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Numerical study of lake-land breeze over Lake Vättern, Sweden
SMHI.
1986 (English)Report (Other academic)
Abstract [en]

This paper describes a two- dimensional lake breeze model With turbulent energy closure. The simulated results show that (1) the front of the lake breeze progresses inland faster in the late afternoon than at the fully developed stage;(2) the lake breeze and land breeze have larger extension offshore than inland. The acceleration of the front in the declining phase of the lake breeze is explained in terms of the decreased turbulent friction acting on the head of the lake breeze. The larger extension offshore, probably, is attributed to the smaller roughness of water surface and to the offshore synoptic wind.

Place, publisher, year, edition, pages
SMHI , 1986. , p. 19
Series
RMK: Report Meteorology and Climatology, ISSN 0347-2116 ; 48
Keywords [en]
breeze front, declining phase, fully developed stage, lake breeze, land breeze, onset
Keywords [sv]
bris, framstormande
National Category
Meteorology and Atmospheric Sciences
Research subject
Meteorology; Climate
Identifiers
URN: urn:nbn:se:smhi:diva-2703Local ID: Meteorologi, Rapporter, Serie RMKOAI: oai:DiVA.org:smhi-2703DiVA, id: diva2:947999
Available from: 1986-09-17 Created: 2016-07-08 Last updated: 2020-03-19Bibliographically approved

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CiteExportLink to record
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Citation style
  • apa
  • ieee
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  • Other style
More styles
Language
  • de-DE
  • en-GB
  • en-US
  • fi-FI
  • nn-NO
  • nn-NB
  • sv-SE
  • Other locale
More languages
Output format
  • html
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  • asciidoc
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