Constants and ARIMA models in R

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This post is from my new book Forecasting: principles and practice, available freely online at OTexts.com/fpp/.


A non-seasonal ARIMA model can be written as

(1)   \begin{equation*} (1-\phi_1B - \cdots - \phi_p B^p)(1-B)^d y_t = c + (1 + \theta_1 B + \cdots + \theta_q B^q)e_t \end{equation*}

or equivalently as

(2)   \begin{equation*} (1-\phi_1B - \cdots - \phi_p B^p)(1-B)^d (y_t - \mu t^d/d!) = (1 + \theta_1 B + \cdots + \theta_q B^q)e_t, \end{equation*}

where B is the backshift operator, c = \mu(1-\phi_1 - \cdots - \phi_p ) and \mu is the mean of (1-B)^d y_t. R uses the parametrization of equation (2).

Thus, the inclusion of a constant in a non-stationary ARIMA model is equivalent to inducing a polynomial trend of order d in the forecast function. (If the constant is omitted, the forecast function includes a polynomial trend of order d-1.) When d=0, we have the special case that \mu is the mean of y_t.

Including constants in ARIMA models using R

arima()

By default, the arima() command in R sets c=\mu=0 when 0″ title=”Rendered by QuickLaTeX.com” style=”vertical-align: 0px;”/> and provides an estimate of \mu when d=0. The parameter \mu is called the “intercept” in the R output. It will be close to the sample mean of the time series, but usually not identical to it as the sample mean is not the maximum likelihood estimate when 0″ title=”Rendered by QuickLaTeX.com” style=”vertical-align: -4px;”/>.

The arima() command has an argument include.mean which only has an effect when d=0 and is TRUE by default. Setting include.mean=FALSE will force \mu=0.

Arima()

The Arima() command from the forecast package provides more flexibility on the inclusion of a constant. It has an argument include.mean which has identical functionality to the corresponding argument for arima(). It also has an argument include.drift which allows \mu\ne0 when d=1. For 1″ title=”Rendered by QuickLaTeX.com” style=”vertical-align: -1px;”/>, no constant is allowed as a quadratic or higher order trend is particularly dangerous when forecasting. The parameter \mu is called the “drift” in the R output when d=1.

There is also an argument include.constant which, if TRUE, will set include.mean=TRUE if d=0 and include.drift=TRUE when d=1. If include.constant=FALSE, both include.mean and include.drift will be set to FALSE. If include.constant is used, the values of include.mean=TRUE and include.drift=TRUE are ignored.

When d=0 and include.drift=TRUE, the fitted model from Arima() is

    \[(1-\phi_1B - \cdots - \phi_p B^p) (y_t - a - bt) = (1 + \theta_1 B + \cdots + \theta_q B^q)e_t.\]

In this case, the R output will label a as the “intercept” and b as the “drift” coefficient.

auto.arima()

The auto.arima() function automates the inclusion of a constant. By default, for d=0 or d=1, a constant will be included if it improves the AIC value; for 1″ title=”Rendered by QuickLaTeX.com” style=”vertical-align: -1px;”/> the constant is always omitted. If allowdrift=FALSE is specified, then the constant is only allowed when d=0.

Eventual forecast functions

The eventual forecast function (EFF) is the limit of \hat{y}_{t+h|t} as a function of the forecast horizon h as h\rightarrow\infty.

The constant c has an important effect on the long-term forecasts obtained from these models.

  • If c=0 and d=0, the EFF will go to zero.
  • If c=0 and d=1, the EFF will go to a non-zero constant determined by the last few observations.
  • If c=0 and d=2, the EFF will follow a straight line with intercept and slope determined by the last few observations.
  • If c\ne0 and d=0, the EFF will go to the mean of the data.
  • If c\ne0 and d=1, the EFF will follow a straight line with slope equal to the mean of the differenced data.
  • If c\ne0 and d=2, the EFF will follow a quadratic trend.

Seasonal ARIMA models

If a seasonal model is used, all of the above will hold with d replaced by d+D where D is the order of seasonal differencing and d is the order of non-seasonal differencing.

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