Skip to main content Accessibility help
×
Hostname: page-component-78c5997874-v9fdk Total loading time: 0 Render date: 2024-11-14T23:00:09.000Z Has data issue: false hasContentIssue false

11 - Conjugate direction/gradient methods

from PART III - COMPUTATIONAL TECHNIQUES

Published online by Cambridge University Press:  18 December 2009

John M. Lewis
Affiliation:
National Severe Storms Laboratory, Oklahoma
S. Lakshmivarahan
Affiliation:
University of Oklahoma
Sudarshan Dhall
Affiliation:
University of Oklahoma
Get access

Summary

The major impetus for the development of conjugate direction/gradient methods stems from the weakness of the steepest descent method (Chapter 10). Recall that while the search directions which are the negative of the gradient of the function being minimized can be computed rather easily, the convergence of the steepest descent method can be annoyingly slow. This is often exhibited by the zig-zag or oscillatory behavior of the iterates. To use an analogy, there is lot of talk with very little substance. The net force that drives the iterates towards the minimum becomes very weak as the problem becomes progressively ill-conditioned (see Remark 10.3.1). The reason for this undesirable behavior is largely a result of the absence of transitivity of the orthogonality of the successive search directions (Exercise 10.5). Consequently the iterates are caged up in a smaller (two) dimensional subspace and the method is unable to exploit the full n degrees of freedom that are available at our disposal. Conjugate direction method was designed to remedy this situation by requiring that the successive search directions are mutually A-Conjugate (Exercise 10.6). A-Conjugacy is a natural extension of the classical orthogonality. It can be shown that if a set of vectors are A-Conjugate, then they are also linearly independent. Thus, as the iteration proceeds conjugate direction/gradient method guarantees that the iterates minimize the given function in subspaces of increasing dimension. It is this expanding subspace property which is a hallmark of this method that guarantees convergence in almost n steps provided that the arithmetic is exact. Conjugate gradient (CG) method is a special class of conjugate direction (CD) method where the mutually A-Conjugate directions are recursively derived using the gradient of the function being minimized.

Type
Chapter
Information
Dynamic Data Assimilation
A Least Squares Approach
, pp. 190 - 208
Publisher: Cambridge University Press
Print publication year: 2006

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
×