# Moving Averages and Exponential Smoothing

Applied Business Forecasting and Planning MOVING AVERAGES AND EXPONENTIAL SMOOTHING Introduction This chapter introduces models applicable to time series data with seasonal, trend, or both seasonal and trend component and stationary data. Forecasting methods discussed in this chapter can be classified as: Averaging methods. Equally weighted observations Exponential Smoothing methods. Unequal set of weights to past data, where the weights decay exponentially from the most recent to the most distant data points. All methods in this group require that certain parameters to be defined. These parameters (with values between 0 and 1) will determine the unequal weights to be applied to past data. Introduction Averaging methods

If a time series is generated by a constant process subject to random error, then mean is a useful statistic and can be used as a forecast for the next period. Averaging methods are suitable for stationary time series data where the series is in equilibrium around a constant value ( the underlying mean) with a constant variance over time. Introduction Exponential smoothing methods The simplest exponential smoothing method is the single smoothing (SES) method where only one parameter needs to be estimated Holts method makes use of two different parameters and allows forecasting for series with trend. Holt-Winters method involves three smoothing parameters to smooth the data, the trend, and the seasonal index. Averaging Methods The Mean Uses the average of all the historical data as the forecast 1 t Ft 1 yi t i 1

When new data becomes available , the forecast for time t+2 is the new mean including the previously observed data plus this new observation. Ft 2 1 t 1 yi t 1 i 1 This method is appropriate when there is no noticeable trend or seasonality. Averaging Methods The moving average for time period t is the mean of the k most recent observations. The constant number k is specified at the outset. The smaller the number k, the more weight is given to recent periods. The greater the number k, the less weight is given to more recent periods. Moving Averages

A large k is desirable when there are wide, infrequent fluctuations in the series. A small k is most desirable when there are sudden shifts in the level of series. For quarterly data, a four-quarter moving average, MA(4), eliminates or averages out seasonal effects. Moving Averages For monthly data, a 12-month moving average, MA(12), eliminate or averages out seasonal effect. Equal weights are assigned to each observation used in the average. Each new data point is included in the average as it becomes available, and the oldest data point is discarded. Moving Averages A moving average of order k, MA(k) is the value of k consecutive observations. Ft 1 y t 1 ( yt yt 1 yt 2 yt k 1 ) K 1 t Ft 1 yi k i t k 1

K is the number of terms in the moving average. The moving average model does not handle trend or seasonality very well although it can do better than the total mean. Example: Weekly Department Store Sales The weekly sales figures (in millions of dollars) presented in the following table are used by a major department store to determine the need for temporary sales personnel. Period (t) 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17

18 19 20 21 22 23 24 25 Sales (y) 5.3 4.4 5.4 5.8 5.6 4.8 5.6 5.6 5.4 6.5 5.1 5.8 5 6.2 5.6 6.7 5.2 5.5 5.8 5.1 5.8 6.7 5.2 6 5.8 Example: Weekly Department Store Sales Weekly Sales 8 7

6 Sales 5 4 Sales (y) 3 2 1 0 0 5 10 15 Weeks 20 25 30 Example: Weekly Department Store Sales Use a three-week moving average (k=3) for the department store sales to forecast for the week 24 and 26. y 24

( y23 y22 y21 ) 5.2 6.7 5.8 5.9 3 3 The forecast error is e24 y24 y 24 6 5.9 .1 Example: Weekly Department Store Sales The forecast for the week 26 is y 26 y25 y24 y23 5.8 6 5.2 5.7 3 3 Example: Weekly Department Store Sales RMSE = 0.63 Weekly Sales Forecasts 8 7 6 Sales 5 Sales (y)

4 forecast 3 2 1 0 0 5 10 15 Weeks 20 25 30 Period (t) 1 2 3 4 5 6 7 8 9 10 11 12 13 14

15 16 17 18 19 20 21 22 23 24 25 Sales (y) forecast 5.3 4.4 5.4 5.8 5.033333 5.6 5.2 4.8 5.6 5.6 5.4 5.6 5.333333 5.4 5.333333 6.5 5.533333 5.1 5.833333 5.8 5.666667 5 5.8 6.2 5.3 5.6 5.666667 6.7

