:type="simple"/></inline-formula>), where t stands for the particular point in time. These four classes of time series components may or may not coexist in real-life data.</p><p>In addition to identifying the patterns (the components), the main two goals of a time series analysis are better achieved if and only if the correct model is used. The specific functional relationship between these components can assume different forms. However, the possibilities are that they combine in an additive (additive seasonality) or a multiplicative (multiplicative seasonality) fashion, but can also take other forms such as pseudo-additive/mixed (combining the elements of both the additive and multiplicative models).</p><p>Additive model (when trend, seasonal and cyclical components are additively combined):</p><disp-formula id="scirp.72899-formula52"><label>(1.1)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/13-1240560x9.png"  xlink:type="simple"/></disp-formula><p>Multiplicative model (when trend, seasonal and cyclical components are multiplicatively combined):</p><disp-formula id="scirp.72899-formula53"><label>(1.2)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/13-1240560x10.png"  xlink:type="simple"/></disp-formula><p>Pseudo-Additive/Mixed Model: (combining the elements of both the additive and multiplicative models):</p><disp-formula id="scirp.72899-formula54"><label>(1.3)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/13-1240560x11.png"  xlink:type="simple"/></disp-formula><p>Cyclical variation refers to the long term oscillation or swings about the trend and only long period sets of data will show cyclical fluctuation of any appreciable magnitude. If short period of time are involved (which is true of all examples of this study), the cyclical component is superimposed into the trend [<xref ref-type="bibr" rid="scirp.72899-ref6">6</xref>] and we obtain a trend-cycle component denoted by M<sub>t</sub>. In this case Equations (1.1), (1.2) and (1.3) may be written as:</p><disp-formula id="scirp.72899-formula55"><label>(1.4)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/13-1240560x12.png"  xlink:type="simple"/></disp-formula><disp-formula id="scirp.72899-formula56"><label>(1.5)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/13-1240560x13.png"  xlink:type="simple"/></disp-formula><p>and</p><disp-formula id="scirp.72899-formula57"><label>(1.6)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/13-1240560x14.png"  xlink:type="simple"/></disp-formula><p>where <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x15.png" xlink:type="simple"/></inline-formula> is the trend-cycle component; <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x16.png" xlink:type="simple"/></inline-formula>is the seasonal component with the property that<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x17.png" xlink:type="simple"/></inline-formula>, and <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x18.png" xlink:type="simple"/></inline-formula> is the irregular or random component. For the additive model (1.1), it is assumed that the irregular/error component <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x19.png" xlink:type="simple"/></inline-formula> is the Gaussian <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x19.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x20.png" xlink:type="simple"/></inline-formula> white noise, while for the multiplicative model (1.2), <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x19.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x20.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x21.png" xlink:type="simple"/></inline-formula>is the Gaussian <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x19.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x20.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x21.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x22.png" xlink:type="simple"/></inline-formula> white noise. For the additive model (1.1), the assumption is</p><p>that the sum of the seasonal component over a complete period is zero<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x23.png" xlink:type="simple"/></inline-formula>,</p><p>while for the multiplicative model (1.2), the sum of the seasonal component over a</p><p>complete period is<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x24.png" xlink:type="simple"/></inline-formula>.</p><p>The multiplicative model (1.5) can be linearized to become the additive model (1.4).</p><disp-formula id="scirp.72899-formula58"><label>(1.7)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/13-1240560x25.png"  xlink:type="simple"/></disp-formula><p>where<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x26.png" xlink:type="simple"/></inline-formula>. It follows that we can study the additive model (1.1) and apply the results obtain to the multiplicative model after linearization. The pseudo-additive model is used when the original time series contains very small or zero values. For this reason, this work will discuss only the additive and multiplicative models.</p><p>As far as the traditional method of decomposition is concerned (to be referred to as the Least Squares Estimation (LSE) Method), the first step will usually be to estimate and eliminate <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x27.png" xlink:type="simple"/></inline-formula> for each time period from the actual data either by subtraction for Equation (1.4) or division for Equation (1.5). The de-trended series is obtained as <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x27.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x28.png" xlink:type="simple"/></inline-formula> for Equation (1.4) or <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x27.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x28.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x29.png" xlink:type="simple"/></inline-formula> for Equation (1.5). In the second step, the seasonal effect is obtained by estimating the average of the de-trended series at each season. The de-trended, de-seasonalized series is obtained as <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x27.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x28.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x29.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x30.png" xlink:type="simple"/></inline-formula> for Equation (1.4) or <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x27.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x28.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x29.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x30.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x31.png" xlink:type="simple"/></inline-formula> for Equation (1.5). This gives the residual or irregular component. Having fitted a model to a time series, one often wants to see if the residuals are purely random. For detailed discussion of residual analysis, see [<xref ref-type="bibr" rid="scirp.72899-ref1">1</xref>] [<xref ref-type="bibr" rid="scirp.72899-ref14">14</xref>] .</p><p>This LSE as describe above is known to be associated with computational difficulties and does not give an insight for choice of models for time series decomposition and detection of presence of seasonal effect in a series.</p><p>However, by arranging a series of length n into m rows <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x32.png" xlink:type="simple"/></inline-formula> and s columns<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x32.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x33.png" xlink:type="simple"/></inline-formula>, Iwueze et al. [<xref ref-type="bibr" rid="scirp.72899-ref15">15</xref>] showed that the row and column averages and variances can be used to 1) determine the need for and appropriate transformation 2) choose the appropriate model for decomposition, 3) detect the presence of seasonal effect in the series and 4) obtain estimates of the trend parameters and seasonal indices of the entire series. In particular, for a seasonal series, the rows represent the periods/years while the columns are the seasons. This two-dimensional arrangement of a series is referred to as Buys-Ballot table, see [<xref ref-type="bibr" rid="scirp.72899-ref16">16</xref>] [<xref ref-type="bibr" rid="scirp.72899-ref17">17</xref>] .</p><p>Using the periodic means<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x34.png" xlink:type="simple"/></inline-formula>, Iwueze and Nwogu [<xref ref-type="bibr" rid="scirp.72899-ref17">17</xref>] constructed two derived variables, the Chain Base Estimation (CBE) and the Fixed Base Estimation (FBE)-derived variables, on bases of which they derived the estimates of linear trend-cycle parameters. Iwueze and Ohakwe [<xref ref-type="bibr" rid="scirp.72899-ref18">18</xref>] derived the estimates of quadratic trend-cycle parameters from the corresponding CBE and the FBE-derived variables, while Iwueze and Nwogu [<xref ref-type="bibr" rid="scirp.72899-ref19">19</xref>] derived the estimates of the exponential trend-cycle parameters from the corresponding CBE and the FBE-derived variables.