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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