SOME OBSERVATIONS OF THE DIURNAL HEAT WAVE IN THE OCEAN’

The diurnal heat wave was observed over several days at a station in the subtropical North Atlantic Occnn. Measurements were made every 30 min using an in situ tempera-ture-salinity-depth recorder; the isotherms were plotted (to an accuracy O.OlC) at 2-m depth intervals. For a day of average conditi...

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Main Authors: M. R. Howe, R. I. Tait
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.551.6299
http://www.aslo.org/lo/toc/vol_14/issue_1/0016.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.551.6299 2023-05-15T17:31:48+02:00 SOME OBSERVATIONS OF THE DIURNAL HEAT WAVE IN THE OCEAN’ M. R. Howe R. I. Tait The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.551.6299 http://www.aslo.org/lo/toc/vol_14/issue_1/0016.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.551.6299 http://www.aslo.org/lo/toc/vol_14/issue_1/0016.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.aslo.org/lo/toc/vol_14/issue_1/0016.pdf text ftciteseerx 2016-01-08T11:35:12Z The diurnal heat wave was observed over several days at a station in the subtropical North Atlantic Occnn. Measurements were made every 30 min using an in situ tempera-ture-salinity-depth recorder; the isotherms were plotted (to an accuracy O.OlC) at 2-m depth intervals. For a day of average conditions, the maximum penetration of the dis-ccrnible heat wave was to about 30 m, but throughout the cycle approximately 80 % of the gain of heat in the water column was confined to the top 14 m. Estimates of the coefficient of vertical eddy diffusion were made at several depths, and for the top 4 m the daily values varied between 93 cm’/scc and 432 cm”/sec. Text North Atlantic Unknown
institution Open Polar
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op_collection_id ftciteseerx
language English
description The diurnal heat wave was observed over several days at a station in the subtropical North Atlantic Occnn. Measurements were made every 30 min using an in situ tempera-ture-salinity-depth recorder; the isotherms were plotted (to an accuracy O.OlC) at 2-m depth intervals. For a day of average conditions, the maximum penetration of the dis-ccrnible heat wave was to about 30 m, but throughout the cycle approximately 80 % of the gain of heat in the water column was confined to the top 14 m. Estimates of the coefficient of vertical eddy diffusion were made at several depths, and for the top 4 m the daily values varied between 93 cm’/scc and 432 cm”/sec.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author M. R. Howe
R. I. Tait
spellingShingle M. R. Howe
R. I. Tait
SOME OBSERVATIONS OF THE DIURNAL HEAT WAVE IN THE OCEAN’
author_facet M. R. Howe
R. I. Tait
author_sort M. R. Howe
title SOME OBSERVATIONS OF THE DIURNAL HEAT WAVE IN THE OCEAN’
title_short SOME OBSERVATIONS OF THE DIURNAL HEAT WAVE IN THE OCEAN’
title_full SOME OBSERVATIONS OF THE DIURNAL HEAT WAVE IN THE OCEAN’
title_fullStr SOME OBSERVATIONS OF THE DIURNAL HEAT WAVE IN THE OCEAN’
title_full_unstemmed SOME OBSERVATIONS OF THE DIURNAL HEAT WAVE IN THE OCEAN’
title_sort some observations of the diurnal heat wave in the ocean’
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.551.6299
http://www.aslo.org/lo/toc/vol_14/issue_1/0016.pdf
genre North Atlantic
genre_facet North Atlantic
op_source http://www.aslo.org/lo/toc/vol_14/issue_1/0016.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.551.6299
http://www.aslo.org/lo/toc/vol_14/issue_1/0016.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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