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WAVE DRAG EFFECTS IN A MESOSCALE MODEL WITH A HIGHER-ORDER CLOSURE TURBULENCE SCHEME
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
1995 (English)In: JOURNAL OF APPLIED METEOROLOGY, ISSN 0894-8763, Vol. 34, no 4, 941-954 p.Article in journal (Refereed) Published
Abstract [en]

An incompressible, mesoscale model is used to estimate wave drag (WD) profiles over inhomogeneous 2D terrain. The goal is twofold: to evaluate the WD based on the model's fields and to analyze the atmospheric boundary layer(ABL) response to wave breaking

Place, publisher, year, edition, pages
AMER METEOROLOGICAL SOC , 1995. Vol. 34, no 4, 941-954 p.
Keyword [en]
HYDROSTATIC MOUNTAIN WAVES; COMPLEX TERRAIN; BOUNDARY-LAYER; DOWNSLOPE WINDSTORMS; STRATIFIED FLOW; CRITICAL-LEVEL; AIR-FLOW; SIMULATION; SURFACE; INSTABILITY
National Category
Meteorology and Atmospheric Sciences
Identifiers
URN: urn:nbn:se:uu:diva-28196OAI: oai:DiVA.org:uu-28196DiVA: diva2:56092
Note
Addresses: GRISOGONO B, UNIV UPPSALA, DEPT METEOROL, BOZ 516, S-75120 UPPSALA, SWEDEN.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-16

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