</p><p>Iwueze and Nwogu [<xref ref-type="bibr" rid="scirp.72899-ref20">20</xref>] have shown that, for seasonal time series data and for all trending curves, the row, column and overall averages and variances of the Buys-Ballot table are 1) functions of the trend parameters and 2) different for the additive and multiplicative models. Therefore, the row, column and overall averages and variances can be used for i) choice of appropriate model, ii) detection of presence of seasonal effect in a series in addition to estimation of trend parameters and seasonal indices. Since estimates of the trend parameters and seasonal indices can also be derived from the Least Squares method, there is the need to compare the two decomposition methods.</p><p>Therefore, the ultimate objective of this study is to compare the estimates of trend parameters and seasonal indices from the Buys Ballot method with the results from the conventional least squares method. The specific objectives are to: 1) Review the Buys Ballot method for estimation of trend parameters and seasonal indices for some selected trending curves, 2) obtain estimates of the trend parameters and seasonal indices using simulated examples, 3) compare the estimates of the trend parameters and seasonal indices from the Buys Ballot method with estimates from the traditional method (LSE) using simulated examples. Based on the results, recommendations are made.</p></sec><sec id="s2"><title>2. Methodology</title><p>The comparison of Least Squares Estimates and Buys-Ballot Estimates in this study is done using measures often referred to in the literature as Forecasting Accuracy Measures. These include the Mean Error (ME), Mean Square Error (MSE), the Mean Absolute Error (MAE), and the Mean Absolute Percentage Error (MAPE).</p><p>Given the actual values of the parameters <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x35.png" xlink:type="simple"/></inline-formula> these accuracy measures may be defined in terms of the deviations of the parameter estimates from the corresponding actual values used in the simulations. Thus, if <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x35.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x36.png" xlink:type="simple"/></inline-formula> is the estimate of the parameter<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x35.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x36.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x37.png" xlink:type="simple"/></inline-formula>, then <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x35.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x36.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x37.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x38.png" xlink:type="simple"/></inline-formula> is the error made in estimating<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x35.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x36.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x37.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x38.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x39.png" xlink:type="simple"/></inline-formula>. In terms of<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x35.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x36.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x37.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x38.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x39.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x40.png" xlink:type="simple"/></inline-formula>, the accuracy measures adapted from the forecasting Accuracy Measures are</p><disp-formula id="scirp.72899-formula59"><label>(2.1)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/13-1240560x41.png"  xlink:type="simple"/></disp-formula><disp-formula id="scirp.72899-formula60"><label>(2.2)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/13-1240560x42.png"  xlink:type="simple"/></disp-formula><disp-formula id="scirp.72899-formula61"><label>(2.3)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/13-1240560x43.png"  xlink:type="simple"/></disp-formula><disp-formula id="scirp.72899-formula62"><label>(2.4)</label><graphic position="anchor" xlink:href="http://html.scirp.org/file/13-1240560x44.png"  xlink:type="simple"/></disp-formula><p>In these definitions, the comparison of parameter estimates is done directly using the actual and estimated values of the parameters.</p><p>The summary of the estimates of trend parameters and seasonal indices obtained by Iwueze and Nwogu [<xref ref-type="bibr" rid="scirp.72899-ref20">20</xref>] are given in <xref ref-type="table" rid="table1">Table 1</xref> for Linear, <xref ref-type="table" rid="table2">Table 2</xref> for Quadratic and <xref ref-type="table" rid="table3">Table 3</xref> Exponential trend-cycle component for the additive and multiplicative models.</p><p>We note the following for Tables 1-3:</p><p>1)<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x45.png" xlink:type="simple"/></inline-formula>, <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x45.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x46.png" xlink:type="simple"/></inline-formula>and <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x45.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x46.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x47.png" xlink:type="simple"/></inline-formula> are estimates derived from the regression equations of row averages on row number.</p><p>2) Additive and Multiplicative models give different estimates.</p><p>3) <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x48.png" xlink:type="simple"/></inline-formula></p><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> Estimates of parameters of Linear trend-cycle components and seasonal indices</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >Parameter</th><th align="center" valign="middle"  colspan="2"  >Model</th></tr></thead><tr><td align="center" valign="middle" >Additive model</td><td align="center" valign="middle" >Multiplicative model</td></tr><tr><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x49.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x50.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x51.png" xlink:type="simple"/></inline-formula></td></tr><tr><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x52.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x53.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x54.png" xlink:type="simple"/></inline-formula></td></tr><tr><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x55.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x56.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x57.png" xlink:type="simple"/></inline-formula></td></tr></tbody></table></table-wrap><p>Source: Iwueze and Nwogu [<xref ref-type="bibr" rid="scirp.72899-ref20">20</xref>] .</p><table-wrap id="table2" ><label><xref ref-type="table" rid="table2">Table 2</xref></label><caption><title> Estimates of parameters of quadratic trend-cycle component and seasonal indices</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >Parameter</th><th align="center" valign="middle"  colspan="2"  >Model</th></tr></thead><tr><td align="center" valign="middle" >Additive model</td><td align="center" valign="middle" >Multiplicative model</td></tr><tr><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x58.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x59.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x60.png" xlink:type="simple"/></inline-formula></td></tr><tr><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x61.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x62.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x63.png" xlink:type="simple"/></inline-formula></td></tr><tr><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x64.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x65.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x66.png" xlink:type="simple"/></inline-formula></td></tr><tr><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x67.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x68.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x69.png" xlink:type="simple"/></inline-formula></td></tr><tr><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x70.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x71.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x72.png" xlink:type="simple"/></inline-formula></td></tr></tbody></table></table-wrap><p>Source: Iwueze and Nwogu [<xref ref-type="bibr" rid="scirp.72899-ref20">20</xref>] .</p><table-wrap id="table3" ><label><xref ref-type="table" rid="table3">Table 3</xref></label><caption><title> Estimates of parameters of exponential trend-cycle component and seasonal indices</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >Parameter</th><th align="center" valign="middle"  colspan="2"  >Model</th></tr></thead><tr><td align="center" valign="middle" >Additive model</td><td align="center" valign="middle" >Multiplicative model</td></tr><tr><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x73.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x74.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x75.png" xlink:type="simple"/></inline-formula></td></tr><tr><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x76.