Surface heat fluxes and subsurface heat content at a site over the southeastern Bering Sea shelf, May–July

Observations from a surface mooring, in a weak-flow regime over the southeastern Bering Sea shelf, were used to derive surface heat fluxes for the period May–July 1996. Changes in heat content of the water column also were determined from subsurface temperature measurements. Agreement of net surface...

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Bibliographic Details
Main Authors: R. K. Reed, P. J. Stabeno
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2003
Subjects:
Bering Sea
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.584.9791
http://www.pmel.noaa.gov/foci/publications/2002/reedB392.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.584.9791 2023-05-15T15:43:09+02:00 Surface heat fluxes and subsurface heat content at a site over the southeastern Bering Sea shelf, May–July R. K. Reed P. J. Stabeno The Pennsylvania State University CiteSeerX Archives 2003 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.584.9791 http://www.pmel.noaa.gov/foci/publications/2002/reedB392.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.584.9791 http://www.pmel.noaa.gov/foci/publications/2002/reedB392.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.pmel.noaa.gov/foci/publications/2002/reedB392.pdf text 2003 ftciteseerx 2016-01-08T13:12:59Z Observations from a surface mooring, in a weak-flow regime over the southeastern Bering Sea shelf, were used to derive surface heat fluxes for the period May–July 1996. Changes in heat content of the water column also were determined from subsurface temperature measurements. Agreement of net surface heat flux and change in heat content was within 2%. This result provides additional evidence that heat advection and diffusion are small in this region. Text Bering Sea Unknown Bering Sea
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description Observations from a surface mooring, in a weak-flow regime over the southeastern Bering Sea shelf, were used to derive surface heat fluxes for the period May–July 1996. Changes in heat content of the water column also were determined from subsurface temperature measurements. Agreement of net surface heat flux and change in heat content was within 2%. This result provides additional evidence that heat advection and diffusion are small in this region.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author R. K. Reed
P. J. Stabeno
spellingShingle R. K. Reed
P. J. Stabeno
Surface heat fluxes and subsurface heat content at a site over the southeastern Bering Sea shelf, May–July
author_facet R. K. Reed
P. J. Stabeno
author_sort R. K. Reed
title Surface heat fluxes and subsurface heat content at a site over the southeastern Bering Sea shelf, May–July
title_short Surface heat fluxes and subsurface heat content at a site over the southeastern Bering Sea shelf, May–July
title_full Surface heat fluxes and subsurface heat content at a site over the southeastern Bering Sea shelf, May–July
title_fullStr Surface heat fluxes and subsurface heat content at a site over the southeastern Bering Sea shelf, May–July
title_full_unstemmed Surface heat fluxes and subsurface heat content at a site over the southeastern Bering Sea shelf, May–July
title_sort surface heat fluxes and subsurface heat content at a site over the southeastern bering sea shelf, may–july
publishDate 2003
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.584.9791
http://www.pmel.noaa.gov/foci/publications/2002/reedB392.pdf
geographic Bering Sea
geographic_facet Bering Sea
genre Bering Sea
genre_facet Bering Sea
op_source http://www.pmel.noaa.gov/foci/publications/2002/reedB392.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.584.9791
http://www.pmel.noaa.gov/foci/publications/2002/reedB392.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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