Returns forecasts and other information for exponential smoothing forecasts
applied to y
.
Usage
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,
...
)
Arguments
- y
a numeric vector or time series of class
ts
- h
Number of periods for forecasting.
- level
Confidence level for prediction intervals.
- fan
If TRUE, level is set to seq(51,99,by=3). This is suitable for fan plots.
- initial
Method used for selecting initial state values. If
optimal
, the initial values are optimized along with the smoothing parameters usingets
. Ifsimple
, the initial values are set to values obtained using simple calculations on the first few observations. See Hyndman & Athanasopoulos (2014) for details.- alpha
Value of smoothing parameter for the level. If
NULL
, it will be estimated.- lambda
Box-Cox transformation parameter. If
lambda="auto"
, then a transformation is automatically selected usingBoxCox.lambda
. The transformation is ignored if NULL. Otherwise, data transformed before model is estimated.- biasadj
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.
- x
Deprecated. Included for backwards compatibility.
- ...
Other arguments passed to
forecast.ets
.- damped
If TRUE, use a damped trend.
- exponential
If TRUE, an exponential trend is fitted. Otherwise, the trend is (locally) linear.
- beta
Value of smoothing parameter for the trend. If
NULL
, it will be estimated.- phi
Value of damping parameter if
damped=TRUE
. IfNULL
, it will be estimated.- seasonal
Type of seasonality in
hw
model. "additive" or "multiplicative"- gamma
Value of smoothing parameter for the seasonal component. If
NULL
, it will be estimated.
Value
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:
- model
A list containing information about the fitted model
- method
The name of the forecasting method as a character string
- mean
Point forecasts as a time series
- lower
Lower limits for prediction intervals
- upper
Upper limits for prediction intervals
- level
The confidence values associated with the prediction intervals
- x
The original time series (either
object
itself or the time series used to create the model stored asobject
).- residuals
Residuals from the fitted model.
- fitted
Fitted values (one-step forecasts)
References
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/
See also
ets
, HoltWinters
,
rwf
, arima
.