Returns forecasts and other information for Croston's forecasts applied to y.

croston(y, h = 10, alpha = 0.1, x = y)



a numeric vector or time series of class ts


Number of periods for forecasting.


Value of alpha. Default value is 0.1.


Deprecated. Included for backwards compatibility.


An object of class "forecast" is a list containing at least the following elements:


A list containing information about the fitted model. The first element gives the model used for non-zero demands. The second element gives the model used for times between non-zero demands. Both elements are of class forecast.


The name of the forecasting method as a character string


Point forecasts as a time series


The original time series (either object itself or the time series used to create the model stored as object).


Residuals from the fitted model. That is y minus fitted values.


Fitted values (one-step forecasts)

The function summary is used to obtain and print a summary of the results, while the function plot produces a plot of the forecasts. The generic accessor functions fitted.values and residuals extract useful features of the value returned by croston and associated functions.


Based on Croston's (1972) method for intermittent demand forecasting, also described in Shenstone and Hyndman (2005). Croston's method involves using simple exponential smoothing (SES) on the non-zero elements of the time series and a separate application of SES to the times between non-zero elements of the time series. The smoothing parameters of the two applications of SES are assumed to be equal and are denoted by alpha.

Note that prediction intervals are not computed as Croston's method has no underlying stochastic model.


Croston, J. (1972) "Forecasting and stock control for intermittent demands", Operational Research Quarterly, 23(3), 289-303.

Shenstone, L., and Hyndman, R.J. (2005) "Stochastic models underlying Croston's method for intermittent demand forecasting". Journal of Forecasting, 24, 389-402.

See also


Rob J Hyndman


y <- rpois(20,lambda=.3) fcast <- croston(y) plot(fcast)