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x77.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x78.png" xlink:type="simple"/></inline-formula></td></tr><tr><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x79.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x80.png" xlink:type="simple"/></inline-formula></td><td align="center" valign="middle" ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x81.png" xlink:type="simple"/></inline-formula></td></tr></tbody></table></table-wrap><p>Source: Iwueze and Nwogu [<xref ref-type="bibr" rid="scirp.72899-ref20">20</xref>] .</p></sec><sec id="s3"><title>3. Simulation Examples</title><p>This Section presents some simulations examples used to compare the estimates of the parameters of the selected trend curves and seasonal indices using Buys-Ballot method with those based on the conventional Least Squares Estimation method. For the linear trend-cycle, the simulated examples consist of 106 series of 120 observations each simulated from <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x82.png" xlink:type="simple"/></inline-formula> with <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x82.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x83.png" xlink:type="simple"/></inline-formula> and 2.0 and</p><p><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x84.png" xlink:type="simple"/></inline-formula>for the additive model, <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x84.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x85.png" xlink:type="simple"/></inline-formula>, with</p><p><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x86.png" xlink:type="simple"/></inline-formula>and <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x86.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x87.png" xlink:type="simple"/></inline-formula> for the multiplicative model. These values of a, b and c were arbitrarily chosen for simulation purposes. The values of</p><p><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x88.png" xlink:type="simple"/></inline-formula>for the simulated additive and the multiplicative models are given in <xref ref-type="table" rid="table4">Table 4</xref>.</p><p>The Buys-Ballot estimates of trend parameters and seasonal indices are computed using the expressions in <xref ref-type="table" rid="table1">Table 1</xref>. The estimates of the error means and standard deviations are computed from the residuals from the fitted models. The deviations of these estimates from the parameters used in the simulations are given in Appendix A for the Additive model and Appendix B for the Multiplicative model, while the summary statistics for 20 simulations only are given in <xref ref-type="table" rid="table5">Table 5</xref> for the Additive model and Tables 6-8 for the Multiplicative model.</p><table-wrap id="table4" ><label><xref ref-type="table" rid="table4">Table 4</xref></label><caption><title> Seasonal <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x89.png" xlink:type="simple"/></inline-formula> indices used in the simulation of series from additive and multiplicative models</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x90.png" xlink:type="simple"/></inline-formula></th><th align="center" valign="middle"  colspan="2"  ><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x91.png" xlink:type="simple"/></inline-formula></th></tr></thead><tr><td align="center" valign="middle" >Additive</td><td align="center" valign="middle" >Multiplicative</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.89</td><td align="center" valign="middle" >0.91</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >−1.22</td><td align="center" valign="middle" >0.88</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >1.00</td></tr><tr><td align="center" valign="middle" >4</td><td align="center" valign="middle" >−0.15</td><td align="center" valign="middle" >0.98</td></tr><tr><td align="center" valign="middle" >5</td><td align="center" valign="middle" >−0.09</td><td align="center" valign="middle" >0.98</td></tr><tr><td align="center" valign="middle" >6</td><td align="center" valign="middle" >1.16</td><td align="center" valign="middle" >1.12</td></tr><tr><td align="center" valign="middle" >7</td><td align="center" valign="middle" >2.34</td><td align="center" valign="middle" >1.26</td></tr><tr><td align="center" valign="middle" >8</td><td align="center" valign="middle" >1.95</td><td align="center" valign="middle" >1.20</td></tr><tr><td align="center" valign="middle" >9</td><td align="center" valign="middle" >0.64</td><td align="center" valign="middle" >1.05</td></tr><tr><td align="center" valign="middle" >10</td><td align="center" valign="middle" >−0.73</td><td align="center" valign="middle" >0.92</td></tr><tr><td align="center" valign="middle" >11</td><td align="center" valign="middle" >−2.14</td><td align="center" valign="middle" >0.80</td></tr><tr><td align="center" valign="middle" >12</td><td align="center" valign="middle" >−0.97</td><td align="center" valign="middle" >0.90</td></tr></tbody></table></table-wrap><table-wrap id="table5" ><label><xref ref-type="table" rid="table5">Table 5</xref></label><caption><title> Summary statistics for additive model (a = 1 and b = 2)</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >Series</th><th align="center" valign="middle"  colspan="2"  >ME</th><th align="center" valign="middle"  colspan="2"  >MAE</th><th align="center" valign="middle"  colspan="2"  >MSE</th></tr></thead><tr><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.009</td><td align="center" valign="middle" >−0.009</td><td align="center" valign="middle" >0.221</td><td align="center" valign="middle" >0.219</td><td align="center" valign="middle" >0.074</td><td align="center" valign="middle" >0.076</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.001</td><td align="center" valign="middle" >0.156</td><td align="center" valign="middle" >0.160</td><td align="center" valign="middle" >0.038</td><td align="center" valign="middle" >0.041</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >0.003</td><td align="center" valign="middle" >0.002</td><td align="center" valign="middle" >0.226</td><td align="center" valign="middle" >0.228</td><td align="center" valign="middle" >0.080</td><td align="center" valign="middle" >0.085</td></tr><tr><td align="center" valign="middle" >4</td><td align="center" valign="middle" >−0.003</td><td align="center" valign="middle" >−0.002</td><td align="center" valign="middle" >0.213</td><td align="center" valign="middle" >0.221</td><td align="center" valign="middle" >0.074</td><td align="center" valign="middle" >0.078</td></tr><tr><td align="center" valign="middle" >5</td><td align="center" valign="middle" >0.002</td><td align="center" valign="middle" >0.004</td><td align="center" valign="middle" >0.157</td><td align="center" valign="middle" >0.159</td><td align="center" valign="middle" >0.062</td><td align="center" valign="middle" >0.065</td></tr><tr><td align="center" valign="middle" >6</td><td align="center" valign="middle" >0.016</td><td align="center" valign="middle" >0.017</td><td align="center" valign="middle" >0.200</td><td align="center" valign="middle" >0.199</td><td align="center" valign="middle" >0.071</td><td align="center" valign="middle" >0.069</td></tr><tr><td align="center" valign="middle" >7</td><td align="center" valign="middle" >−0.003</td><td align="center" valign="middle" >−0.002</td><td align="center" valign="middle" >0.207</td><td align="center" valign="middle" >0.214</td><td align="center" valign="middle" >0.073</td><td align="center" valign="middle" >0.078</td></tr><tr><td align="center" valign="middle" >8</td><td align="center" valign="middle" >0.026</td><td align="center" valign="middle" >0.027</td><td align="center" valign="middle" >0.192</td><td align="center" valign="middle" >0.191</td><td align="center" valign="middle" >0.072</td><td align="center" valign="middle" >0.069</td></tr><tr><td align="center" valign="middle" >9</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.003</td><td align="center" valign="middle" >0.180</td><td align="center" valign="middle" >0.173</td><td align="center" valign="middle" >0.076</td><td align="center" valign="middle" >0.075</td></tr><tr><td align="center" valign="middle" >10</td><td align="center" valign="middle" >0.024</td><td align="center" valign="middle" >0.025</td><td align="center" valign="middle" >0.252</td><td align="center" valign="middle" >0.256</td><td align="center" valign="middle" >0.097</td><td align="center" valign="middle" >0.101</td></tr><tr><td align="center" valign="middle" >11</td><td align="center" valign="middle" >0.004</td><td align="center" valign="middle" >0.004</td><td align="center" valign="middle" >0.167</td><td align="center" valign="middle" >0.170</td><td align="center" valign="middle" >0.048</td><td align="center" valign="middle" >0.049</td></tr><tr><td align="center" valign="middle" >12</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >−0.002</td><td align="center" valign="middle" >0.224</td><td align="center" valign="middle" >0.235</td><td align="center" valign="middle" >0.131</td><td