Skip to main content Accessibility help
×
Hostname: page-component-8448b6f56d-c4f8m Total loading time: 0 Render date: 2024-04-18T08:05:35.437Z Has data issue: false hasContentIssue false

6 - Cointegration and Error Correction Models

Published online by Cambridge University Press:  05 December 2014

Janet M. Box-Steffensmeier
Affiliation:
Ohio State University
John R. Freeman
Affiliation:
University of Minnesota
Matthew P. Hitt
Affiliation:
Louisiana State University
Jon C. W. Pevehouse
Affiliation:
University of Wisconsin, Madison
Get access

Summary

INTRODUCTION

The study of equilibrium relationships is at the heart of time series analysis. Because cointegration provides one way to study equilibrium relationships, it is a cornerstone of current time series analysis. The original idea behind cointegraton is that two series may be in equilibrium in the long run, but in the short run the two series deviate from that equilibrium. Clarke, Stewart, and Whiteley (1998, 562) explain that “cointegrated series are in a dynamic equilibrium in the sense that they tend to move together in the long run. Shocks that persist over a single period are ‘reequilibrated’ or adjusted by this cointegrating relationship.” Thus cointegration suggests a long-run relationship between two or more series that may move in quite different ways in the short run. Put a bit more formally, cointegration says that a specific combination of two non stationary series may be stationary. We then say these two series or variables are cointegrated, and the vector that defines the stationary linear combination is called the cointegrating vector.

Recall from the previous chapter that a time series is stationary when its mean and variance do not vary over or depend on time. Lin and Brannigan(2003, 153) point out that “many times series variables in the social sciences and historical studies are nonstationary since the variables typically measure the changing properties of social events over, for example, the last century or over the last x-number of months or days of observations. These variables display time varying means, variances, and sometimes autocovariances.”

Type
Chapter
Information
Publisher: Cambridge University Press
Print publication year: 2014

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Save book to Kindle

To save this book to your Kindle, first ensure coreplatform@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×