Parameter space Kalman smoothers for multi-decadal climate analysis in high resolution coupled Global Circulation Models

In climate reanalyses for multi-decadal or longer scales with coupled atmosphere-ocean General Circulation models (CGCMs) it can be assumed that the growth of prediction errors arises chiefly from imprecisely known model parameters, which have a nonlinear relationship with the climate observations (...

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Main Authors: García-Pintado, Javier, Paul, André
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications (EGU) 2018
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/44321/
https://oceanrep.geomar.de/id/eprint/44321/1/gmd-2018-48.pdf
https://doi.org/10.5194/gmd-2018-48
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spelling ftoceanrep:oai:oceanrep.geomar.de:44321 2023-05-15T16:30:22+02:00 Parameter space Kalman smoothers for multi-decadal climate analysis in high resolution coupled Global Circulation Models García-Pintado, Javier Paul, André 2018 text https://oceanrep.geomar.de/id/eprint/44321/ https://oceanrep.geomar.de/id/eprint/44321/1/gmd-2018-48.pdf https://doi.org/10.5194/gmd-2018-48 en eng Copernicus Publications (EGU) https://oceanrep.geomar.de/id/eprint/44321/1/gmd-2018-48.pdf García-Pintado, J. and Paul, A. (2018) Parameter space Kalman smoothers for multi-decadal climate analysis in high resolution coupled Global Circulation Models. Open Access Geoscientific Model Development Discussions . pp. 1-38. DOI 10.5194/gmd-2018-48 <https://doi.org/10.5194/gmd-2018-48>. doi:10.5194/gmd-2018-48 cc_by_3.0 info:eu-repo/semantics/openAccess Article NonPeerReviewed 2018 ftoceanrep https://doi.org/10.5194/gmd-2018-48 2023-04-07T15:41:22Z In climate reanalyses for multi-decadal or longer scales with coupled atmosphere-ocean General Circulation models (CGCMs) it can be assumed that the growth of prediction errors arises chiefly from imprecisely known model parameters, which have a nonlinear relationship with the climate observations (paleoclimate proxies). Also, high-resolution CGCMs for climate analysis are extremely expensive to run, which constrains the applicability of assimilation schemes. In a model framework where we assume that model dynamic parameters account for (nearly) all forecast errors at observation times, we compare two computationally efficient iterative schemes for approximate nonlinear model parameter estimation and joint flux estimation (taking the specific shape of freshwater from melting in the Greenland ice sheet), and its physically consistent state. First, a trivial adaptation of the strong constraint incremental 4D-Var formulation leads to what we refer to as the parameter space iterative extended Kalman smoother (pIKS); a Gauss-Newton scheme. Second, a so-called parameter space fractional Kalman smoother (pFKS) is an alternative controlled-step line search, which can potentially be a more stable approach. While these iterative schemes have been used in data assimilation, we revisit them together within the context of parameter estimation in climate reanalysis, as compared to the more general 4D-Var formulation. Then, the two schemes are evaluated in numerical experiments with a simple 1D energy balance model (Ebm1D) and with a fully-coupled Community Earth System Model (CESM v1.2). Firstly, with Ebm1D the pFKS obtains a cost function similar to the adjoint method with highly reduced computational cost, while an ensemble transform Kalman filter with an m = 60 ensemble size (ETKF60) behaves slightly worse. The pIKS behaves worse than the ETKF60, but an ETKF10 (m = 10) is even worst. Accordingly, with CESM we evaluate the pKFS and the ETKF60 along with an ETKF with Gaussian Anamorphosis (ETKF-GA60). From all the options, ... Article in Journal/Newspaper Greenland Ice Sheet OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Greenland
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language English
description In climate reanalyses for multi-decadal or longer scales with coupled atmosphere-ocean General Circulation models (CGCMs) it can be assumed that the growth of prediction errors arises chiefly from imprecisely known model parameters, which have a nonlinear relationship with the climate observations (paleoclimate proxies). Also, high-resolution CGCMs for climate analysis are extremely expensive to run, which constrains the applicability of assimilation schemes. In a model framework where we assume that model dynamic parameters account for (nearly) all forecast errors at observation times, we compare two computationally efficient iterative schemes for approximate nonlinear model parameter estimation and joint flux estimation (taking the specific shape of freshwater from melting in the Greenland ice sheet), and its physically consistent state. First, a trivial adaptation of the strong constraint incremental 4D-Var formulation leads to what we refer to as the parameter space iterative extended Kalman smoother (pIKS); a Gauss-Newton scheme. Second, a so-called parameter space fractional Kalman smoother (pFKS) is an alternative controlled-step line search, which can potentially be a more stable approach. While these iterative schemes have been used in data assimilation, we revisit them together within the context of parameter estimation in climate reanalysis, as compared to the more general 4D-Var formulation. Then, the two schemes are evaluated in numerical experiments with a simple 1D energy balance model (Ebm1D) and with a fully-coupled Community Earth System Model (CESM v1.2). Firstly, with Ebm1D the pFKS obtains a cost function similar to the adjoint method with highly reduced computational cost, while an ensemble transform Kalman filter with an m = 60 ensemble size (ETKF60) behaves slightly worse. The pIKS behaves worse than the ETKF60, but an ETKF10 (m = 10) is even worst. Accordingly, with CESM we evaluate the pKFS and the ETKF60 along with an ETKF with Gaussian Anamorphosis (ETKF-GA60). From all the options, ...
format Article in Journal/Newspaper
author García-Pintado, Javier
Paul, André
spellingShingle García-Pintado, Javier
Paul, André
Parameter space Kalman smoothers for multi-decadal climate analysis in high resolution coupled Global Circulation Models
author_facet García-Pintado, Javier
Paul, André
author_sort García-Pintado, Javier
title Parameter space Kalman smoothers for multi-decadal climate analysis in high resolution coupled Global Circulation Models
title_short Parameter space Kalman smoothers for multi-decadal climate analysis in high resolution coupled Global Circulation Models
title_full Parameter space Kalman smoothers for multi-decadal climate analysis in high resolution coupled Global Circulation Models
title_fullStr Parameter space Kalman smoothers for multi-decadal climate analysis in high resolution coupled Global Circulation Models
title_full_unstemmed Parameter space Kalman smoothers for multi-decadal climate analysis in high resolution coupled Global Circulation Models
title_sort parameter space kalman smoothers for multi-decadal climate analysis in high resolution coupled global circulation models
publisher Copernicus Publications (EGU)
publishDate 2018
url https://oceanrep.geomar.de/id/eprint/44321/
https://oceanrep.geomar.de/id/eprint/44321/1/gmd-2018-48.pdf
https://doi.org/10.5194/gmd-2018-48
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_relation https://oceanrep.geomar.de/id/eprint/44321/1/gmd-2018-48.pdf
García-Pintado, J. and Paul, A. (2018) Parameter space Kalman smoothers for multi-decadal climate analysis in high resolution coupled Global Circulation Models. Open Access Geoscientific Model Development Discussions . pp. 1-38. DOI 10.5194/gmd-2018-48 <https://doi.org/10.5194/gmd-2018-48>.
doi:10.5194/gmd-2018-48
op_rights cc_by_3.0
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/gmd-2018-48
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