align="center" valign="middle" >0.128</td></tr><tr><td align="center" valign="middle" >13</td><td align="center" valign="middle" >0.015</td><td align="center" valign="middle" >0.015</td><td align="center" valign="middle" >0.220</td><td align="center" valign="middle" >0.226</td><td align="center" valign="middle" >0.077</td><td align="center" valign="middle" >0.078</td></tr><tr><td align="center" valign="middle" >14</td><td align="center" valign="middle" >−0.011</td><td align="center" valign="middle" >−0.010</td><td align="center" valign="middle" >0.230</td><td align="center" valign="middle" >0.232</td><td align="center" valign="middle" >0.093</td><td align="center" valign="middle" >0.094</td></tr><tr><td align="center" valign="middle" >15</td><td align="center" valign="middle" >0.019</td><td align="center" valign="middle" >0.020</td><td align="center" valign="middle" >0.215</td><td align="center" valign="middle" >0.226</td><td align="center" valign="middle" >0.083</td><td align="center" valign="middle" >0.092</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >0.010</td><td align="center" valign="middle" >0.011</td><td align="center" valign="middle" >0.167</td><td align="center" valign="middle" >0.172</td><td align="center" valign="middle" >0.057</td><td align="center" valign="middle" >0.060</td></tr><tr><td align="center" valign="middle" >17</td><td align="center" valign="middle" >0.003</td><td align="center" valign="middle" >0.004</td><td align="center" valign="middle" >0.143</td><td align="center" valign="middle" >0.152</td><td align="center" valign="middle" >0.041</td><td align="center" valign="middle" >0.044</td></tr><tr><td align="center" valign="middle" >18</td><td align="center" valign="middle" >0.015</td><td align="center" valign="middle" >0.015</td><td align="center" valign="middle" >0.274</td><td align="center" valign="middle" >0.275</td><td align="center" valign="middle" >0.146</td><td align="center" valign="middle" >0.148</td></tr><tr><td align="center" valign="middle" >19</td><td align="center" valign="middle" >0.002</td><td align="center" valign="middle" >0.003</td><td align="center" valign="middle" >0.203</td><td align="center" valign="middle" >0.203</td><td align="center" valign="middle" >0.070</td><td align="center" valign="middle" >0.067</td></tr><tr><td align="center" valign="middle" >20</td><td align="center" valign="middle" >0.006</td><td align="center" valign="middle" >0.006</td><td align="center" valign="middle" >0.222</td><td align="center" valign="middle" >0.228</td><td align="center" valign="middle" >0.082</td><td align="center" valign="middle" >0.085</td></tr></tbody></table></table-wrap><table-wrap id="table6" ><label><xref ref-type="table" rid="table6">Table 6</xref></label><caption><title> Summary statistics for multiplicative model (a = 1 and b = 0.02)</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >S/N</th><th align="center" valign="middle"  colspan="2"  >ME</th><th align="center" valign="middle"  colspan="2"  >MAE</th><th align="center" valign="middle"  colspan="2"  >MAPE</th><th align="center" valign="middle"  colspan="2"  >MSE</th><th align="center" valign="middle"  colspan="2"  >RSME</th></tr></thead><tr><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >−0.001</td><td align="center" valign="middle" >−0.001</td><td align="center" valign="middle" >0.005</td><td align="center" valign="middle" >0.012</td><td align="center" valign="middle" >0.840</td><td align="center" valign="middle" >2.834</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.006</td><td align="center" valign="middle" >0.016</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.003</td><td align="center" valign="middle" >0.013</td><td align="center" valign="middle" >0.470</td><td align="center" valign="middle" >3.271</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.004</td><td align="center" valign="middle" >0.018</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.005</td><td align="center" valign="middle" >0.014</td><td align="center" valign="middle" >0.799</td><td align="center" valign="middle" >3.368</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.006</td><td align="center" valign="middle" >0.018</td></tr><tr><td align="center" valign="middle" >4</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >−0.001</td><td align="center" valign="middle" >0.004</td><td align="center" valign="middle" >0.015</td><td align="center" valign="middle" >0.798</td><td align="center" valign="middle" >4.924</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.001</td><td align="center" valign="middle" >0.006</td><td align="center" valign="middle" >0.023</td></tr><tr><td align="center" valign="middle" >5</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.003</td><td align="center" valign="middle" >0.011</td><td align="center" valign="middle" >0.578</td><td align="center" valign="middle" >2.873</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.005</td><td align="center" valign="middle" >0.014</td></tr><tr><td align="center" valign="middle" >6</td><td align="center" valign="middle" >0.001</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.004</td><td align="center" valign="middle" >0.014</td><td align="center" valign="middle" >0.766</td><td align="center" valign="middle" >4.834</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.006</td><td align="center" valign="middle" >0.021</td></tr><tr><td align="center" valign="middle" >7</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >−0.001</td><td align="center" valign="middle" >0.004</td><td align="center" valign="middle" >0.013</td><td align="center" valign="middle" >0.773</td><td align="center" valign="middle" >4.223</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.006</td><td align="center" valign="middle" >0.017</td></tr><tr><td align="center" valign="middle" >8</td><td align="center" valign="middle" >0.001</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.004</td><td align="center" valign="middle" >0.012</td><td align="center" valign="middle" >0.883</td><td align="center" valign="middle" >3.054</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.006</td><td align="center" valign="middle" >0.016</td></tr><tr><td align="center" valign="middle" >9</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.004</td><td align="center" valign="middle" >0.010</td><td align="center" valign="middle" >0.713</td><td align="center" valign="middle" >2.069</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.005</td><td align="center" valign="middle" >0.014</td></tr><tr><td align="center" valign="middle" >10</td><td align="center" valign="middle" >0.001</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.006</td><td align="center" valign="middle" >0.013</td><td align="center" valign="middle" >1.055</td><td align="center" valign="middle" >4.062</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.007</td><td align="center" valign="middle" >0.017</td></tr><tr><td align="center" valign="middle" >11</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >−0.001</td><td align="center" valign="middle" >0.004</td><td align="center" valign="middle" >0.018</td><td align="center" valign="middle" >0.554</td><td align="center" valign="middle" >6.065</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.001</td><td align="center" valign="middle" >0.005</td><td align="center" valign="middle" >0.023</td></tr><tr><td align="center" valign="middle" >12</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >−0.001</td><td align="center" valign="middle" >0.005</td><td align="center" valign="middle" >0.012</td><td align="center" valign="middle" >1.065</td><td align="center" valign="middle" >3.591</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.008</td><td align="center" valign="middle" >0.019</td></tr><tr><td align="center" valign="middle" >13</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.004</td><td align="center" valign="middle" >0.014</td><td align="center" valign="middle" >0.837</td><td align="center" valign="middle" >3.310</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.006</td><td align="center" valign="middle" >0.017</td></tr><tr><td align="center" valign="middle" >14</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >−0.001</td><td align="center" valign="middle" >0.005</td><td align="center" valign="middle" >0.010</td><td align="center" valign="middle" >0.989</td><td align="center" valign="middle" >2.517</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.006</td><td align="center" valign="middle" >0.015</td></tr><tr><td align="center" valign="middle" >15</td><td align="center" valign="middle" >0.001</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.004</td><td align="center" valign="middle" >0.009</td><td align="center" valign="middle" >0.893</td><td align="center" valign="middle" >2.073</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.006</td><td align="center" valign="middle" >0.013</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.003</td><td align="center" valign="middle" >0.014</td><td align="center" valign="middle" >0.577</td><td align="center" valign="middle" >3.555</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.005</td><td