Impacts of using spectral nudging on regional climate model RCA4 simulations of the Arctic

The performance of the Rossby Centre regional climate model RCA4 is investigated for the Arctic CORDEX (COordinated Regional climate Downscaling EXperiment) region, with an emphasis on its suitability to be coupled to a regional ocean and sea ice model. Large biases in mean sea level pressure (MSLP)...

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Published in:Geoscientific Model Development
Main Authors: Berg, P., Döscher, R., Koenigk, T.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2013
Subjects:
Online Access:https://doi.org/10.5194/gmd-6-849-2013
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spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00022522 2023-05-15T14:56:09+02:00 Impacts of using spectral nudging on regional climate model RCA4 simulations of the Arctic Berg, P. Döscher, R. Koenigk, T. 2013-06 electronic https://doi.org/10.5194/gmd-6-849-2013 https://noa.gwlb.de/receive/cop_mods_00022522 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00022477/gmd-6-849-2013.pdf https://gmd.copernicus.org/articles/6/849/2013/gmd-6-849-2013.pdf eng eng Copernicus Publications Geoscientific Model Development -- http://www.bibliothek.uni-regensburg.de/ezeit/?2456725 -- http://www.geosci-model-dev.net/ -- 1991-9603 https://doi.org/10.5194/gmd-6-849-2013 https://noa.gwlb.de/receive/cop_mods_00022522 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00022477/gmd-6-849-2013.pdf https://gmd.copernicus.org/articles/6/849/2013/gmd-6-849-2013.pdf uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2013 ftnonlinearchiv https://doi.org/10.5194/gmd-6-849-2013 2022-02-08T22:51:04Z The performance of the Rossby Centre regional climate model RCA4 is investigated for the Arctic CORDEX (COordinated Regional climate Downscaling EXperiment) region, with an emphasis on its suitability to be coupled to a regional ocean and sea ice model. Large biases in mean sea level pressure (MSLP) are identified, with pronounced too-high pressure centred over the North Pole in summer of over 5 hPa, and too-low pressure in winter of a similar magnitude. These lead to biases in the surface winds, which will potentially lead to strong sea ice biases in a future coupled system. The large-scale circulation is believed to be the major reason for the biases, and an implementation of spectral nudging is applied to remedy the problems by constraining the large-scale components of the driving fields within the interior domain. It is found that the spectral nudging generally corrects for the MSLP and wind biases, while not significantly affecting other variables, such as surface radiative components, two-metre temperature and precipitation. Article in Journal/Newspaper Arctic North Pole Sea ice Niedersächsisches Online-Archiv NOA Arctic North Pole Geoscientific Model Development 6 3 849 859
institution Open Polar
collection Niedersächsisches Online-Archiv NOA
op_collection_id ftnonlinearchiv
language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Berg, P.
Döscher, R.
Koenigk, T.
Impacts of using spectral nudging on regional climate model RCA4 simulations of the Arctic
topic_facet article
Verlagsveröffentlichung
description The performance of the Rossby Centre regional climate model RCA4 is investigated for the Arctic CORDEX (COordinated Regional climate Downscaling EXperiment) region, with an emphasis on its suitability to be coupled to a regional ocean and sea ice model. Large biases in mean sea level pressure (MSLP) are identified, with pronounced too-high pressure centred over the North Pole in summer of over 5 hPa, and too-low pressure in winter of a similar magnitude. These lead to biases in the surface winds, which will potentially lead to strong sea ice biases in a future coupled system. The large-scale circulation is believed to be the major reason for the biases, and an implementation of spectral nudging is applied to remedy the problems by constraining the large-scale components of the driving fields within the interior domain. It is found that the spectral nudging generally corrects for the MSLP and wind biases, while not significantly affecting other variables, such as surface radiative components, two-metre temperature and precipitation.
format Article in Journal/Newspaper
author Berg, P.
Döscher, R.
Koenigk, T.
author_facet Berg, P.
Döscher, R.
Koenigk, T.
author_sort Berg, P.
title Impacts of using spectral nudging on regional climate model RCA4 simulations of the Arctic
title_short Impacts of using spectral nudging on regional climate model RCA4 simulations of the Arctic
title_full Impacts of using spectral nudging on regional climate model RCA4 simulations of the Arctic
title_fullStr Impacts of using spectral nudging on regional climate model RCA4 simulations of the Arctic
title_full_unstemmed Impacts of using spectral nudging on regional climate model RCA4 simulations of the Arctic
title_sort impacts of using spectral nudging on regional climate model rca4 simulations of the arctic
publisher Copernicus Publications
publishDate 2013
url https://doi.org/10.5194/gmd-6-849-2013
https://noa.gwlb.de/receive/cop_mods_00022522
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00022477/gmd-6-849-2013.pdf
https://gmd.copernicus.org/articles/6/849/2013/gmd-6-849-2013.pdf
geographic Arctic
North Pole
geographic_facet Arctic
North Pole
genre Arctic
North Pole
Sea ice
genre_facet Arctic
North Pole
Sea ice
op_relation Geoscientific Model Development -- http://www.bibliothek.uni-regensburg.de/ezeit/?2456725 -- http://www.geosci-model-dev.net/ -- 1991-9603
https://doi.org/10.5194/gmd-6-849-2013
https://noa.gwlb.de/receive/cop_mods_00022522
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00022477/gmd-6-849-2013.pdf
https://gmd.copernicus.org/articles/6/849/2013/gmd-6-849-2013.pdf
op_rights uneingeschränkt
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op_doi https://doi.org/10.5194/gmd-6-849-2013
container_title Geoscientific Model Development
container_volume 6
container_issue 3
container_start_page 849
op_container_end_page 859
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