Open ocean deep convection, Mediterranean and Greenland Seas
Recent observations within deep convection regimes of the Gulf of Lions and Greenland Sea all confirm the existence of small-scale plumes of only a few 100 m horizontal scale during cooling periods, in agreement with scaling arguments and non-hydrostatic modelling results. The integral effect of the...
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ftoceanrep:oai:oceanrep.geomar.de:1013 2024-09-30T14:35:42+00:00 Open ocean deep convection, Mediterranean and Greenland Seas Schott, Friedrich Visbeck, Martin Send, Uwe Rizzoli, P. Robinson, A. 1994 text https://oceanrep.geomar.de/id/eprint/1013/ https://oceanrep.geomar.de/id/eprint/1013/1/20180507171350.pdf en eng Kluwer https://oceanrep.geomar.de/id/eprint/1013/1/20180507171350.pdf Schott, F., Visbeck, M. and Send, U. (1994) Open ocean deep convection, Mediterranean and Greenland Seas. Open Access In: Ocean processes in climate dynamics: Global and Mediterranean examples. , ed. by Rizzoli, P. and Robinson, A. Kluwer, Alphen aan den Rijn, Netherlands, pp. 203-225. ISBN 978-94-010-4376-2 info:eu-repo/semantics/openAccess Book chapter NonPeerReviewed 1994 ftoceanrep 2024-09-04T05:04:40Z Recent observations within deep convection regimes of the Gulf of Lions and Greenland Sea all confirm the existence of small-scale plumes of only a few 100 m horizontal scale during cooling periods, in agreement with scaling arguments and non-hydrostatic modelling results. The integral effect of the plumes is that of a mixing agent rather than carrying water downward in a mean motion. It depends on the intensity and duration of the cooling how complete the mixing within the depth range of the plumes is. In the Greenland Sea, the role of the ice through brine rejection was found to be important in the preconditioning period (November - February) rather than for the deep convection itself (March) which occurred when the water was ice-free. After the convection period water masses are exchanged with the environment through baroclinic instability, causing increased deep T,S variance on a larger scale that continues to exist well into the next summer, allowing identification of previous-winter convection activity Book Part Greenland Greenland Sea OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Greenland |
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Open Polar |
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OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
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ftoceanrep |
language |
English |
description |
Recent observations within deep convection regimes of the Gulf of Lions and Greenland Sea all confirm the existence of small-scale plumes of only a few 100 m horizontal scale during cooling periods, in agreement with scaling arguments and non-hydrostatic modelling results. The integral effect of the plumes is that of a mixing agent rather than carrying water downward in a mean motion. It depends on the intensity and duration of the cooling how complete the mixing within the depth range of the plumes is. In the Greenland Sea, the role of the ice through brine rejection was found to be important in the preconditioning period (November - February) rather than for the deep convection itself (March) which occurred when the water was ice-free. After the convection period water masses are exchanged with the environment through baroclinic instability, causing increased deep T,S variance on a larger scale that continues to exist well into the next summer, allowing identification of previous-winter convection activity |
author2 |
Rizzoli, P. Robinson, A. |
format |
Book Part |
author |
Schott, Friedrich Visbeck, Martin Send, Uwe |
spellingShingle |
Schott, Friedrich Visbeck, Martin Send, Uwe Open ocean deep convection, Mediterranean and Greenland Seas |
author_facet |
Schott, Friedrich Visbeck, Martin Send, Uwe |
author_sort |
Schott, Friedrich |
title |
Open ocean deep convection, Mediterranean and Greenland Seas |
title_short |
Open ocean deep convection, Mediterranean and Greenland Seas |
title_full |
Open ocean deep convection, Mediterranean and Greenland Seas |
title_fullStr |
Open ocean deep convection, Mediterranean and Greenland Seas |
title_full_unstemmed |
Open ocean deep convection, Mediterranean and Greenland Seas |
title_sort |
open ocean deep convection, mediterranean and greenland seas |
publisher |
Kluwer |
publishDate |
1994 |
url |
https://oceanrep.geomar.de/id/eprint/1013/ https://oceanrep.geomar.de/id/eprint/1013/1/20180507171350.pdf |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Greenland Sea |
genre_facet |
Greenland Greenland Sea |
op_relation |
https://oceanrep.geomar.de/id/eprint/1013/1/20180507171350.pdf Schott, F., Visbeck, M. and Send, U. (1994) Open ocean deep convection, Mediterranean and Greenland Seas. Open Access In: Ocean processes in climate dynamics: Global and Mediterranean examples. , ed. by Rizzoli, P. and Robinson, A. Kluwer, Alphen aan den Rijn, Netherlands, pp. 203-225. ISBN 978-94-010-4376-2 |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1811638958508998656 |