align="center" valign="middle" >0.018</td></tr><tr><td align="center" valign="middle" >17</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >−0.001</td><td align="center" valign="middle" >0.003</td><td align="center" valign="middle" >0.015</td><td align="center" valign="middle" >0.442</td><td align="center" valign="middle" >4.974</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.001</td><td align="center" valign="middle" >0.004</td><td align="center" valign="middle" >0.023</td></tr><tr><td align="center" valign="middle" >18</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.006</td><td align="center" valign="middle" >0.008</td><td align="center" valign="middle" >1.215</td><td align="center" valign="middle" >1.468</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.008</td><td align="center" valign="middle" >0.012</td></tr><tr><td align="center" valign="middle" >19</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.004</td><td align="center" valign="middle" >0.013</td><td align="center" valign="middle" >0.743</td><td align="center" valign="middle" >3.077</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.006</td><td align="center" valign="middle" >0.018</td></tr><tr><td align="center" valign="middle" >20</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >−0.001</td><td align="center" valign="middle" >0.005</td><td align="center" valign="middle" >0.018</td><td align="center" valign="middle" >0.809</td><td align="center" valign="middle" >4.686</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.001</td><td align="center" valign="middle" >0.000</td><td align="center" valign="middle" >0.024</td></tr></tbody></table></table-wrap><table-wrap id="table7" ><label><xref ref-type="table" rid="table7">Table 7</xref></label><caption><title> Summary statistics for multiplicative model (a = 1 and b = 0.2)</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >Series</th><th align="center" valign="middle"  colspan="2"  >ME</th><th align="center" valign="middle"  colspan="2"  >MAE</th><th align="center" valign="middle"  colspan="2"  >MSE</th><th align="center" valign="middle"  colspan="2"  >MAPE</th><th align="center" valign="middle"  colspan="2"  >RMSE</th></tr></thead><tr><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >13.107</td><td align="center" valign="middle" >13.097</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.004</td><td align="center" valign="middle" >13.302</td><td align="center" valign="middle" >13.315</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.002</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >13.292</td><td align="center" valign="middle" >13.304</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.002</td></tr><tr><td align="center" valign="middle" >4</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >13.238</td><td align="center" valign="middle" >13.218</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td></tr><tr><td align="center" valign="middle" >5</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >13.278</td><td align="center" valign="middle" >13.281</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td></tr><tr><td align="center" valign="middle" >6</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.005</td><td align="center" valign="middle" >1.007</td><td align="center" valign="middle" >13.420</td><td align="center" valign="middle" >13.454</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.004</td></tr><tr><td align="center" valign="middle" >7</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >13.171</td><td align="center" valign="middle" >13.143</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >0.998</td></tr><tr><td align="center" valign="middle" >8</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >13.342</td><td align="center" valign="middle" >13.338</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td></tr><tr><td align="center" valign="middle" >9</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >13.234</td><td align="center" valign="middle" >13.232</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td></tr><tr><td align="center" valign="middle" >10</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.005</td><td align="center" valign="middle" >1.005</td><td align="center" valign="middle" >13.423</td><td align="center" valign="middle" >13.440</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.002</td></tr><tr><td align="center" valign="middle" >11</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.004</td><td align="center" valign="middle" >13.333</td><td align="center" valign="middle" >13.364</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.002</td></tr><tr><td align="center" valign="middle" >12</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.997</td><td align="center" valign="middle" >0.997</td><td align="center" valign="middle" >13.169</td><td align="center" valign="middle" >13.166</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td></tr><tr><td align="center" valign="middle" >13</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >13.280</td><td align="center" valign="middle" >13.280</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td></tr><tr><td align="center" valign="middle" >14</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >13.166</td><td align="center" valign="middle" >13.183</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >1.000</td></tr><tr><td align="center" valign="middle" >15</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >13.374</td><td align="center" valign="middle" >13.379</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >13.225</td><td align="center" valign="middle" >13.226</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >0.999</td></tr><tr><td align="center" valign="middle" >17</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >13.251</td><td align="center" valign="middle" >13.257</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td></tr><tr><td align="center" valign="middle" >18</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >13.346</td><td align="center" valign="middle" >13.340</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td></tr><tr><td align="center" valign="middle" >19</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.997</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >13.170</td><td align="center" valign="middle" >13.148</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >0.998</td></tr><tr><td align="center" valign="middle" >20</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >13.296</td><td align="center" valign="middle" >13.304</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.001</td></tr></tbody></table></table-wrap><table-wrap id="table8" ><label><xref ref-type="table" rid="table8">Table 8</xref></label><caption><title> Summary statistics for multiplicative model (a = 1 and b = 2.0)</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >Series</th><th align="center" valign="middle"  colspan="2"  >ME</th><th align="center" valign="middle"  colspan="2"  >MAE</th><th align="center" valign="middle"  colspan="2"  >MSE</th><th align="center" valign="middle"  colspan="2"  >MAPE</th><th align="center" valign="middle"  colspan="2"  >RMSE</th></tr></thead><tr><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.995</td><td align="center" valign="middle" >0.995</td><td align="center" valign="middle" >0.995</td><td align="center" valign="middle" >0.995</td><td align="center" valign="middle" >0.991</td><td align="center" valign="middle" >0.991</td><td align="center" valign="middle" >1.948</td><td align="center" valign="middle" >1.942</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >0.996</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.004</td><td align="center" valign="middle" >1.005</td><td align="center" valign="middle" >2.062</td><td align="center" valign="middle" >2.065</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.003</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.004</td><td align="center" valign="middle" >2.056</td><td align="center" valign="middle" >2.057</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.002</td></tr><tr><td align="center" valign="middle" >4</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >2.025</td><td align="center" valign="middle" >2.021</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td></tr><tr><td align="center" valign="middle" >5</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.004</td><td align="center" valign="middle" >2.051</td><td align="center" valign="middle" >2.051</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.002</td></tr><tr><td align="center" valign="middle" >6</td><td align="center" valign="middle" >1.005</td><td align="center" valign="middle" >1.006</td><td align="center" valign="middle" >1.005</td><td align="center" valign="middle" >1.006</td><td align="center" valign="middle" >1.012</td><td align="center" valign="middle" >1.014</td><td align="center" valign="middle" >2.147</td><td align="center" valign="middle" >2.159</td><td align="center" valign="middle" >1.006</td><td align="center" valign="middle" >1.007</td></tr><tr><td align="center" valign="middle" >7</td><td