Double Exponential Smoothing (Holt's Method) PDF
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This document explains double exponential smoothing (Holt's method) and triple exponential smoothing (Holt-Winters' method), used for forecasting time series data. It covers the methods for both additive and multiplicative seasonality and provides formulas and steps for applying these methods. It also features a numerical example of its application.
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Double Exponential Smoothing (Holtβs Method) Used for forecasting the time series when the data has a linear trend and no seasonal pattern. Also called Holtβs trend corrected or second-order exponential smoothing. Introduce a term to take care of trend present in the time series. Cap...
Double Exponential Smoothing (Holtβs Method) Used for forecasting the time series when the data has a linear trend and no seasonal pattern. Also called Holtβs trend corrected or second-order exponential smoothing. Introduce a term to take care of trend present in the time series. Capable of capturing increase or decrease in linear trend. 1 Steps For π‘ = 0, π 0 = π¦0. For π‘ > 0, π π‘ = πΌπ¦π‘ + (1 β πΌ)(π π‘β1 + ππ‘β1 ) ππ‘ = π½ π π‘ β π π‘β1 + (1 β π½)ππ‘β1 Where, ππ‘ is the best estimate of trend at time t. 0 < π½ < 1 is the trend smoothing factor. 2 Triple Exponential Smoothing (Holt Winterβs Method) Used for forecasting the time series when the data has a linear trend and a seasonal pattern also. Also called Holt Winterβs method or third-order exponential smoothing. Introduce two terms to take care of trend and seasonality present in the time series. Capable of capturing increase or decrease in linear trend and seasonal patterns. 3 Involved Notations π π‘ : smoothed statistic πΌ: smoothing parameter of data. 0 < πΌ < 1. ππ‘ : best estimate of trend at time t. π½: trend smoothing factor. 0 < π½ < 1. ππ‘ : sequence of seasonal correction factor at time t. πΎ: seasonal change smoothing factor. 0 < πΎ < 1. 4 Involved Notations Further, Let L denote the length of the cycle of seasonal change. If we have a monthly data having seasonality of period 12, πΏ = 12. Let N denote the number of cycles. If we have monthly data with seasonality of period 12 for 10 years, π = 10. Two cases of seasonality: Multiplicative and Additive. 5 Additive Seasonality ππ‘ = ππ‘ + ππ‘ + ππ‘ The seasonal effect is added to the trend, and the seasonal effect is roughly constant over time. E.g., imagine sales of a product over the year. In an additive model, the sales might increase by a fixed number (e.g., 100 units) every December due to holiday shopping, regardless of the general sales level throughout the year. 6 Multiplicative Seasonality ππ‘ = ππ‘ Γ ππ‘ Γ ππ‘ The seasonal effect is multiplied to the trend, resulting in larger seasonal fluctuations when the time series is at a higher level. E.g., imagine sales of a product over the year. In a multiplicative model, the sales in December might double as compared to other months. 7 Steps for Multiplicative Seasonality π 0 = π¦0 π¦π‘ π π‘ = πΌ + (1 β πΌ)(π π‘β1 + ππ‘β1 ) ππ‘βπΏ ππ‘ = π½ π π‘ β π π‘β1 + (1 β π½)ππ‘β1 π¦π‘ ππ‘ = πΎ + (1 β πΎ)ππ‘βπΏ π π‘ 8 Steps for Additive Seasonality π 0 = π¦0 π π‘ = πΌ + π¦π‘ β ππ‘βπΏ + (1 β πΌ)(π π‘β1 + ππ‘β1 ) ππ‘ = π½ π π‘ β π π‘β1 + (1 β π½)ππ‘β1 ππ‘ = πΎ(π¦π‘ β π π‘β1 β ππ‘β1 ) + (1 β πΎ)ππ‘βπΏ 9 Numerical Example Data on monthly air passengers. 10 Holtβs Filtering on the Data 11 Holtβs Filtering on the Data 12 Forecasts from the Holtβs Method 13 Holt Winterβs Filtering on the Data 14 Holt Winterβs Filtering on the Data 15 Forecasts from the Holt Winterβs Method 16