On the geographic variability of oceanic mesoscale motions ...

Quasi-synoptic expendable bathythermograph data were acquired, from the Canadian Armed Forces, the United States Navy and the United States National Oceanographic Data Center, for the Pacific and Atlantic Oceans. On the basis of these data and the results of previous studies using climatological dat...

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Main Author: Thomson, Keith Alec
Format: Text
Language:English
Published: University of British Columbia 2010
Subjects:
Online Access:https://dx.doi.org/10.14288/1.0053251
https://doi.library.ubc.ca/10.14288/1.0053251
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spelling ftdatacite:10.14288/1.0053251 2024-04-28T08:32:09+00:00 On the geographic variability of oceanic mesoscale motions ... Thomson, Keith Alec 2010 https://dx.doi.org/10.14288/1.0053251 https://doi.library.ubc.ca/10.14288/1.0053251 en eng University of British Columbia article-journal Text ScholarlyArticle 2010 ftdatacite https://doi.org/10.14288/1.0053251 2024-04-02T09:38:34Z Quasi-synoptic expendable bathythermograph data were acquired, from the Canadian Armed Forces, the United States Navy and the United States National Oceanographic Data Center, for the Pacific and Atlantic Oceans. On the basis of these data and the results of previous studies using climatological data, six geographic regions were defined: the high-energy regions of the Northwest Atlantic and Northwest Pacific, and the low-energy regions of the Northeast Atlantic, Northeast Pacific, South Atlantic and South Pacific. Spatial series of two variables, representative of the upper layer (400 m) mesoscale variability, were obtained for each section - the mid- thermocline temperature and the geopotential anomaly (0 - 4000 kPa). The central moments and the wavenumber spectra of each variable were estimated for the six geographic regions, the combined high-energy areas and the combined low-energy areas. In the high-energy regions and the Northeast Atlantic, it was found that the temperature between 350 and 400 m is ... Text Northeast Atlantic Northwest Atlantic DataCite Metadata Store (German National Library of Science and Technology)
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language English
description Quasi-synoptic expendable bathythermograph data were acquired, from the Canadian Armed Forces, the United States Navy and the United States National Oceanographic Data Center, for the Pacific and Atlantic Oceans. On the basis of these data and the results of previous studies using climatological data, six geographic regions were defined: the high-energy regions of the Northwest Atlantic and Northwest Pacific, and the low-energy regions of the Northeast Atlantic, Northeast Pacific, South Atlantic and South Pacific. Spatial series of two variables, representative of the upper layer (400 m) mesoscale variability, were obtained for each section - the mid- thermocline temperature and the geopotential anomaly (0 - 4000 kPa). The central moments and the wavenumber spectra of each variable were estimated for the six geographic regions, the combined high-energy areas and the combined low-energy areas. In the high-energy regions and the Northeast Atlantic, it was found that the temperature between 350 and 400 m is ...
format Text
author Thomson, Keith Alec
spellingShingle Thomson, Keith Alec
On the geographic variability of oceanic mesoscale motions ...
author_facet Thomson, Keith Alec
author_sort Thomson, Keith Alec
title On the geographic variability of oceanic mesoscale motions ...
title_short On the geographic variability of oceanic mesoscale motions ...
title_full On the geographic variability of oceanic mesoscale motions ...
title_fullStr On the geographic variability of oceanic mesoscale motions ...
title_full_unstemmed On the geographic variability of oceanic mesoscale motions ...
title_sort on the geographic variability of oceanic mesoscale motions ...
publisher University of British Columbia
publishDate 2010
url https://dx.doi.org/10.14288/1.0053251
https://doi.library.ubc.ca/10.14288/1.0053251
genre Northeast Atlantic
Northwest Atlantic
genre_facet Northeast Atlantic
Northwest Atlantic
op_doi https://doi.org/10.14288/1.0053251
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