align="center" valign="middle" >0.997</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >0.997</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >0.995</td><td align="center" valign="middle" >0.993</td><td align="center" valign="middle" >1.984</td><td align="center" valign="middle" >1.978</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.997</td></tr><tr><td align="center" valign="middle" >8</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >2.093</td><td align="center" valign="middle" >2.095</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.001</td></tr><tr><td align="center" valign="middle" >9</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >2.022</td><td align="center" valign="middle" >2.020</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td></tr><tr><td align="center" valign="middle" >10</td><td align="center" valign="middle" >1.005</td><td align="center" valign="middle" >1.006</td><td align="center" valign="middle" >1.005</td><td align="center" valign="middle" >1.006</td><td align="center" valign="middle" >1.012</td><td align="center" valign="middle" >1.013</td><td align="center" valign="middle" >2.155</td><td align="center" valign="middle" >2.168</td><td align="center" valign="middle" >1.006</td><td align="center" valign="middle" >1.006</td></tr><tr><td align="center" valign="middle" >11</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.006</td><td align="center" valign="middle" >1.006</td><td align="center" valign="middle" >2.083</td><td align="center" valign="middle" >2.095</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.003</td></tr><tr><td align="center" valign="middle" >12</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >0.993</td><td align="center" valign="middle" >0.993</td><td align="center" valign="middle" >1.979</td><td align="center" valign="middle" >1.977</td><td align="center" valign="middle" >0.997</td><td align="center" valign="middle" >0.996</td></tr><tr><td align="center" valign="middle" >13</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >2.047</td><td align="center" valign="middle" >2.044</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >1.000</td></tr><tr><td align="center" valign="middle" >14</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >0.997</td><td align="center" valign="middle" >1.984</td><td align="center" valign="middle" >1.985</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.999</td></tr><tr><td align="center" valign="middle" >15</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.007</td><td align="center" valign="middle" >1.007</td><td align="center" valign="middle" >2.114</td><td align="center" valign="middle" >2.119</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.004</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >0.997</td><td align="center" valign="middle" >2.015</td><td align="center" valign="middle" >2.014</td><td align="center" valign="middle" >0.998</td><td align="center" valign="middle" >0.998</td></tr><tr><td align="center" valign="middle" >17</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >0.999</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >2.031</td><td align="center" valign="middle" >2.032</td><td align="center" valign="middle" >1.000</td><td align="center" valign="middle" >1.000</td></tr><tr><td align="center" valign="middle" >18</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.006</td><td align="center" valign="middle" >1.006</td><td align="center" valign="middle" >2.093</td><td align="center" valign="middle" >2.097</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >1.003</td></tr><tr><td align="center" valign="middle" >19</td><td align="center" valign="middle" >0.997</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >0.997</td><td align="center" valign="middle" >0.996</td><td align="center" valign="middle" >0.994</td><td align="center" valign="middle" >0.993</td><td align="center" valign="middle" >1.981</td><td align="center" valign="middle" >1.975</td><td align="center" valign="middle" >0.997</td><td align="center" valign="middle" >0.996</td></tr><tr><td align="center" valign="middle" >20</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.002</td><td align="center" valign="middle" >1.003</td><td align="center" valign="middle" >2.056</td><td align="center" valign="middle" >2.058</td><td align="center" valign="middle" >1.001</td><td align="center" valign="middle" >1.001</td></tr></tbody></table></table-wrap><p>For the additive model the results are the same for the selected values of the slope parameter<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x92.png" xlink:type="simple"/></inline-formula>. Therefore, the summary statistics for b = 2 only is shown in <xref ref-type="table" rid="table5">Table 5</xref>. As <xref ref-type="table" rid="table5">Table 5</xref> shows, the summary statistics (ME, MSE and MAE) for the two estimation methods (LSE and BBE) are equal both in magnitude and direction all the simulations. This indicates that the two methods are equally effective in estimating the trend parameters and seasonal indices when the model for decomposition is additive.</p><p>For the multiplicative model, <xref ref-type="table" rid="table6">Table 6</xref> shows that for b = 0.02, the values of the summary statistics (ME, RMSE, MSE, MAE and MAPE) are equal in almost all the simulations as in the additive model. However, for values of b = 0.2 and 2.0, <xref ref-type="table" rid="table7">Table 7</xref> and <xref ref-type="table" rid="table8">Table 8</xref> show that the values of the summary statistics (ME, RMSE, MSE, MAE and MAPE) are unequal in most all the simulations and the difference increased as the value of b increased from 0.2 to 2.0. In other words, when a series is dominated by trend, not only do the estimates of the parameters by both methods become less precise; estimates of the parameters from the two methods differ more widely from each other.</p><p>It could be recalled that logarithm transformation can be used to transform the multiplicative model to become the additive model. In order to preserve the linearity of the trend, Iwueze and Akpanta [<xref ref-type="bibr" rid="scirp.72899-ref21">21</xref>] have shown that the trend parameters (a and b) satisfy the condition;<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x93.png" xlink:type="simple"/></inline-formula>. Therefore, this lack of agreement between estimates from the two methods and the actual values when b = 0.2 and 2.0 may be attributable to the violation of the condition for successful transformation (linearization in this case). For b = 0.2 and a = 1, <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x93.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x94.png" xlink:type="simple"/></inline-formula>and for b = 2.0 and a = 1,<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x93.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x94.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x95.png" xlink:type="simple"/></inline-formula>.</p><p>For the Quadratic trend-cycle component, the empirical examples also consist of 106 series of 120 observations each simulated from<inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x96.png" xlink:type="simple"/></inline-formula>, with</p><p><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x97.png" xlink:type="simple"/></inline-formula>and <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x97.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x98.png" xlink:type="simple"/></inline-formula> and <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x97.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x98.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x99.png" xlink:type="simple"/></inline-formula> given in <xref ref-type="table" rid="table4">Table 4</xref> for the additive model only. However, for want of space, the summary statistics for 20 simulations only are given in <xref ref-type="table" rid="table9">Table 9</xref>. As <xref ref-type="table" rid="table9">Table 9</xref> shows, the summary statistics (ME, MSE and MAE) for the two estimation methods (LSE and BBE) are equal in almost all the simulations. This indicates that the two methods are equally effective in estimating the trend parameters and seasonal indices when the model for decomposition is additive.</p><p>For the Exponential trend-cycle component, the empirical examples also consist of 106 series of 120 observations each simulated from <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x100.png" xlink:type="simple"/></inline-formula> with <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x100.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x101.png" xlink:type="simple"/></inline-formula> and <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x100.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x101.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x102.png" xlink:type="simple"/></inline-formula> and <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x100.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x101.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x102.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x103.png" xlink:type="simple"/></inline-formula> and <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x100.