CHAPTER 18 Models for Time Series and Forecasting

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Presentation transcript:

CHAPTER 18 Models for Time Series and Forecasting to accompany Introduction to Business Statistics fourth edition, by Ronald M. Weiers Presentation by Priscilla Chaffe-Stengel Donald N. Stengel © 2002 The Wadsworth Group

Chapter 18 - Learning Objectives Describe the trend, cyclical, seasonal, and irregular components of the time series model. Fit a linear or quadratic trend equation to a time series. Smooth a time series with the centered moving average and exponential smoothing techniques. Determine seasonal indexes and use them to compensate for the seasonal effects in a time series. Use the trend extrapolation and exponential smoothing forecast methods to estimate a future value. Use MAD and MSE criteria to compare how well equations fit data. Use index numbers to compare business or economic measures over time. © 2002 The Wadsworth Group

Chapter 18 - Key Terms Time series Classical time series model Trend value Cyclical component Seasonal component Irregular component Trend equation Moving average Exponential smoothing Seasonal index Ratio to moving average method Deseasonalizing MAD criterion MSE criterion Constructing an index using the CPI Shifting the base of an index © 2002 The Wadsworth Group

Classical Time Series Model y = T • C • S • I where y = observed value of the time series variable T = trend component, which reflects the general tendency of the time series without fluctuations C = cyclical component, which reflects systematic fluctuations that are not calendar-related, such as business cycles S = seasonal component, which reflects systematic fluctuations that are calendar-related, such as the day of the week or the month of the year I = irregular component, which reflects fluctuations that are not systematic © 2002 The Wadsworth Group

Trend Equations Linear: = b0 + b1x Quadratic: = b0 + b1x + b2x2 = the trend line estimate of y x = time period b0, b1, and b2 are coefficients that are selected to minimize the deviations between the trend estimates and the actual data values y for the past time periods. Regression methods are used to determine the best values for the coefficients. © 2002 The Wadsworth Group

Smoothing Techniques Smoothing techniques - dampen the impacts of fluctuation in a time series, thereby providing a better view of the trend and (possibly) the cyclical components. Moving average - a technique that replaces a data value with the average of that data value and neighboring data values. Exponential smoothing - a technique that replaces a data value with a weighted average of the actual data value and the value resulting from exponential smoothing for the previous time period. © 2002 The Wadsworth Group

Moving Average A moving average for a time period is the average of N consecutive data values, including the data value for that time period. A centered moving average is a moving average such that the time period is at the center of the N time periods used to determine which values to average. If N is an even number, the techniques need to be adjusted to place the time period at the center of the averaged values. The number of time periods N is usually based on the number of periods in a seasonal cycle. The larger N is, the more fluctuation will be smoothed out. © 2002 The Wadsworth Group

Moving Average - An Example Time Period Data Value 1997, Quarter I 818 1997, Quarter II 861 1997, Quarter III 844 1997, Quarter IV 906 1998, Quarter I 867 1998, Quarter II 899 3-Quarter Centered Moving Average for 1997, Quarter IV: 4-Quarter Centered Moving Average for 1997, Quarter IV: © 2002 The Wadsworth Group

Exponential Smoothing Et = a•yt + (1 – a) Et–1 where Et = exponentially smoothed value for time period t Et–1 = exponentially smoothed value for time period t – 1 yt = actual time series value for time period t a = the smoothing constant, 0 £ a £ 1 The larger a is, the closer the smoothed value will track the original data value. The smaller a is, the more fluctuation is smoothed out. © 2002 The Wadsworth Group

Exponential Smoothing - An Example Data Smoothed Value Smoothed Value Period Value (a = 0.2) (a = 0.8) 1 818 818 818 2 861 826.6 852.4 3 844 830.1 845.7 4 906 845.3 893.9 Calculation for smoothed value for Period 2 (a = 0.2): E2 = a y + (1 – a ) E1 = 0.2 (861) + 0.8 (818) = 826.6 2 © 2002 The Wadsworth Group

Seasonal Indexes A seasonal index is a factor that adjusts a trend value to compensate for typical seasonal fluctuation in that period of a seasonal cycle. A seasonal index is expressed as a percentage with a value of 100% corresponding to an average position in a seasonal cycle. © 2002 The Wadsworth Group

Seasonal Indexes - An Example Season Index (Annual Quarter) Value I 84.5 II 102.3 III 95.5 IV 117.7 If the trend value for Quarter I in the given year was 902, the value with seasonal fluctuation would be y = T • S = 902 • 84.5% = 762.2 © 2002 The Wadsworth Group

Ratio to Moving Average Method A technique for developing a set of seasonal index values from the original time series. Steps: 1. Construct a centered moving average of the time series. Set N = number of periods in the seasonal cycle. 2. Express each original time series value as a percentage of the corresponding centered moving average. The result is the ratio to moving average. Example: If the original data value is 906 and the corresponding centered moving average is 872.3, Ratio to moving average = (906/872.3) • 100 = 103.86 © 2002 The Wadsworth Group

Ratio to Moving Average Method Steps, cont.: 3. For each period in the seasonal cycle, average all the ratio to moving average values (from Step 2) corresponding to that period in the seasonal cycle. The result is the unadjusted seasonal index for that period in the seasonal cycle. Example: If ratios corresponding to Quarter I are 80.4, 87.3, 82.1, 89.5, and 78.7, the unadjusted seasonal index value is © 2002 The Wadsworth Group

