Physically-based data assimilation

Ideally, a validation and assimilation scheme should maintain the physical principles embodied in the model and be able to evaluate and assimilate lower dimensional features (e.g., discontinuities) contained within a bulk simulation, even when these features are not directly observed or represented...

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Published in:Geoscientific Model Development
Main Authors: Levy, G., Coon, M., Nguyen, G., Sulsky, D.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/gmd-3-669-2010
https://gmd.copernicus.org/articles/3/669/2010/
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spelling ftcopernicus:oai:publications.copernicus.org:gmd7348 2023-05-15T18:18:19+02:00 Physically-based data assimilation Levy, G. Coon, M. Nguyen, G. Sulsky, D. 2018-09-27 application/pdf https://doi.org/10.5194/gmd-3-669-2010 https://gmd.copernicus.org/articles/3/669/2010/ eng eng doi:10.5194/gmd-3-669-2010 https://gmd.copernicus.org/articles/3/669/2010/ eISSN: 1991-9603 Text 2018 ftcopernicus https://doi.org/10.5194/gmd-3-669-2010 2020-07-20T16:26:17Z Ideally, a validation and assimilation scheme should maintain the physical principles embodied in the model and be able to evaluate and assimilate lower dimensional features (e.g., discontinuities) contained within a bulk simulation, even when these features are not directly observed or represented by model variables. We present such a scheme and suggest its potential to resolve or alleviate some outstanding problems that stem from making and applying required, yet often non-physical, assumptions and procedures in common operational data assimilation. As proof of concept, we use a sea-ice model with remotely sensed observations of leads in a one-step assimilation cycle. Using the new scheme in a sixteen day simulation experiment introduces model skill (against persistence) several days earlier than in the control run, improves the overall model skill and delays its drop off at later stages of the simulation. The potential and requirements to extend this scheme to different applications, and to both empirical and statistical multivariate and full cycle data assimilation schemes, are discussed. Text Sea ice Copernicus Publications: E-Journals Geoscientific Model Development 3 2 669 677
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Ideally, a validation and assimilation scheme should maintain the physical principles embodied in the model and be able to evaluate and assimilate lower dimensional features (e.g., discontinuities) contained within a bulk simulation, even when these features are not directly observed or represented by model variables. We present such a scheme and suggest its potential to resolve or alleviate some outstanding problems that stem from making and applying required, yet often non-physical, assumptions and procedures in common operational data assimilation. As proof of concept, we use a sea-ice model with remotely sensed observations of leads in a one-step assimilation cycle. Using the new scheme in a sixteen day simulation experiment introduces model skill (against persistence) several days earlier than in the control run, improves the overall model skill and delays its drop off at later stages of the simulation. The potential and requirements to extend this scheme to different applications, and to both empirical and statistical multivariate and full cycle data assimilation schemes, are discussed.
format Text
author Levy, G.
Coon, M.
Nguyen, G.
Sulsky, D.
spellingShingle Levy, G.
Coon, M.
Nguyen, G.
Sulsky, D.
Physically-based data assimilation
author_facet Levy, G.
Coon, M.
Nguyen, G.
Sulsky, D.
author_sort Levy, G.
title Physically-based data assimilation
title_short Physically-based data assimilation
title_full Physically-based data assimilation
title_fullStr Physically-based data assimilation
title_full_unstemmed Physically-based data assimilation
title_sort physically-based data assimilation
publishDate 2018
url https://doi.org/10.5194/gmd-3-669-2010
https://gmd.copernicus.org/articles/3/669/2010/
genre Sea ice
genre_facet Sea ice
op_source eISSN: 1991-9603
op_relation doi:10.5194/gmd-3-669-2010
https://gmd.copernicus.org/articles/3/669/2010/
op_doi https://doi.org/10.5194/gmd-3-669-2010
container_title Geoscientific Model Development
container_volume 3
container_issue 2
container_start_page 669
op_container_end_page 677
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