Coupled regional Earth system modeling in the Baltic Sea region
Nonlinear responses to externally forced climate change are known to dampen or amplify the local climate impact due to complex cross-compartmental feedback loops in the Earth system. These feedbacks are less well represented in the traditional stand-alone atmosphere and ocean models on which many of...
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ftdoajarticles:oai:doaj.org/article:ead028a97a8d4b77afddb32b88c48ac1 2023-05-15T18:18:53+02:00 Coupled regional Earth system modeling in the Baltic Sea region M. Gröger C. Dieterich J. Haapala H. T. M. Ho-Hagemann S. Hagemann J. Jakacki W. May H. E. M. Meier P. A. Miller A. Rutgersson L. Wu 2021-09-01T00:00:00Z https://doi.org/10.5194/esd-12-939-2021 https://doaj.org/article/ead028a97a8d4b77afddb32b88c48ac1 EN eng Copernicus Publications https://esd.copernicus.org/articles/12/939/2021/esd-12-939-2021.pdf https://doaj.org/toc/2190-4979 https://doaj.org/toc/2190-4987 doi:10.5194/esd-12-939-2021 2190-4979 2190-4987 https://doaj.org/article/ead028a97a8d4b77afddb32b88c48ac1 Earth System Dynamics, Vol 12, Pp 939-973 (2021) Science Q Geology QE1-996.5 Dynamic and structural geology QE500-639.5 article 2021 ftdoajarticles https://doi.org/10.5194/esd-12-939-2021 2022-12-31T14:35:12Z Nonlinear responses to externally forced climate change are known to dampen or amplify the local climate impact due to complex cross-compartmental feedback loops in the Earth system. These feedbacks are less well represented in the traditional stand-alone atmosphere and ocean models on which many of today's regional climate assessments rely (e.g., EURO-CORDEX, NOSCCA and BACC II). This has promoted the development of regional climate models for the Baltic Sea region by coupling different compartments of the Earth system into more comprehensive models. Coupled models more realistically represent feedback loops than the information imposed on the region by prescribed boundary conditions and, thus, permit more degrees of freedom. In the past, several coupled model systems have been developed for Europe and the Baltic Sea region. This article reviews recent progress on model systems that allow two-way communication between atmosphere and ocean models; models for the land surface, including the terrestrial biosphere; and wave models at the air–sea interface and hydrology models for water cycle closure. However, several processes that have mostly been realized by one-way coupling to date, such as marine biogeochemistry, nutrient cycling and atmospheric chemistry (e.g., aerosols), are not considered here. In contrast to uncoupled stand-alone models, coupled Earth system models can modify mean near-surface air temperatures locally by up to several degrees compared with their stand-alone atmospheric counterparts using prescribed surface boundary conditions. The representation of small-scale oceanic processes, such as vertical mixing and sea-ice dynamics, appears essential to accurately resolve the air–sea heat exchange over the Baltic Sea, and these parameters can only be provided by online coupled high-resolution ocean models. In addition, the coupling of wave models at the ocean–atmosphere interface allows for a more explicit formulation of small-scale to microphysical processes with local feedbacks to water ... Article in Journal/Newspaper Sea ice Directory of Open Access Journals: DOAJ Articles Earth System Dynamics 12 3 939 973 |
institution |
Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Science Q Geology QE1-996.5 Dynamic and structural geology QE500-639.5 |
spellingShingle |
Science Q Geology QE1-996.5 Dynamic and structural geology QE500-639.5 M. Gröger C. Dieterich J. Haapala H. T. M. Ho-Hagemann S. Hagemann J. Jakacki W. May H. E. M. Meier P. A. Miller A. Rutgersson L. Wu Coupled regional Earth system modeling in the Baltic Sea region |
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Science Q Geology QE1-996.5 Dynamic and structural geology QE500-639.5 |
description |
Nonlinear responses to externally forced climate change are known to dampen or amplify the local climate impact due to complex cross-compartmental feedback loops in the Earth system. These feedbacks are less well represented in the traditional stand-alone atmosphere and ocean models on which many of today's regional climate assessments rely (e.g., EURO-CORDEX, NOSCCA and BACC II). This has promoted the development of regional climate models for the Baltic Sea region by coupling different compartments of the Earth system into more comprehensive models. Coupled models more realistically represent feedback loops than the information imposed on the region by prescribed boundary conditions and, thus, permit more degrees of freedom. In the past, several coupled model systems have been developed for Europe and the Baltic Sea region. This article reviews recent progress on model systems that allow two-way communication between atmosphere and ocean models; models for the land surface, including the terrestrial biosphere; and wave models at the air–sea interface and hydrology models for water cycle closure. However, several processes that have mostly been realized by one-way coupling to date, such as marine biogeochemistry, nutrient cycling and atmospheric chemistry (e.g., aerosols), are not considered here. In contrast to uncoupled stand-alone models, coupled Earth system models can modify mean near-surface air temperatures locally by up to several degrees compared with their stand-alone atmospheric counterparts using prescribed surface boundary conditions. The representation of small-scale oceanic processes, such as vertical mixing and sea-ice dynamics, appears essential to accurately resolve the air–sea heat exchange over the Baltic Sea, and these parameters can only be provided by online coupled high-resolution ocean models. In addition, the coupling of wave models at the ocean–atmosphere interface allows for a more explicit formulation of small-scale to microphysical processes with local feedbacks to water ... |
format |
Article in Journal/Newspaper |
author |
M. Gröger C. Dieterich J. Haapala H. T. M. Ho-Hagemann S. Hagemann J. Jakacki W. May H. E. M. Meier P. A. Miller A. Rutgersson L. Wu |
author_facet |
M. Gröger C. Dieterich J. Haapala H. T. M. Ho-Hagemann S. Hagemann J. Jakacki W. May H. E. M. Meier P. A. Miller A. Rutgersson L. Wu |
author_sort |
M. Gröger |
title |
Coupled regional Earth system modeling in the Baltic Sea region |
title_short |
Coupled regional Earth system modeling in the Baltic Sea region |
title_full |
Coupled regional Earth system modeling in the Baltic Sea region |
title_fullStr |
Coupled regional Earth system modeling in the Baltic Sea region |
title_full_unstemmed |
Coupled regional Earth system modeling in the Baltic Sea region |
title_sort |
coupled regional earth system modeling in the baltic sea region |
publisher |
Copernicus Publications |
publishDate |
2021 |
url |
https://doi.org/10.5194/esd-12-939-2021 https://doaj.org/article/ead028a97a8d4b77afddb32b88c48ac1 |
genre |
Sea ice |
genre_facet |
Sea ice |
op_source |
Earth System Dynamics, Vol 12, Pp 939-973 (2021) |
op_relation |
https://esd.copernicus.org/articles/12/939/2021/esd-12-939-2021.pdf https://doaj.org/toc/2190-4979 https://doaj.org/toc/2190-4987 doi:10.5194/esd-12-939-2021 2190-4979 2190-4987 https://doaj.org/article/ead028a97a8d4b77afddb32b88c48ac1 |
op_doi |
https://doi.org/10.5194/esd-12-939-2021 |
container_title |
Earth System Dynamics |
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12 |
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3 |
container_start_page |
939 |
op_container_end_page |
973 |
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