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x101.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x102.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x103.png" xlink:type="simple"/></inline-formula><inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x104.png" xlink:type="simple"/></inline-formula> given in <xref ref-type="table" rid="table4">Table 4</xref> for the additive model only. The summary statistics for 20 simulations given in <xref ref-type="table" rid="table1">Table 1</xref>0 shows that the summary statistics (ME, MSE and MAE) for the two estimation methods (LSE and BBE) are equal in almost all the simulations. This indicates that the two methods are equally effective in estimating the trend parameters and seasonal indices when the model for decomposition is additive.</p><table-wrap id="table9" ><label><xref ref-type="table" rid="table9">Table 9</xref></label><caption><title> Summary statistics for additive quadratic model (a = 1, b = 2 and c = 3)</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >S/No</th><th align="center" valign="middle"  colspan="2"  >ME</th><th align="center" valign="middle"  colspan="2"  >MAE</th><th align="center" valign="middle"  colspan="2"  >MAPE</th><th align="center" valign="middle"  colspan="2"  >MSE</th><th align="center" valign="middle"  colspan="2"  >RMSE</th></tr></thead><tr><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.15</td><td align="center" valign="middle" >−0.11</td><td align="center" valign="middle" >0.88</td><td align="center" valign="middle" >0.99</td><td align="center" valign="middle" >0.94</td><td align="center" valign="middle" >1.00</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.06</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.93</td><td align="center" valign="middle" >0.99</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >1.00</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.07</td><td align="center" valign="middle" >−0.09</td><td align="center" valign="middle" >0.88</td><td align="center" valign="middle" >0.99</td><td align="center" valign="middle" >0.94</td><td align="center" valign="middle" >1.00</td></tr><tr><td align="center" valign="middle" >4</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.12</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.87</td><td align="center" valign="middle" >0.94</td><td align="center" valign="middle" >0.93</td><td align="center" valign="middle" >0.97</td></tr><tr><td align="center" valign="middle" >5</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.90</td><td align="center" valign="middle" >0.97</td><td align="center" valign="middle" >0.95</td><td align="center" valign="middle" >0.98</td></tr><tr><td align="center" valign="middle" >6</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.34</td><td align="center" valign="middle" >−0.16</td><td align="center" valign="middle" >0.99</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >0.99</td><td align="center" valign="middle" >0.98</td></tr><tr><td align="center" valign="middle" >7</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.89</td><td align="center" valign="middle" >0.98</td><td align="center" valign="middle" >0.94</td><td align="center" valign="middle" >0.99</td></tr><tr><td align="center" valign="middle" >8</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.86</td><td align="center" valign="middle" >0.89</td><td align="center" valign="middle" >0.93</td><td align="center" valign="middle" >0.94</td></tr><tr><td align="center" valign="middle" >9</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.19</td><td align="center" valign="middle" >0.15</td><td align="center" valign="middle" >0.89</td><td align="center" valign="middle" >0.93</td><td align="center" valign="middle" >0.94</td><td align="center" valign="middle" >0.97</td></tr><tr><td align="center" valign="middle" >10</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.01</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.83</td><td align="center" valign="middle" >0.90</td><td align="center" valign="middle" >0.91</td><td align="center" valign="middle" >0.95</td></tr><tr><td align="center" valign="middle" >11</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.13</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.91</td><td align="center" valign="middle" >0.94</td><td align="center" valign="middle" >0.95</td><td align="center" valign="middle" >0.97</td></tr><tr><td align="center" valign="middle" >12</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.82</td><td align="center" valign="middle" >0.89</td><td align="center" valign="middle" >0.90</td><td align="center" valign="middle" >0.94</td></tr><tr><td align="center" valign="middle" >13</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >0.88</td><td align="center" valign="middle" >0.95</td><td align="center" valign="middle" >0.94</td><td align="center" valign="middle" >0.97</td></tr><tr><td align="center" valign="middle" >14</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.15</td><td align="center" valign="middle" >0.85</td><td align="center" valign="middle" >0.91</td><td align="center" valign="middle" >0.92</td><td align="center" valign="middle" >0.96</td></tr><tr><td align="center" valign="middle" >15</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.15</td><td align="center" valign="middle" >0.20</td><td align="center" valign="middle" >0.86</td><td align="center" valign="middle" >0.92</td><td align="center" valign="middle" >0.93</td><td align="center" valign="middle" >0.96</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.13</td><td align="center" valign="middle" >0.14</td><td align="center" valign="middle" >0.90</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >0.95</td><td align="center" valign="middle" >0.98</td></tr><tr><td align="center" valign="middle" >17</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.94</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >0.97</td><td align="center" valign="middle" >0.98</td></tr><tr><td align="center" valign="middle" >18</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.14</td><td align="center" valign="middle" >−0.08</td><td align="center" valign="middle" >0.78</td><td align="center" valign="middle" >0.86</td><td align="center" valign="middle" >0.88</td><td align="center" valign="middle" >0.93</td></tr><tr><td align="center" valign="middle" >19</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.22</td><td align="center" valign="middle" >−0.15</td><td align="center" valign="middle" >0.89</td><td align="center" valign="middle" >1.02</td><td align="center" valign="middle" >0.95</td><td align="center" valign="middle" >1.01</td></tr><tr><td align="center" valign="middle" >20</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.04</td><td align="center" valign="middle" >0.88</td><td align="center" valign="middle" >0.95</td><td align="center" valign="middle" >0.94</td><td align="center" valign="middle" >0.97</td></tr></tbody></table></table-wrap><table-wrap id="table10" ><label><xref ref-type="table" rid="table1">Table 1</xref>0</label><caption><title> Summary statistics for additive exponential model (b = 10 and c = 0.02)</title></caption><table><tbody><thead><tr><th align="center" valign="middle"  rowspan="2"  >S/No</th><th align="center" valign="middle"  colspan="2"  >ME</th><th align="center" valign="middle"  colspan="2"  >MAE</th><th align="center" valign="middle"  colspan="2"  >MAPE</th><th align="center" valign="middle"  colspan="2"  >MSE</th><th align="center" valign="middle"  colspan="2"  >RMSE</th></tr></thead><tr><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td><td align="center" valign="middle" >LSE</td><td align="center" valign="middle" >BBE</td></tr><tr><td align="center" valign="middle" >1</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.09</td><td align="center" valign="middle" >0.09</td><td align="center" valign="middle" >0.89</td><td align="center" valign="middle" >0.89</td><td align="center" valign="middle" >0.94</td><td align="center" valign="middle" >0.94</td></tr><tr><td align="center" valign="middle" >2</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >0.98</td><td align="center" valign="middle" >0.98</td></tr><tr><td align="center" valign="middle" >3</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.09</td><td align="center" valign="middle" >0.09</td><td align="center" valign="middle" >0.89</td><td align="center" valign="middle" >0.89</td><td align="center" valign="middle" >0.94</td><td align="center" valign="middle" >0.94</td></tr><tr><td align="center" valign="middle" >4</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.95</td><td align="center" valign="middle" >0.95</td><td align="center" valign="middle" >0.98</td><td align="center" valign="middle" >0.98</td></tr><tr><td align="center" valign="middle" >5</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.92</td><td align="center" valign="middle" >0.92</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >0.96</td></tr><tr><td align="center" valign="middle" >6</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.88</td><td align="center" valign="middle" >0.88</td><td