5.6 5.2 6.166667 5.5 5.833333 5.8 5.8 5.1 5.5 5.8 5.466667 6.7 5.566667 5.2 5.866667 6 5.9 5.8 5.966667 5.666667 Exponential Smoothing Methods This method provides an exponentially weighted moving average of all previously observed values. Appropriate for data with no predictable upward or downward trend. The aim is to estimate the current level and use it as a forecast of future value. Simple Exponential Smoothing Method Formally, the exponential smoothing equation is Ft 1 yt (1 ) Ft

= smoothing constant. yt = observed value of series in period t. Ft = old forecast for period t. The forecast Ft+1 is based on weighting the most recent observation yt with a weight and weighting the most recent forecast Ft with a weight of 1- Ft 1 forecast for the next period. Simple Exponential Smoothing Method The implication of exponential smoothing can be better seen if the previous equation is expanded by replacing Ft with its components as follows: Ft 1 yt (1 ) Ft yt (1 )[ yt 1 (1 ) Ft 1 ] yt (1 ) y t 1 (1 ) 2 Ft 1 Simple Exponential Smoothing Method If this substitution process is repeated by replacing Ft-1 by its components, Ft-2 by its components, and so on the result is: Ft 1 yt (1 ) y t 1 (1 ) 2 y t 2 (1 )3 y t 3 (1 )t 1 y1 Therefore, Ft+1 is the weighted moving average of all past observations.

Simple Exponential Smoothing Method The following table shows the weights assigned to past observations for = 0.2, 0.4, 0.6, 0.8, 0.9 Weight assigned to Yt Yt-1 0.2 0.2 0.4 0.4 0.6 0.6 Yt-2 0.2(1-0.2) 0.2(1-0.2)2 0.4(1-0.4) 0.4(1-0.4)2 0.6(1-0.6) 0.6(1-0.6)2 Yt-3 0.2(1-0.2)3 0.4(1-0.4)3 0.6(1-0.6)3 Yt-4 0.2(1-0.2)4

0.4(1-0.4)4 0.6(1-0.6)4 Yt-5 0.2(1-0.2)5 0.4(1-0.4)5 0.6(1-0.6)5 0.8 0.8 0.9 0.9 Simple Exponential Smoothing Method The exponential smoothing equation rewritten in the following form elucidate the role of weighting factor . Ft 1 Ft ( yt Ft ) Exponential smoothing forecast is the old forecast plus an adjustment for the error that occurred in the last forecast. Simple Exponential Smoothing Method

The value of smoothing constant must be between 0 and 1 can not be equal to 0 or 1. If stable predictions with smoothed random variation is desired then a small value of is desire. If a rapid response to a real change in the pattern of observations is desired, a large value of is appropriate. Simple Exponential Smoothing Method To estimate , Forecasts are computed for equal to .1, .2, .3, , .9 and the sum of squared forecast error is computed for each. The value of with the smallest RMSE is chosen for use in producing the future forecasts. Simple Exponential Smoothing Method To start the algorithm, we need F1 because F2 y1 (1 ) F1 Since F1 is not known, we can Set the first estimate equal to the first observation. Use the average of the first five or six observations for the initial smoothed value. Example:University of Michigan Index

of Consumer Sentiment University of Michigan Index of Consumer Sentiment for January1995December1996. we want to forecast the University of Michigan Index of Consumer Sentiment using Simple Exponential Smoothing Method. Date Observed Jan-95 97.6 Feb-95 95.1 Mar-95 90.3 Apr-95 92.5 May-95 89.8 Jun-95 92.7 Jul-95 94.4 Aug-95 96.2 Sep-95 88.9 Oc t-95 90.2 Nov-95 88.2 Dec-95

91 Jan-96 89.3 Feb-96 88.5 Mar-96 93.7 Apr-96 92.7 May-96 94.7 Jun-96 95.3 Jul-96 94.7 Aug-96 95.3 Sep-96 94.7 Oc t-96 96.5 Nov-96 99.2 Dec-96 96.9 Jan-97 Example:University of Michigan Index of Consumer Sentiment Since no forecast is available for the first period, we will set the first estimate equal to the first observation. We try =0.3, and 0.6. University of Michigan Index of Consumer

Sentiment 100 Consumer Sentiment Index 98 96 94 92 90 88 86 Sep-94 Apr-95 Oct-95 May-96 Date Dec-96 Jun-97 Example:University of Michigan Index of Consumer Sentiment Note the first forecast is the first observed value. The forecast for Feb. 95 (t = 2) and Mar. 95 (t = 3) are evaluated as follows: y t 1 y t ( yt y t ) y 2 y1 0.6( y1 y1 ) 97.6 0.6(97.6 97.6) 97.6 y 3 y 2 0.6( y2 y 2 ) 97.6 0.6(95.1 97.6) 96.1

