Show simple item record

contributor authorGera, B. S.
contributor authorWeill, A.
date accessioned2017-06-09T14:01:51Z
date available2017-06-09T14:01:51Z
date copyright1987/08/01
date issued1987
identifier issn0733-3021
identifier otherams-11195.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146396
description abstractDoppler sodar information on the wind field in relation to frontal slope observed on reflectivity facsimile records was considered during Mesogers 84 experiment. The data have been analyzed to examine and quantify the correlation between vertical (updraft/downdraft) velocities and the frictional velocity in the surface layer. Based on theoretical considerations, the frontal slope modifications due to divergence of frontal friction have been quantified, and the associated drag coefficients are tentatively established. It has been observed that the downdraft velocities tend to increase with the horizontal wind speed in the surface layer. Frontal slope is directly proportional to the magnitude of momentum transfer (in the direction of front propagation) caused by friction velocity in the surface layer. Estimated values of drag are realistic.
publisherAmerican Meteorological Society
titleDoppler Sodar Analysis of Frontal Friction in Relation to Frontal Slope
typeJournal Paper
journal volume26
journal issue8
journal titleJournal of Climate and Applied Meteorology
identifier doi10.1175/1520-0450(1987)026<0885:DSAOFF>2.0.CO;2
journal fristpage885
journal lastpage891
treeJournal of Climate and Applied Meteorology:;1987:;Volume( 026 ):;Issue: 008
contenttypeFulltext


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record