Development of a spring thermocline at temperatures below the temperature of maximum density with application to the Baltic Sea
Local buoyancy supply associated with the pulsed horizontal advection of water of lower salinity at the sea surface can initiate the development of a shallow thermocline in spring. This process has been studied with an analysis of historical hydrographic data from the central parts of the Baltic pro...
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Published in: | Journal of Geophysical Research, Washington, DC Vol. 102; no. C4; pp. 8657 - 8662 |
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Main Author: | |
Format: | Journal Article |
Language: | English |
Published: |
Washington, DC
Blackwell Publishing Ltd
15-04-1997
American Geophysical Union |
Subjects: | |
Online Access: | Get full text |
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Summary: | Local buoyancy supply associated with the pulsed horizontal advection of water of lower salinity at the sea surface can initiate the development of a shallow thermocline in spring. This process has been studied with an analysis of historical hydrographic data from the central parts of the Baltic proper and numerical experiments with a seasonal pycnocline model. It is shown that this situation occurs in the Baltic Sea when the temperature of the surface water is below the temperature of maximum water density and the buoyancy flux due to heating at the sea surface is negative. |
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Bibliography: | ark:/67375/WNG-FTJG3D4X-2 ArticleID:97JC00295 istex:263F231B42A940681E8520B268BCE33B8AE1A8C7 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 ObjectType-Article-2 ObjectType-Feature-1 |
ISSN: | 0148-0227 2169-9275 2156-2202 2169-9291 |
DOI: | 10.1029/97JC00295 |