Date Jan-95 Feb-95 Mar-95 Apr-95 May-95 Jun-95 Jul-95 Aug-95 Sep-95 Oct-95 Nov-95 Dec-95 Jan-96 Feb-96 Mar-96 Apr-96 May-96 Jun-96 Jul-96 Aug-96 Sep-96 Oct-96 Nov-96 Dec-96 Jan-97 Feb-97 Mar-97 Apr-97 May-97 Jun-97 Jul-97 Aug-97 Sep-97 Oct-97 Nov-97 Dec-97 Consumer Sentiment 97.6

95.1 90.3 92.5 89.8 92.7 94.4 96.2 88.9 90.2 88.2 91 89.3 88.5 93.7 92.7 89.4 92.4 94.7 95.3 94.7 96.5 99.2 96.9 97.4 99.7 100 101.4 103.2 104.5 107.1 104.4 106 105.6 107.2 102.1 Alpha =0.3 #N/A 97.60 96.85 94.89

94.17 92.86 92.81 93.29 94.16 92.58 91.87 90.77 90.84 90.38 89.81 90.98 91.50 90.87 91.33 92.34 93.23 93.67 94.52 95.92 96.22 96.57 97.51 98.26 99.20 100.40 101.63 103.27 103.61 104.33 104.71 105.46 Alpha=0.6 #N/A 97.60 96.10 92.62 92.55 90.90 91.98

93.43 95.09 91.38 90.67 89.19 90.28 89.69 88.98 91.81 92.34 90.58 91.67 93.49 94.58 94.65 95.76 97.82 97.27 97.35 98.76 99.50 100.64 102.18 103.57 105.69 104.92 105.57 105.59 106.55 Example:University of Michigan Index of Consumer Sentiment RMSE =2.66 for = 0.6 RMSE =2.96 for = 0.3 University of Michigan Index of Consumer sentiments 120

100 Sentiment Index 80 Consumer Sentiment 60 SES (Alpha =0.3) SES(Alpha=0.6) 40 20 0 Jun-94 Oct-95 Mar-97 Jul-98 Months Dec-99 Apr-01 Holts Exponential smoothing Holts two parameter exponential smoothing method is an extension of simple exponential smoothing. It adds a growth factor (or trend factor) to the smoothing equation as a way of adjusting for the trend.

Holts Exponential smoothing Three equations and two smoothing constants are used in the model. The exponentially smoothed series or current level estimate. L t yt (1 )( Lt 1 bt 1 ) The trend estimate. bt ( Lt Lt 1 ) (1 )bt 1 Forecast m periods into the future. F t m Lt mbt Holts Exponential smoothing Lt = Estimate of the level of the series at time t = smoothing constant for the data. yt = new observation or actual value of series in period t. = smoothing constant for trend estimate bt = estimate of the slope of the series at time t

m = periods to be forecast into the future. Holts Exponential smoothing The weight and can be selected subjectively or by minimizing a measure of forecast error such as RMSE. Large weights result in more rapid changes in the component. Small weights result in less rapid changes. Holts Exponential smoothing The initialization process for Holts linear exponential smoothing requires two estimates: One to get the first smoothed value for L1 The other to get the trend b1. One alternative is to set L1 = y1 and b1 y 2 y1 or b1 y 4 y1 3

or b1 0 Example:Quarterly sales of saws for Acme tool company The following table shows the sales of saws for the Acme tool Company. These are quarterly sales From 1994 through 2000. Year 1994 1995 1996 1997 1998 1999 2000 Quarter t 1 2 3 4 1

2 3 4 1 2 3 4 1 2 3 4 1 2 3 4 1 2 3 4 1 2 3 4 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17

18 19 20 21 22 23 24 25 26 27 28 sales 500 350 250 400 450 350 200 300 350 200 150 400 550 350 250 550 550 400 350 600 750 500 400 650 850 600 450 700

Example:Quarterly sales of saws for Acme tool company Examination of the plot shows: A non-stationary time series data. Seasonal variation seems to exist. Sales for the first and fourth quarter are larger than other quarters. Sales of saws for the Acme Tool Company: 1994-2000 900 800 700 600 500 Saws 400 300 200 100

0 0 5 10 15 Year 20 25 30 Example:Quarterly sales of saws for Acme tool company The plot of the Acme data shows that there might be trending in the data therefore we will try Holts model to produce forecasts. We need two initial values The first smoothed value for L1 The initial trend value b1. We will use the first observation for the estimate of the smoothed value L1, and the initial trend value b1 = 0. We will use = .3 and =.1.

