The linearisation of maps in data assimilation

For the purpose of linearising maps in data assimilation, the tangent-linear approximation is often used. We compare this with the use of the ‘best linear’ approximation, which is the linear map that minimises the mean square error. As a benchmark, we use minimum variance filte...

Full description

Bibliographic Details
Main Author: Timothy J. Payne
Format: Article
Language:English
Published: Taylor & Francis Group 2013-04-01
Series:Tellus: Series A, Dynamic Meteorology and Oceanography
Subjects:
Online Access:http://www.tellusa.net/index.php/tellusa/article/download/18840/pdf_1
id doaj-758db1fee22f4c819bb1ca9b8734226a
record_format Article
spelling doaj-758db1fee22f4c819bb1ca9b8734226a2020-11-24T21:55:28ZengTaylor & Francis GroupTellus: Series A, Dynamic Meteorology and Oceanography0280-64951600-08702013-04-0165011510.3402/tellusa.v65i0.18840The linearisation of maps in data assimilationTimothy J. PayneFor the purpose of linearising maps in data assimilation, the tangent-linear approximation is often used. We compare this with the use of the ‘best linear’ approximation, which is the linear map that minimises the mean square error. As a benchmark, we use minimum variance filters and smoothers which are non-linear generalisations of Kalman filters and smoothers. We show that use of the best linear approximation leads to a filter whose prior has first moment unapproximated compared with the benchmark, and second moment whose departure from the benchmark is bounded independently of the derivative of the map, with similar results for smoothers. This is particularly advantageous where the maps in question are strongly non-linear on the scale of the increments. Furthermore, the best linear approximation works equally well for maps which are non-differentiable. We illustrate the results with examples using low-dimensional chaotic maps.http://www.tellusa.net/index.php/tellusa/article/download/18840/pdf_1tangent-linear approximationincremental 4D-Varextended Kalman smoother
collection DOAJ
language English
format Article
sources DOAJ
author Timothy J. Payne
spellingShingle Timothy J. Payne
The linearisation of maps in data assimilation
Tellus: Series A, Dynamic Meteorology and Oceanography
tangent-linear approximation
incremental 4D-Var
extended Kalman smoother
author_facet Timothy J. Payne
author_sort Timothy J. Payne
title The linearisation of maps in data assimilation
title_short The linearisation of maps in data assimilation
title_full The linearisation of maps in data assimilation
title_fullStr The linearisation of maps in data assimilation
title_full_unstemmed The linearisation of maps in data assimilation
title_sort linearisation of maps in data assimilation
publisher Taylor & Francis Group
series Tellus: Series A, Dynamic Meteorology and Oceanography
issn 0280-6495
1600-0870
publishDate 2013-04-01
description For the purpose of linearising maps in data assimilation, the tangent-linear approximation is often used. We compare this with the use of the ‘best linear’ approximation, which is the linear map that minimises the mean square error. As a benchmark, we use minimum variance filters and smoothers which are non-linear generalisations of Kalman filters and smoothers. We show that use of the best linear approximation leads to a filter whose prior has first moment unapproximated compared with the benchmark, and second moment whose departure from the benchmark is bounded independently of the derivative of the map, with similar results for smoothers. This is particularly advantageous where the maps in question are strongly non-linear on the scale of the increments. Furthermore, the best linear approximation works equally well for maps which are non-differentiable. We illustrate the results with examples using low-dimensional chaotic maps.
topic tangent-linear approximation
incremental 4D-Var
extended Kalman smoother
url http://www.tellusa.net/index.php/tellusa/article/download/18840/pdf_1
work_keys_str_mv AT timothyjpayne thelinearisationofmapsindataassimilation
AT timothyjpayne linearisationofmapsindataassimilation
_version_ 1725862529496776704