A Model Analysis of Potential Vorticity on Isopycnal Surfaces for the Global Ocean
Charts of potential vorticity (q) within four different density layers, calculated from an eddy resolving global ocean general circulation model, are presented for the Atlantic, Pacific, and Indian Ocean Basins. Potential Vorticity is evaluated as q = (f/p)*(delta sigma/delta z), a formulation that...
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ftdtic:ADA275047 2023-05-15T14:04:37+02:00 A Model Analysis of Potential Vorticity on Isopycnal Surfaces for the Global Ocean Marble, Douglas C. NAVAL POSTGRADUATE SCHOOL MONTEREY CA 1993-09 text/html http://www.dtic.mil/docs/citations/ADA275047 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA275047 en eng http://www.dtic.mil/docs/citations/ADA275047 Approved for public release; distribution is unlimited. DTIC AND NTIS Physical and Dynamic Oceanography *OCEAN CURRENTS *VORTICES *THERMOCLINES *OCEAN BASINS MATHEMATICAL MODELS OUTPUT OCEAN SURFACE LAYERS CONVECTION COORDINATES CIRCULATION CORIOLIS EFFECT OCEANOGRAPHY INDIAN OCEAN GRADIENTS CHARTS BOUNDARIES EDDIES(FLUID MECHANICS) VENTILATION MODELS DENSITY GLOBAL *OCEAN CIRCULATION VORTICITY Text 1993 ftdtic 2016-02-22T03:05:37Z Charts of potential vorticity (q) within four different density layers, calculated from an eddy resolving global ocean general circulation model, are presented for the Atlantic, Pacific, and Indian Ocean Basins. Potential Vorticity is evaluated as q = (f/p)*(delta sigma/delta z), a formulation that is valid for large, slow scales and allows it to be readily calculated from model output. Here, f is Coriolis, p in situ density, sigma the potential density referred to the sea surface, and z the vertical coordinate. The model is shown to represent oceanic density structure with reasonable accuracy. The most significant departure from observations are the steep density gradients on the northern boundary of the Antarctic Circumpolar Current. This may be due to model convective adjustment parameterizations and the extent of the smoothing in the cataloged data, which may be greater in the southern oceans due to relatively scarce observations. Model derived values of potential vorticity correspond well with those calculated from observations. In the middle and lower layers, the three basins tend toward homogenization, representing unventilated layers. Gyres of q in the upper layers of the northern Atlantic and Pacific Oceans, with their northern boundaries anchored in the outcrop region, illustrate the ventilation of these layers. Oceanography, Numerical modeling, Potential vorticity. Text Antarc* Antarctic Defense Technical Information Center: DTIC Technical Reports database Antarctic Indian Pacific The Antarctic |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Physical and Dynamic Oceanography *OCEAN CURRENTS *VORTICES *THERMOCLINES *OCEAN BASINS MATHEMATICAL MODELS OUTPUT OCEAN SURFACE LAYERS CONVECTION COORDINATES CIRCULATION CORIOLIS EFFECT OCEANOGRAPHY INDIAN OCEAN GRADIENTS CHARTS BOUNDARIES EDDIES(FLUID MECHANICS) VENTILATION MODELS DENSITY GLOBAL *OCEAN CIRCULATION VORTICITY |
spellingShingle |
Physical and Dynamic Oceanography *OCEAN CURRENTS *VORTICES *THERMOCLINES *OCEAN BASINS MATHEMATICAL MODELS OUTPUT OCEAN SURFACE LAYERS CONVECTION COORDINATES CIRCULATION CORIOLIS EFFECT OCEANOGRAPHY INDIAN OCEAN GRADIENTS CHARTS BOUNDARIES EDDIES(FLUID MECHANICS) VENTILATION MODELS DENSITY GLOBAL *OCEAN CIRCULATION VORTICITY Marble, Douglas C. A Model Analysis of Potential Vorticity on Isopycnal Surfaces for the Global Ocean |
topic_facet |
Physical and Dynamic Oceanography *OCEAN CURRENTS *VORTICES *THERMOCLINES *OCEAN BASINS MATHEMATICAL MODELS OUTPUT OCEAN SURFACE LAYERS CONVECTION COORDINATES CIRCULATION CORIOLIS EFFECT OCEANOGRAPHY INDIAN OCEAN GRADIENTS CHARTS BOUNDARIES EDDIES(FLUID MECHANICS) VENTILATION MODELS DENSITY GLOBAL *OCEAN CIRCULATION VORTICITY |
description |
Charts of potential vorticity (q) within four different density layers, calculated from an eddy resolving global ocean general circulation model, are presented for the Atlantic, Pacific, and Indian Ocean Basins. Potential Vorticity is evaluated as q = (f/p)*(delta sigma/delta z), a formulation that is valid for large, slow scales and allows it to be readily calculated from model output. Here, f is Coriolis, p in situ density, sigma the potential density referred to the sea surface, and z the vertical coordinate. The model is shown to represent oceanic density structure with reasonable accuracy. The most significant departure from observations are the steep density gradients on the northern boundary of the Antarctic Circumpolar Current. This may be due to model convective adjustment parameterizations and the extent of the smoothing in the cataloged data, which may be greater in the southern oceans due to relatively scarce observations. Model derived values of potential vorticity correspond well with those calculated from observations. In the middle and lower layers, the three basins tend toward homogenization, representing unventilated layers. Gyres of q in the upper layers of the northern Atlantic and Pacific Oceans, with their northern boundaries anchored in the outcrop region, illustrate the ventilation of these layers. Oceanography, Numerical modeling, Potential vorticity. |
author2 |
NAVAL POSTGRADUATE SCHOOL MONTEREY CA |
format |
Text |
author |
Marble, Douglas C. |
author_facet |
Marble, Douglas C. |
author_sort |
Marble, Douglas C. |
title |
A Model Analysis of Potential Vorticity on Isopycnal Surfaces for the Global Ocean |
title_short |
A Model Analysis of Potential Vorticity on Isopycnal Surfaces for the Global Ocean |
title_full |
A Model Analysis of Potential Vorticity on Isopycnal Surfaces for the Global Ocean |
title_fullStr |
A Model Analysis of Potential Vorticity on Isopycnal Surfaces for the Global Ocean |
title_full_unstemmed |
A Model Analysis of Potential Vorticity on Isopycnal Surfaces for the Global Ocean |
title_sort |
model analysis of potential vorticity on isopycnal surfaces for the global ocean |
publishDate |
1993 |
url |
http://www.dtic.mil/docs/citations/ADA275047 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA275047 |
geographic |
Antarctic Indian Pacific The Antarctic |
geographic_facet |
Antarctic Indian Pacific The Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA275047 |
op_rights |
Approved for public release; distribution is unlimited. |
_version_ |
1766275823559507968 |