Example:Quarterly sales of saws for Acme tool company Year 1994 1995 1996 1997 1998 1999 2000 Quarter 1 2 3 4 1 2 3 4 1 2 3 4 1 2 3 4 1 2 3 4 1 2 3

4 1 2 3 4 t sales 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 500 350 250

400 450 350 200 300 350 200 150 400 550 350 250 550 550 400 350 600 750 500 400 650 850 600 450 700 Lt 500.00 455.00 390.35 385.88 398.18 378.34 318.61 303.23 307.38 266.55 220.98 261.95 339.77 340.55

311.38 379.12 431.67 427.00 407.92 467.83 558.73 553.10 517.56 564.16 659.35 656.71 608.16 644.43 bt 0.00 -4.50 -10.52 -9.91 -7.69 -8.90 -13.99 -14.13 -12.30 -15.15 -18.19 -12.28 -3.27 -2.86 -5.49 1.83 6.90 5.74 3.26 8.93 17.12 14.85 9.81 13.49 21.66

19.23 12.45 14.83 Ft+m 500.00 500.00 450.50 379.84 375.97 390.49 369.44 304.62 289.11 295.08 251.40 202.79 249.67 336.50 337.69 305.89 380.95 438.57 432.74 411.18 476.75 575.85 567.94 527.37 577.65 681.01 675.94 620.61 Example:Quarterly sales of saws for Acme tool company RMSE for this application is:

= .3 and = .1 RMSE = 155.5 The plot also showed the possibility of seasonal variation that needs to be investigated. Quarterly Saw Sales Forecast Holt's Method 900 800 700 600 500 sales Sales Ht+m 400 300 200 100 0 0 5 10 15

Quarters 20 25 30 Winters Exponential Smoothing Winters exponential smoothing model is the second extension of the basic Exponential smoothing model. It is used for data that exhibit both trend and seasonality. It is a three parameter model that is an extension of Holts method. An additional equation adjusts the model for the seasonal component. Winters Exponential Smoothing The four equations necessary for Winters multiplicative method are: The exponentially smoothed series: Lt yt (1 )( Lt 1 bt 1 )

St s The trend estimate: bt ( Lt Lt 1 ) (1 )bt 1 The seasonality estimate: St yt (1 ) S t s Lt Winters Exponential Smoothing Forecast m period into the future: Ft m ( Lt mbt ) St m s Lt = level of series. = smoothing constant for the data. yt = new observation or actual value in period t. = smoothing constant for trend estimate. bt = trend estimate. = smoothing constant for seasonality estimate. St =seasonal component estimate. m = Number of periods in the forecast lead period. s = length of seasonality (number of periods in the season) = forecast for m periods into the future.

Ft m Winters Exponential Smoothing As with Holts linear exponential smoothing, the weights , , and can be selected subjectively or by minimizing a measure of forecast error such as RMSE. As with all exponential smoothing methods, we need initial values for the components to start the algorithm. To start the algorithm, the initial values for L t, the trend bt, and the indices St must be set. Winters Exponential Smoothing To determine initial estimates of the seasonal indices we need to use at least one complete season's data (i.e. s periods).Therefore,we initialize trend and level at period s. Initialize level as: Initialize trend as 1 Ls ( y1 y2 y s ) s Initialize seasonal indices as: y ys

1 y y y y2 bs ( s 1 1 s 2 s s ) s s s s S1 y y1 y , S 2 2 ,, S s s Ls Ls Ls Winters Exponential Smoothing We will apply Winters method to Acme Tool company sales. The value for is .4, the value for is .1, and the value for is .3. The smoothing constant smoothes the data to eliminate randomness. The smoothing constant smoothes the trend in the data set. Winters Exponential Smoothing The smoothing constant smoothes the seasonality in the data.

