Performs Holt's two-parameter exponential smoothing for linear trend or damped trend.
Holt(x, type = c("additive", "multiplicative"), alpha = 0.2,
beta = 0.1057, lead = 0, damped = FALSE, phi = 0.98, plot = TRUE)A list with class "Holt" containing the following components:
the estimate values.
the smoothing parameter used for level.
the smoothing parameter used for trend.
the smoothing parameter used for damped trend.
the predicted values, only available for lead > 0.
the accurate measurements.
a numeric vector or univariate time series.
the type of interaction between the level and the linear trend. See details.
the parameter for the level smoothing. The default is 0.2.
the parameter for the trend smoothing. The default is 0.1057.
the number of steps ahead for which prediction is required.
The default is 0.
a logical value indicating a damped trend. See details. The default is
FALSE.
a smoothing parameter for damped trend. The default is 0.98, only valid
for damped = TRUE.
a logical value indicating to print the plot of original data v.s smoothed
data. The default is TRUE.
Debin Qiu
Holt's two parameter is used to forecast a time series with trend, but
wihtout seasonal pattern. For the additive model (type = "additive"), the
\(h\)-step-ahead forecast is given by \(hat{x}[t+h|t] = level[t] + h*b[t]\),
where
$$level[t] = \alpha *x[t] + (1-\alpha)*(b[t-1] + level[t-1]),$$
$$b[t] = \beta*(level[t] - level[t-1]) + (1-\beta)*b[t-1],$$
in which \(b[t]\) is the trend component.
For the multiplicative (type = "multiplicative") model, the
\(h\)-step-ahead forecast is given by \(hat{x}[t+h|t] = level[t] + h*b[t]\),
where
$$level[t] = \alpha *x[t] + (1-\alpha)*(b[t-1] * level[t-1]),$$
$$b[t] = \beta*(level[t] / level[t-1]) + (1-\beta)*b[t-1].$$
Compared with the Holt's linear trend that displays a constant increasing or
decreasing, the damped trend generated by exponential smoothing method shows a
exponential growth or decline, which is a situation between simple exponential
smoothing (with 0 increasing or decreasing rate) and Holt's two-parameter smoothing.
If damped = TRUE, the additive model becomes
$$hat{x}[t+h|t] = level[t] + (\phi + \phi^{2} + ... + \phi^{h})*b[t],$$
$$level[t] = \alpha *x[t] + (1-\alpha)*(\phi*b[t-1] + level[t-1]),$$
$$b[t] = \beta*(level[t] - level[t-1]) + (1-\beta)*\phi*b[t-1].$$
The multiplicative model becomes
$$hat{x}[t+h|t] = level[t] *b[t]^(\phi + \phi^{2} + ... + \phi^{h}),$$
$$level[t] = \alpha *x[t] + (1-\alpha)*(b[t-1]^{\phi} * level[t-1]),$$
$$b[t] = \beta*(level[t] / level[t-1]) + (1-\beta)*b[t-1]^{\phi}.$$
See Chapter 7.4 for more details in R. J. Hyndman and G. Athanasopoulos (2013).
R. J. Hyndman and G. Athanasopoulos, "Forecasting: principles and practice," 2013. [Online]. Available: http://otexts.org/fpp/.
HoltWinters, expsmooth, Winters
x <- (1:100)/100
y <- 2 + 1.2*x + rnorm(100)
ho0 <- Holt(y) # with additive interaction
ho1 <- Holt(y,damped = TRUE) # with damped trend
# multiplicative model for AirPassengers data,
# although seasonal pattern exists.
ho2 <- Holt(AirPassengers,type = "multiplicative")
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