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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Bibliographic Details
Published in:Journal of Geophysical Research, Washington, DC Vol. 102; no. C4; pp. 8657 - 8662
Main Author: Eilola, Kari
Format: Journal Article
Language:English
Published: Washington, DC Blackwell Publishing Ltd 15-04-1997
American Geophysical Union
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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.
Bibliography:ark:/67375/WNG-FTJG3D4X-2
ArticleID:97JC00295
istex:263F231B42A940681E8520B268BCE33B8AE1A8C7
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
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ISSN:0148-0227
2169-9275
2156-2202
2169-9291
DOI:10.1029/97JC00295