Arctic Ocean Eddies and Baroclinic Instability.
Baroclinic eddies with diameters of about 10 km and maximum current speeds of about 50 cm/s have been widely observed in the central Arctic Ocean north of Alaska and Canada. The possible origin of these eddies through an instability of the mean baroclinic flow is investigated using an ocean model wi...
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ftdtic:ADA101620 2023-05-15T14:47:08+02:00 Arctic Ocean Eddies and Baroclinic Instability. Hunkins,Kenneth LAMONT-DOHERTY GEOLOGICAL OBSERVATORY PALISADES NY 1981-07 text/html http://www.dtic.mil/docs/citations/ADA101620 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA101620 en eng http://www.dtic.mil/docs/citations/ADA101620 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography Fluid Mechanics *OCEAN CURRENTS *ARCTIC OCEAN SHEAR PROPERTIES VELOCITY SOURCES WATER FLOW VORTICES VARIABLES PROFILES DIFFUSION OCEAN MODELS CIRCULATION SHALLOW DEPTH *Eddies(Ocean currents) Baroclinic instability Baroclinic eddies Geostrophic currents Ice cover Ekman pumping Mesoscale currents WUNR307359 Text 1981 ftdtic 2016-02-20T20:13:40Z Baroclinic eddies with diameters of about 10 km and maximum current speeds of about 50 cm/s have been widely observed in the central Arctic Ocean north of Alaska and Canada. The possible origin of these eddies through an instability of the mean baroclinic flow is investigated using an ocean model with exponential profiles of mean shear and Vaisala frequency. The model includes Ekman pumping at a rigid bottom and at either a free or rigid upper surface. The central Arctic Ocean where the eddies were found is baroclinically stable with no possibility of eddy production. If the eddies are spawned by this mechanism, they must be formed at a site far from where they were observed. On the periphery of the Arctic Ocean north of Alaska the combination of greater current shear, shallower depth and lack of ice cover leads to unstable conditions and the eddies apparently originate in that region. The instability theory predicts maximum velocity at the surface instead of below the surface as observed. Apparently after formation in open water the eddies are advected beneath the ice cover and dissipate the momentum of their upper layers against the ice. This is demonstrated by calculations for the diffusion of vorticity against the ice in the case of an initial exponential profile. A subsurface maximum then develops which resembles the observed profiles. (Author) Text Arctic Arctic Ocean Central Arctic Alaska Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Canada |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Physical and Dynamic Oceanography Fluid Mechanics *OCEAN CURRENTS *ARCTIC OCEAN SHEAR PROPERTIES VELOCITY SOURCES WATER FLOW VORTICES VARIABLES PROFILES DIFFUSION OCEAN MODELS CIRCULATION SHALLOW DEPTH *Eddies(Ocean currents) Baroclinic instability Baroclinic eddies Geostrophic currents Ice cover Ekman pumping Mesoscale currents WUNR307359 |
spellingShingle |
Physical and Dynamic Oceanography Fluid Mechanics *OCEAN CURRENTS *ARCTIC OCEAN SHEAR PROPERTIES VELOCITY SOURCES WATER FLOW VORTICES VARIABLES PROFILES DIFFUSION OCEAN MODELS CIRCULATION SHALLOW DEPTH *Eddies(Ocean currents) Baroclinic instability Baroclinic eddies Geostrophic currents Ice cover Ekman pumping Mesoscale currents WUNR307359 Hunkins,Kenneth Arctic Ocean Eddies and Baroclinic Instability. |
topic_facet |
Physical and Dynamic Oceanography Fluid Mechanics *OCEAN CURRENTS *ARCTIC OCEAN SHEAR PROPERTIES VELOCITY SOURCES WATER FLOW VORTICES VARIABLES PROFILES DIFFUSION OCEAN MODELS CIRCULATION SHALLOW DEPTH *Eddies(Ocean currents) Baroclinic instability Baroclinic eddies Geostrophic currents Ice cover Ekman pumping Mesoscale currents WUNR307359 |
description |
Baroclinic eddies with diameters of about 10 km and maximum current speeds of about 50 cm/s have been widely observed in the central Arctic Ocean north of Alaska and Canada. The possible origin of these eddies through an instability of the mean baroclinic flow is investigated using an ocean model with exponential profiles of mean shear and Vaisala frequency. The model includes Ekman pumping at a rigid bottom and at either a free or rigid upper surface. The central Arctic Ocean where the eddies were found is baroclinically stable with no possibility of eddy production. If the eddies are spawned by this mechanism, they must be formed at a site far from where they were observed. On the periphery of the Arctic Ocean north of Alaska the combination of greater current shear, shallower depth and lack of ice cover leads to unstable conditions and the eddies apparently originate in that region. The instability theory predicts maximum velocity at the surface instead of below the surface as observed. Apparently after formation in open water the eddies are advected beneath the ice cover and dissipate the momentum of their upper layers against the ice. This is demonstrated by calculations for the diffusion of vorticity against the ice in the case of an initial exponential profile. A subsurface maximum then develops which resembles the observed profiles. (Author) |
author2 |
LAMONT-DOHERTY GEOLOGICAL OBSERVATORY PALISADES NY |
format |
Text |
author |
Hunkins,Kenneth |
author_facet |
Hunkins,Kenneth |
author_sort |
Hunkins,Kenneth |
title |
Arctic Ocean Eddies and Baroclinic Instability. |
title_short |
Arctic Ocean Eddies and Baroclinic Instability. |
title_full |
Arctic Ocean Eddies and Baroclinic Instability. |
title_fullStr |
Arctic Ocean Eddies and Baroclinic Instability. |
title_full_unstemmed |
Arctic Ocean Eddies and Baroclinic Instability. |
title_sort |
arctic ocean eddies and baroclinic instability. |
publishDate |
1981 |
url |
http://www.dtic.mil/docs/citations/ADA101620 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA101620 |
geographic |
Arctic Arctic Ocean Canada |
geographic_facet |
Arctic Arctic Ocean Canada |
genre |
Arctic Arctic Ocean Central Arctic Alaska |
genre_facet |
Arctic Arctic Ocean Central Arctic Alaska |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA101620 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766318268643016704 |