Water mass formation from revised COADS data
Surface heat and freshwater fluxes from the Comprehensive 0cean-Atmosphere Data Set are revised and used diagnostically to compute air-sea transformation rates on density, temperature, and salinity classes over the domain of the data. Maximum rates occur over the warmest water and over mode waters,...
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AMS (American Meteorological Society)
1995
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ftoceanrep:oai:oceanrep.geomar.de:3778 2024-09-30T14:39:28+00:00 Water mass formation from revised COADS data Speer, K. G. Isemer, H.-J. Biastoch, Arne 1995 text https://oceanrep.geomar.de/id/eprint/3778/ https://oceanrep.geomar.de/id/eprint/3778/1/1520-0485%281995%29025_2444_wmffrc_2.0.co%3B2-1.pdf https://doi.org/10.1175/1520-0485(1995)025<2444:WMFFRC>2.0.CO;2 en eng AMS (American Meteorological Society) https://oceanrep.geomar.de/id/eprint/3778/1/1520-0485%281995%29025_2444_wmffrc_2.0.co%3B2-1.pdf Speer, K. G., Isemer, H. J. and Biastoch, A. (1995) Water mass formation from revised COADS data. Open Access Journal of Physical Oceanography, 25 (10). pp. 2444-2457. DOI 10.1175/1520-0485(1995)025<2444:WMFFRC>2.0.CO;2 <https://doi.org/10.1175/1520-0485%281995%29025%3C2444%3AWMFFRC%3E2.0.CO%3B2>. doi:10.1175/1520-0485(1995)025<2444:WMFFRC>2.0.CO;2 info:eu-repo/semantics/openAccess Article PeerReviewed 1995 ftoceanrep https://doi.org/10.1175/1520-0485(1995)025<2444:WMFFRC>2.0.CO;2 2024-09-04T05:04:40Z Surface heat and freshwater fluxes from the Comprehensive 0cean-Atmosphere Data Set are revised and used diagnostically to compute air-sea transformation rates on density, temperature, and salinity classes over the domain of the data. Maximum rates occur over the warmest water and over mode waters, which are the dominant result of air-sea interaction. Transformation in different is accordingly distinguished by temperature and salinity, just as water masses in different oceans are so distinguished. Over the entire domain, to about 30°S, approximately 80×106 m3 s−1 of warm cool water are transformed by air-sea fluxes, on annual average. Calculations for several seas in the North Atlantic, where deep water is thought to originate, we also presented. Article in Journal/Newspaper North Atlantic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
Surface heat and freshwater fluxes from the Comprehensive 0cean-Atmosphere Data Set are revised and used diagnostically to compute air-sea transformation rates on density, temperature, and salinity classes over the domain of the data. Maximum rates occur over the warmest water and over mode waters, which are the dominant result of air-sea interaction. Transformation in different is accordingly distinguished by temperature and salinity, just as water masses in different oceans are so distinguished. Over the entire domain, to about 30°S, approximately 80×106 m3 s−1 of warm cool water are transformed by air-sea fluxes, on annual average. Calculations for several seas in the North Atlantic, where deep water is thought to originate, we also presented. |
format |
Article in Journal/Newspaper |
author |
Speer, K. G. Isemer, H.-J. Biastoch, Arne |
spellingShingle |
Speer, K. G. Isemer, H.-J. Biastoch, Arne Water mass formation from revised COADS data |
author_facet |
Speer, K. G. Isemer, H.-J. Biastoch, Arne |
author_sort |
Speer, K. G. |
title |
Water mass formation from revised COADS data |
title_short |
Water mass formation from revised COADS data |
title_full |
Water mass formation from revised COADS data |
title_fullStr |
Water mass formation from revised COADS data |
title_full_unstemmed |
Water mass formation from revised COADS data |
title_sort |
water mass formation from revised coads data |
publisher |
AMS (American Meteorological Society) |
publishDate |
1995 |
url |
https://oceanrep.geomar.de/id/eprint/3778/ https://oceanrep.geomar.de/id/eprint/3778/1/1520-0485%281995%29025_2444_wmffrc_2.0.co%3B2-1.pdf https://doi.org/10.1175/1520-0485(1995)025<2444:WMFFRC>2.0.CO;2 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://oceanrep.geomar.de/id/eprint/3778/1/1520-0485%281995%29025_2444_wmffrc_2.0.co%3B2-1.pdf Speer, K. G., Isemer, H. J. and Biastoch, A. (1995) Water mass formation from revised COADS data. Open Access Journal of Physical Oceanography, 25 (10). pp. 2444-2457. DOI 10.1175/1520-0485(1995)025<2444:WMFFRC>2.0.CO;2 <https://doi.org/10.1175/1520-0485%281995%29025%3C2444%3AWMFFRC%3E2.0.CO%3B2>. doi:10.1175/1520-0485(1995)025<2444:WMFFRC>2.0.CO;2 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1175/1520-0485(1995)025<2444:WMFFRC>2.0.CO;2 |
_version_ |
1811642064778035200 |