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The response of bora-type flow to sea surface temperature
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
1998 (English)In: QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, ISSN 0035-9009, Vol. 124, no 548, 1227-1244 p.Article in journal (Refereed) Published
Abstract [en]

A non-linear, two-dimensional, hydrostatic, incompressible numerical model with a higher-order turbulence closure scheme is used to study the effect of sea surface temperature on the severe downslope wind called bora at the Adriatic coast. A non-linear la

Place, publisher, year, edition, pages
ROYAL METEOROLOGICAL SOC , 1998. Vol. 124, no 548, 1227-1244 p.
Keyword [en]
downslope wind; mountain wave; numerical model; THERMAL MESOSCALE CIRCULATIONS; SEVERE DOWNSLOPE WINDS; NUMERICAL SIMULATIONS; BOUNDARY-LAYER; MOUNTAIN WAVES; BALTIC COAST; MODEL; TURBULENCE; DRAG; SENSITIVITY
National Category
Meteorology and Atmospheric Sciences
Identifiers
URN: urn:nbn:se:uu:diva-28378OAI: oai:DiVA.org:uu-28378DiVA: diva2:56274
Note
Addresses: Enger L, Villavagen 16, S-75136 Uppsala, Sweden. Univ Uppsala, S-75105 Uppsala, Sweden.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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