Returns forecasts and other information for exponential smoothing forecasts
applied to y
.
ses(
y,
h = 10,
level = c(80, 95),
fan = FALSE,
initial = c("optimal", "simple"),
alpha = NULL,
lambda = NULL,
biasadj = FALSE,
x = y,
...
)holt(
y,
h = 10,
damped = FALSE,
level = c(80, 95),
fan = FALSE,
initial = c("optimal", "simple"),
exponential = FALSE,
alpha = NULL,
beta = NULL,
phi = NULL,
lambda = NULL,
biasadj = FALSE,
x = y,
...
)
hw(
y,
h = 2 * frequency(x),
seasonal = c("additive", "multiplicative"),
damped = FALSE,
level = c(80, 95),
fan = FALSE,
initial = c("optimal", "simple"),
exponential = FALSE,
alpha = NULL,
beta = NULL,
gamma = NULL,
phi = NULL,
lambda = NULL,
biasadj = FALSE,
x = y,
...
)
An object of class "forecast
".
The function summary
is used to obtain and print a summary of the
results, while the function plot
produces a plot of the forecasts and
prediction intervals.
The generic accessor functions fitted.values
and residuals
extract useful features of the value returned by ets
and associated
functions.
An object of class "forecast"
is a list containing at least the
following elements:
A list containing information about the fitted model
The name of the forecasting method as a character string
Point forecasts as a time series
Lower limits for prediction intervals
Upper limits for prediction intervals
The confidence values associated with the prediction intervals
The original time series
(either object
itself or the time series used to create the model
stored as object
).
Residuals from the fitted model.
Fitted values (one-step forecasts)
a numeric vector or time series of class ts
Number of periods for forecasting.
Confidence level for prediction intervals.
If TRUE, level is set to seq(51,99,by=3). This is suitable for fan plots.
Method used for selecting initial state values. If
optimal
, the initial values are optimized along with the smoothing
parameters using ets
. If simple
, the initial values are
set to values obtained using simple calculations on the first few
observations. See Hyndman & Athanasopoulos (2014) for details.
Value of smoothing parameter for the level. If NULL
, it
will be estimated.
Box-Cox transformation parameter. If lambda="auto"
,
then a transformation is automatically selected using BoxCox.lambda
.
The transformation is ignored if NULL. Otherwise,
data transformed before model is estimated.
Use adjusted back-transformed mean for Box-Cox transformations. If transformed data is used to produce forecasts and fitted values, a regular back transformation will result in median forecasts. If biasadj is TRUE, an adjustment will be made to produce mean forecasts and fitted values.
Deprecated. Included for backwards compatibility.
Other arguments passed to forecast.ets
.
If TRUE, use a damped trend.
If TRUE, an exponential trend is fitted. Otherwise, the trend is (locally) linear.
Value of smoothing parameter for the trend. If NULL
, it
will be estimated.
Value of damping parameter if damped=TRUE
. If NULL
,
it will be estimated.
Type of seasonality in hw
model. "additive" or
"multiplicative"
Value of smoothing parameter for the seasonal component. If
NULL
, it will be estimated.
Rob J Hyndman
ses, holt and hw are simply convenient wrapper functions for
forecast(ets(...))
.
Hyndman, R.J., Koehler, A.B., Ord, J.K., Snyder, R.D. (2008) Forecasting with exponential smoothing: the state space approach, Springer-Verlag: New York. http://www.exponentialsmoothing.net.
Hyndman and Athanasopoulos (2018) Forecasting: principles and practice, 2nd edition, OTexts: Melbourne, Australia. https://otexts.com/fpp2/
ets
, HoltWinters
,
rwf
, arima
.
fcast <- holt(airmiles)
plot(fcast)
deaths.fcast <- hw(USAccDeaths,h=48)
plot(deaths.fcast)
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