Ratio to Moving Average Method Steps, cont.: 4. The average of the seasonal index values should be 100.0 or their sum should be N•100. If not, multiply all seasonal index values by the appropriate adjustment factor, N•100 divided by the sum of unadjusted seasonal index values. Example: Unadjusted Adjusted Season Seasonal Index Seasonal Index I 83.60 83.83 II 102.07 102.35 III 95.42 95.68 IV 117.81 118.34 00276 . 1 81 117 42 95 07 102 60 83 100 4 Factor Adjustment = + × © 2002 The Wadsworth Group

Deseasonalizing a Time Series This procedure involves use of a seasonal index to remove the effect of typical seasonal fluctuation from a time series data value. The result is also called a seasonally-adjusted value. Example: If the original data value for the first quarter of a given year is 1124 and the seasonal index for Quarter I is 83.4, the seasonally-adjusted value is: 100 Period for Index Seasonal Value Data Original ized Deseasonal × = © 2002 The Wadsworth Group

Forecasting with Classical Time Series Models To forecast a value in a future time period: 1. Use the trend equation to forecast the trend value for that time period. 2. Adjust the data value using the cyclical and seasonal index values. If there is no cyclical index, do not do a cyclical adjustment. © 2002 The Wadsworth Group

Forecasting with Classical Time Series Models - An Example Example - Trend Equation: where = trend value x = number of quarters to 1997, Quarter IV To forecast the value for 1999, Quarter II Forecast of trend = 970.2 + 12.3 (6) = 1044.0 If the seasonal index for Quarter II is 102.35, the forecast with seasonal fluctuation is: © 2002 The Wadsworth Group

Forecasting with Exponential Smoothing A technique for generating a forecast for the next time period using the forecast and actual data value for the current time period. This technique is not valid if there is a significant upward or downward trend. Ft+1 = a yt + (1 – a) Ft Ft+1 = forecast for period t+1 yt = actual value for period t Ft = forecast for period t a = smoothing constant, (0 £ a £ 1) © 2002 The Wadsworth Group

Forecasting with Exponential Smoothing - An Example If the forecast for the current time period was 842 and the actual value was 872, using a smoothing constant of a = 0.6, the forecast for the next period is: (0.6) (872) + (0.4) (842) = 860 © 2002 The Wadsworth Group

Evaluating Time Series Models Models can be evaluated using past data by examining the differences (or errors) between the values predicted from the models and the actual data values. The errors can be summarized and accuracy measured using either of the following criteria: Mean Absolute Deviation (MAD) Criterion: 1. Express each difference as a positive number. 2. Find the average of the differences from Step 1. Mean Squared Error (MSE) Criterion: 1. Square each error difference. 2. Find the average of the squared error differences from Step 1. © 2002 The Wadsworth Group

Evaluating Time Series Models - An Example Value Actual Computed Data Absolute Squared By Model Value Deviation Error 1440 1436 4 16 1456 1461 5 25 1472 1480 8 64 1488 1472 16 156 1504 1495 9 81 Sums: 42 342 MAD = 42/5 = 8.4 MSE = 342/5 = 68.4 © 2002 The Wadsworth Group

What are index numbers? Index numbers: are time series that focus on the relative change in a count or measurement over time. express the count or measurement as a percentage of the comparable count or measurement in a base period. © 2002 The Wadsworth Group

Base Periods for Index Numbers The base period is arbitrary but should be a convenient point of reference. The value of an index number corresponding to the base period is always 100. The base period may be a single period or an average of multiple adjacent periods. © 2002 The Wadsworth Group

Applications of Index Numbers in Business and Economics A price index shows the change in the price of a commodity or group of commodities over time. A quantity index shows the change in quantity of a commodity or group of commodities used or purchased over time. A value index shows a change in total dollar value (price • quantity) of a commodity or group of commodities over time. © 2002 The Wadsworth Group

Simple Relative Index A simple relative index shows the change in the price, quantity, or value of a single commodity over time. Calculation of a simple relative index: Index in period t = © 2002 The Wadsworth Group

Example: Simple Relative Price Index Price Index Price Index Year Price 1985 as base year 1995 as base year 1985 $140 100.0 58.3 1990 195 139.3 81.3 1995 240 171.4 100.0 2000 275 196.4 114.6 Computation of index for 1990 (1985 as base year): © 2002 The Wadsworth Group

Consumer Price Index A weighted aggregate price index used to reflect the overall change in the cost of goods and services purchased by a typical consumer. Applications: Indicator of rate of inflation Used to adjust wages to compensate for lost purchasing power due to inflation Used to convert a price or wage to a real price or real wage to show the equivalent amount in a base period after adjusting for inflation. © 2002 The Wadsworth Group

Example: The CPI as Deflator Suppose a person was earning $50,000 per year in June 2001, when the CPI was 178.0 (base year: 1982-84 ). What was the person’s real income in its 1982-84 equivalent? Real income in period t = Income in period t • Real earnings in 2001 = $50,000 • 100/178.0 = $28,090 © 2002 The Wadsworth Group

Example: The CPI as Deflator Suppose the same person was earning $46,500 per year in 1997, when the CPI was 160.5 (base year: 1982-84 ). What was the person’s real income in its 1982-84 equivalent? Real earnings in 1997 = $46,500 • 100/160.5 = $28,972 The purchasing power of the person’s earnings was higher in 1997 than in 2001. © 2002 The Wadsworth Group

Shifting the Base of an Index For useful interpretation, it is often desirable for the base year to be fairly recent. To shift the base year to another year without recalculating the index from the original data: © 2002 The Wadsworth Group

Example: Shifting a Base Year To shift a base year from 1985 to 1995: Price Index Price Index Yr 1985 as base yr 1995 as base yr 1985 100.0 58.3 1990 139.3 81.3 1995 171.4 100.0 2000 196.4 114.6 An Illustration: © 2002 The Wadsworth Group