A non-Gaussian analysis scheme using rank histograms for ensemble data assimilation
One challenge of geophysical data assimilation is to address the issue of non-Gaussianities in the distributions of the physical variables ensuing, in many cases, from nonlinear dynamical models. Non-Gaussian ensemble analysis methods fall into two categories, those remapping the ensemble particles...
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2014-08-01
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doaj-e64b69a2e7014f7d82af187b93b4935a2020-11-24T22:26:00ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462014-08-0121486988510.5194/npg-21-869-2014A non-Gaussian analysis scheme using rank histograms for ensemble data assimilationS. Metref0E. Cosme1C. Snyder2P. Brasseur3CNRS – Univ. Grenoble Alpes, LGGE (UMR5183), 38041 Grenoble, FranceCNRS – Univ. Grenoble Alpes, LGGE (UMR5183), 38041 Grenoble, FranceNational Center for Atmospheric Research, Boulder, Colorado, USACNRS – Univ. Grenoble Alpes, LGGE (UMR5183), 38041 Grenoble, FranceOne challenge of geophysical data assimilation is to address the issue of non-Gaussianities in the distributions of the physical variables ensuing, in many cases, from nonlinear dynamical models. Non-Gaussian ensemble analysis methods fall into two categories, those remapping the ensemble particles by approximating the best linear unbiased estimate, for example, the ensemble Kalman filter (EnKF), and those resampling the particles by directly applying Bayes' rule, like particle filters. In this article, it is suggested that the most common remapping methods can only handle weakly non-Gaussian distributions, while the others suffer from sampling issues. In between those two categories, a new remapping method directly applying Bayes' rule, the multivariate rank histogram filter (MRHF), is introduced as an extension of the rank histogram filter (RHF) first introduced by Anderson (2010). Its performance is evaluated and compared with several data assimilation methods, on different levels of non-Gaussianity with the Lorenz 63 model. The method's behavior is then illustrated on a simple density estimation problem using ensemble simulations from a coupled physical–biogeochemical model of the North Atlantic ocean. The MRHF performs well with low-dimensional systems in strongly non-Gaussian regimes.http://www.nonlin-processes-geophys.net/21/869/2014/npg-21-869-2014.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
S. Metref E. Cosme C. Snyder P. Brasseur |
spellingShingle |
S. Metref E. Cosme C. Snyder P. Brasseur A non-Gaussian analysis scheme using rank histograms for ensemble data assimilation Nonlinear Processes in Geophysics |
author_facet |
S. Metref E. Cosme C. Snyder P. Brasseur |
author_sort |
S. Metref |
title |
A non-Gaussian analysis scheme using rank histograms for ensemble data assimilation |
title_short |
A non-Gaussian analysis scheme using rank histograms for ensemble data assimilation |
title_full |
A non-Gaussian analysis scheme using rank histograms for ensemble data assimilation |
title_fullStr |
A non-Gaussian analysis scheme using rank histograms for ensemble data assimilation |
title_full_unstemmed |
A non-Gaussian analysis scheme using rank histograms for ensemble data assimilation |
title_sort |
non-gaussian analysis scheme using rank histograms for ensemble data assimilation |
publisher |
Copernicus Publications |
series |
Nonlinear Processes in Geophysics |
issn |
1023-5809 1607-7946 |
publishDate |
2014-08-01 |
description |
One challenge of geophysical data assimilation is to address the issue of
non-Gaussianities in the distributions of the physical variables ensuing, in
many cases, from nonlinear dynamical models. Non-Gaussian ensemble analysis
methods fall into two categories, those remapping the ensemble particles by
approximating the best linear unbiased estimate, for example, the ensemble Kalman
filter (EnKF), and those resampling the particles by directly applying Bayes'
rule, like particle filters. In this article, it is suggested that the most
common remapping methods can only handle weakly non-Gaussian distributions,
while the others suffer from sampling issues. In between those two
categories, a new remapping method directly applying Bayes' rule, the
multivariate rank histogram filter (MRHF), is introduced as an extension of
the rank histogram filter (RHF) first introduced by Anderson (2010). Its
performance is evaluated and compared with several data assimilation methods,
on different levels of non-Gaussianity with the Lorenz 63 model. The method's
behavior is then illustrated on a simple density estimation problem using
ensemble simulations from a coupled physical–biogeochemical model of the
North Atlantic ocean. The MRHF performs well with low-dimensional systems in
strongly non-Gaussian regimes. |
url |
http://www.nonlin-processes-geophys.net/21/869/2014/npg-21-869-2014.pdf |
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