Validation of surface fluxes in climate simulations of the Arctic with the regional model REMO
To study the variability of the thermohaline circulation in the North Atlantic on decadal time scales, the atmospheric regional model REMO is currently investigated as a component of a fully-coupled atmosphere–ice–ocean model for the Arctic/North Atlantic. A comparison of a 5-year uncoupled simulati...
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ftoceanrep:oai:oceanrep.geomar.de:1350 2024-09-30T14:28:03+00:00 Validation of surface fluxes in climate simulations of the Arctic with the regional model REMO Jürrens, Rolf 1999 text https://oceanrep.geomar.de/id/eprint/1350/ https://oceanrep.geomar.de/id/eprint/1350/1/14488-42456-1-SM.pdf https://doi.org/10.1034/j.1600-0870.1999.00012.x en eng Taylor & Francis https://oceanrep.geomar.de/id/eprint/1350/1/14488-42456-1-SM.pdf Jürrens, R. (1999) Validation of surface fluxes in climate simulations of the Arctic with the regional model REMO. Open Access Tellus A: Dynamic meteorology and oceanography, 51 (5). pp. 698-710. DOI 10.1034/j.1600-0870.1999.00012.x <https://doi.org/10.1034/j.1600-0870.1999.00012.x>. doi:10.1034/j.1600-0870.1999.00012.x info:eu-repo/semantics/openAccess Article PeerReviewed 1999 ftoceanrep https://doi.org/10.1034/j.1600-0870.1999.00012.x 2024-09-04T05:04:40Z To study the variability of the thermohaline circulation in the North Atlantic on decadal time scales, the atmospheric regional model REMO is currently investigated as a component of a fully-coupled atmosphere–ice–ocean model for the Arctic/North Atlantic. A comparison of a 5-year uncoupled simulation of the regional model with a 5-year NCEP/NCAR reanalysis period is carried out in order to assess the performance of the regional model in polar and subpolar regions. The model simulates basic structures realistically. It performs well in middle latitudes but shows some problems in the region of the marginal ice zone and in continental regions with extreme temperature amplitudes. The high elevations of Greenland in the central part of the model domain give rise to problems in the model dynamics, resulting in moderate deviations from NCEP/NCAR reanalysis. Article in Journal/Newspaper Arctic Arctic Greenland North Atlantic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Arctic Greenland Remo ENVELOPE(-128.718,-128.718,54.496,54.496) Tellus A 51 5 698 709 |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
To study the variability of the thermohaline circulation in the North Atlantic on decadal time scales, the atmospheric regional model REMO is currently investigated as a component of a fully-coupled atmosphere–ice–ocean model for the Arctic/North Atlantic. A comparison of a 5-year uncoupled simulation of the regional model with a 5-year NCEP/NCAR reanalysis period is carried out in order to assess the performance of the regional model in polar and subpolar regions. The model simulates basic structures realistically. It performs well in middle latitudes but shows some problems in the region of the marginal ice zone and in continental regions with extreme temperature amplitudes. The high elevations of Greenland in the central part of the model domain give rise to problems in the model dynamics, resulting in moderate deviations from NCEP/NCAR reanalysis. |
format |
Article in Journal/Newspaper |
author |
Jürrens, Rolf |
spellingShingle |
Jürrens, Rolf Validation of surface fluxes in climate simulations of the Arctic with the regional model REMO |
author_facet |
Jürrens, Rolf |
author_sort |
Jürrens, Rolf |
title |
Validation of surface fluxes in climate simulations of the Arctic with the regional model REMO |
title_short |
Validation of surface fluxes in climate simulations of the Arctic with the regional model REMO |
title_full |
Validation of surface fluxes in climate simulations of the Arctic with the regional model REMO |
title_fullStr |
Validation of surface fluxes in climate simulations of the Arctic with the regional model REMO |
title_full_unstemmed |
Validation of surface fluxes in climate simulations of the Arctic with the regional model REMO |
title_sort |
validation of surface fluxes in climate simulations of the arctic with the regional model remo |
publisher |
Taylor & Francis |
publishDate |
1999 |
url |
https://oceanrep.geomar.de/id/eprint/1350/ https://oceanrep.geomar.de/id/eprint/1350/1/14488-42456-1-SM.pdf https://doi.org/10.1034/j.1600-0870.1999.00012.x |
long_lat |
ENVELOPE(-128.718,-128.718,54.496,54.496) |
geographic |
Arctic Greenland Remo |
geographic_facet |
Arctic Greenland Remo |
genre |
Arctic Arctic Greenland North Atlantic |
genre_facet |
Arctic Arctic Greenland North Atlantic |
op_relation |
https://oceanrep.geomar.de/id/eprint/1350/1/14488-42456-1-SM.pdf Jürrens, R. (1999) Validation of surface fluxes in climate simulations of the Arctic with the regional model REMO. Open Access Tellus A: Dynamic meteorology and oceanography, 51 (5). pp. 698-710. DOI 10.1034/j.1600-0870.1999.00012.x <https://doi.org/10.1034/j.1600-0870.1999.00012.x>. doi:10.1034/j.1600-0870.1999.00012.x |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1034/j.1600-0870.1999.00012.x |
container_title |
Tellus A |
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51 |
container_issue |
5 |
container_start_page |
698 |
op_container_end_page |
709 |
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1811633906522259456 |