align="center" valign="middle" >0.94</td><td align="center" valign="middle" >0.94</td></tr><tr><td align="center" valign="middle" >7</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.09</td><td align="center" valign="middle" >0.09</td><td align="center" valign="middle" >0.90</td><td align="center" valign="middle" >0.90</td><td align="center" valign="middle" >0.95</td><td align="center" valign="middle" >0.95</td></tr><tr><td align="center" valign="middle" >8</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >−0.03</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >1.00</td><td align="center" valign="middle" >1.00</td><td align="center" valign="middle" >1.00</td><td align="center" valign="middle" >1.00</td></tr><tr><td align="center" valign="middle" >9</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.90</td><td align="center" valign="middle" >0.90</td><td align="center" valign="middle" >0.95</td><td align="center" valign="middle" >0.95</td></tr><tr><td align="center" valign="middle" >10</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >0.83</td><td align="center" valign="middle" >0.83</td><td align="center" valign="middle" >0.91</td><td align="center" valign="middle" >0.91</td></tr><tr><td align="center" valign="middle" >11</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >0.93</td><td align="center" valign="middle" >0.93</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >0.96</td></tr><tr><td align="center" valign="middle" >12</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.20</td><td align="center" valign="middle" >0.20</td><td align="center" valign="middle" >0.83</td><td align="center" valign="middle" >0.83</td><td align="center" valign="middle" >0.91</td><td align="center" valign="middle" >0.91</td></tr><tr><td align="center" valign="middle" >13</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.05</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.98</td><td align="center" valign="middle" >0.98</td><td align="center" valign="middle" >0.99</td><td align="center" valign="middle" >0.99</td></tr><tr><td align="center" valign="middle" >14</td><td align="center" valign="middle" >0.08</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >0.08</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.91</td><td align="center" valign="middle" >0.91</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >0.96</td></tr><tr><td align="center" valign="middle" >15</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.03</td><td align="center" valign="middle" >0.08</td><td align="center" valign="middle" >0.08</td><td align="center" valign="middle" >0.87</td><td align="center" valign="middle" >0.87</td><td align="center" valign="middle" >0.93</td><td align="center" valign="middle" >0.93</td></tr><tr><td align="center" valign="middle" >16</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >−0.02</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >0.01</td><td align="center" valign="middle" >1.03</td><td align="center" valign="middle" >1.03</td><td align="center" valign="middle" >1.01</td><td align="center" valign="middle" >1.01</td></tr><tr><td align="center" valign="middle" >17</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.04</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.94</td><td align="center" valign="middle" >0.95</td><td align="center" valign="middle" >0.97</td><td align="center" valign="middle" >0.97</td></tr><tr><td align="center" valign="middle" >18</td><td align="center" valign="middle" >−0.63</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >−0.63</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >−2.88</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >2.77</td><td align="center" valign="middle" >0.79</td><td align="center" valign="middle" >1.66</td><td align="center" valign="middle" >0.89</td></tr><tr><td align="center" valign="middle" >19</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.02</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.07</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >0.96</td><td align="center" valign="middle" >0.98</td><td align="center" valign="middle" >0.98</td></tr><tr><td align="center" valign="middle" >20</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.14</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >0.14</td><td align="center" valign="middle" >0.15</td><td align="center" valign="middle" >0.47</td><td align="center" valign="middle" >0.88</td><td align="center" valign="middle" >0.90</td><td align="center" valign="middle" >0.94</td><td align="center" valign="middle" >0.95</td></tr></tbody></table></table-wrap></sec><sec id="s4"><title>4. Summary, Recommendation and Conclusion</title><p>This study has compared the estimates of trend parameters and seasonal indices from the Buys Ballot method with the results from the Least Squares Estimation (LSE) method for the linear, quadratic and exponential trending curves. The rationale for this study is to assess the performance of the Buys Ballot Estimation (BBE) method in relation to the Least Squares Estimation (LSE) method.</p><p>The comparison of Least Squares Estimates and Buys-Ballot Estimates in this study is done using Accuracy Measures (the Mean Error (ME), Mean Square Error (MSE), the Mean Absolute Error (MAE), and the Mean Absolute Percentage Error (MAPE)). These Accuracy Measures are defined, for each estimation procedure, in terms of the deviations of the parameter estimates (using simulated series) from the corresponding actual values used in the simulations.</p><p>The results of the analyses show that, for the additive model the summary statistics (ME, MSE and MAE) are equal both in magnitude and direction all the simulations for the two estimation methods (LSE and BBE) and all the selected trending curves. This indicates that the two estimation methods are equally effective in estimating the trend parameters and seasonal indices when the model for decomposition is additive.</p><p>For the multiplicative model (shown for linear trend only), results of the analyses show that when the slope b = 0.02, the values of the summary statistics (ME, RMSE, MSE, MAE and MAPE) are equal in all the simulations as in the additive model. However, as the value of b increased from 0.02 to 2.0 the results show that the values of the summary statistics (ME, RMSE, MSE, MAE and MAPE) are unequal in all the simulations and the difference increases with an increase in b. In other words, when a series is dominated by the trend, the estimates of the parameters by both methods become less precise and differ more widely from each other. This has been attributed to the violation of the condition for successful transformation (linearization in this case). It could be recalled that logarithm transformation of the multiplicative model to the additive model can preserve the linearity of a linear trend only if the trend parameters (a and b) satisfy the condition; <inline-formula><inline-graphic xlink:href="http://html.scirp.org/file/13-1240560x105.png" xlink:type="simple"/></inline-formula> [<xref ref-type="bibr" rid="scirp.72899-ref21">21</xref>] ).</p><p>Therefore, when the model is additive, the estimates of trend parameters and seasonal indices are the same for both estimation procedures. However, because of the insight it gives into choice of model and detection of presence of seasonal effect, the BBE is recommended.</p></sec><sec id="s5"><title>Cite this paper</title><p>Iwueze, I.S., Nwogu, E.C., Nlebedim, V.U. and Imoh, J.C. (2016) Comparison of Two Time Series Decomposition Methods: Least Squares and Buys-Ballot Methods. Open Journal of Statistics, 6, 1123-1137. http://dx.doi.org/10.4236/ojs.2016.66091</p></sec><sec id="s6"><title>Appendix A</title><p>Deviations of the Buys-Ballot and Least Squares estimates of the linear trend parameters and seasonal indices from the Parameter values (for Additive model with a = 1and b= 2.0).</p></sec><sec id="s7"><title>Appendix B</title><p>Deviations of the Buys-Ballot and Least Squares estimates of the linear trend parameters and seasonal indices from the Parameter values (Multiplicative Model and b = 0.02).</p><disp-formula id="scirp.72899-formula63"><graphic  xlink:href="http://html.scirp.org/file/13-1240560x138.png"  xlink:type="simple"/></disp-formula><p>Submit or recommend next manuscript to SCIRP and we will provide best service for you:</p><p>Accepting pre-submission inquiries through Email, Facebook, LinkedIn, Twitter, etc.</p><p>A wide selection of journals (inclusive of 9 subjects, more than 200 journals)</p><p>Providing 24-hour high-quality service</p><p>User-friendly online submission system</p><p>Fair and swift peer-review system</p><p>Efficient typesetting and proofreading procedure</p><p>Display of the result of downloads and visits, as well as the number of cited articles</p><p>Maximum dissemination of your research work</p><p>Submit your manuscript at: http://papersubmission.scirp.org/</p><p>Or contact ojs@scirp.org</p></sec></body><back><ref-list><title>References</title><ref id="scirp.72899-ref1"><label>1</label><mixed-citation publication-type="other" xlink:type="simple">Iwueze, I.S. and Akpanta, A.C. 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