The initial values for the smoothed series L t, the trend bt, and the seasonal index St must be set. Example: Quarterly Sales of Saws for Acme tool Year 1994 1995 1996 1997 1998 1999 2000 Quarter 1 2 3 4 1 2 3 4 1 2 3 4 1 2 3 4 1 2 3

4 1 2 3 4 1 2 3 4 t 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 sales

500 350 250 400 450 350 200 300 350 200 150 400 550 350 250 550 550 400 350 600 750 500 400 650 850 600 450 700 Lt 375 396.9667 372.3747 296.7938 287.3869 302.1219 252.9623 201.4173 268.2504 373.5062

363.8087 317.4823 406.7605 465.9614 444.9496 410.5851 487.3071 597.7855 570.255 510.9496 570.7076 689.6728 667.561 591.6084 640.1658 bt -12.5 -9.05333 -10.6072 -17.1046 -16.3348 -13.2278 -16.821 -20.2934 -11.5807 0.102908 -0.87713 -5.42206 4.047961 9.563264 6.505758 2.418728 9.84905 19.91199 15.16774 7.720431 12.92419 23.52829 18.96428

9.472591 13.38107 St 1.333333 0.933333 0.666667 1.066667 1.273412 0.935307 0.668827 1.059833 1.23893 0.891905 0.691596 1.189227 1.309011 0.912946 0.720351 1.238103 1.270414 0.908756 0.759978 1.236049 1.265679 0.899169 0.766841 1.206915 1.255716 0.899057 0.764981 1.172881 Ft+m 483.3333 362.0524 241.1783 298.3352 345.161 270.2048

157.9377 191.9611 317.9958 333.2237 251.002 371.1103 537.7528 434.1286 325.2062 511.3412 631.5942 561.3363 444.9085 641.1016 738.6906 641.2886 526.4561 725.4539 Example: Quarterly Sales of Saws for Acme tool RMSE for this application is: = 0.4, = 0.1, = 0.3 and RMSE = 83.36 Note the decrease in RMSE. Quarterly Saw Sales Forecas:t Winter's Method 900 800 700 600 500

sales Sales Ft+m 400 300 200 100 0 0 5 10 15 Quarters 20 25 30 Additive Seasonality The seasonal component in Holt-Winters method. The basic equations for Holts Winters additive method are:

Lt ( yt St s ) (1 )( Lt 1 bt 1 ) bt ( Lt Lt 1 ) (1 )bt 1 St ( yt Lt ) (1 ) St s Ft m Lt bt m St m s Additive Seasonality The initial values for Ls and bs are identical to those for the multiplicative method. To initialize the seasonal indices we use S1 y1 Ls , S 2 y2 Ls , , S s Ys Ls

## Recently Viewed Presentations

• Integration of my NCBI Tools. Method A&B. Method C&D. Information from the fields in PubMed, PubMed Central and the NIH Manuscript Submission System are all part of NCBI and transferred to other NCBI fields.
• It offers an opportunity to consider how we take part in Mass. It is especially aimed at participants in the liturgy - which of course includes the ministers - it seeks to inform, and to promote a liturgical spirituality How...
• Spinal or existing working epidural. Take care to interrogate your epidural. It may have been turned down to aid pushing efforts. Mom in a very fragile state may cloud the issue. C/S - at a Glance. Regional vs GA. Time,...
• Changing Landscape and Client Communication . Obligation to Notify. How to Keep Clients Informed. Indirect or Direct Impact to Case. Will client be impacted v. likelihood that a change may impact client
• Stage 3 - Black Putrefaction. Most of body mass lost mainly due to the activity of the maggots and other insects. Body's organs will degenerate into soupy mess. Black Putrefaction occurs 10-20 days after death. Stage 4 - Butyric Fermentation.
• Write a one-sentence summary of the point of the poemâ€”be specific!! Read "Douglass" Identify the type of sonnet (English/Italian) Label the rhyme scheme Identify the two parts (depending on which type of sonnet it is) Annotate What is the tone...
• Maximum Extent of Pleistocene Glaciation - 1/3 of land surface Most recent glacial maximum peaked 18,000 years ago and is considered to have ended 10,000 B.P. Current Extent of Glaciation - about 10% of land surface Franz Joseph Glacier and...
• Eduardo Nebot (BI) 2ndMarch2011 - ICE meeting. Contents. What are BLMs? What are they used for? Types of BLMs. During the MD. Data saving and other useful tips for analysis . 2ndMarch2011 - ICE meeting. Contents. What are BLMs? What...