Show simple item record

contributor authorPanofsky, Hans A.
contributor authorDutton, John A.
contributor authorHemmerich, Kurt H.
contributor authorMcCreary, G.
contributor authorLoving, N. V.
date accessioned2017-06-09T16:56:08Z
date available2017-06-09T16:56:08Z
date copyright1968/06/01
date issued1968
identifier issn0021-8952
identifier otherams-7669.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4219166
description abstractTwo separate case studies of clear air turbulence are presented, one in the stratosphere over the Rocky Mountains, the other in the upper troposphere over the midwestern plains. The mechanism in both situations appears to be similar. CAT occurs in strongly baroclinic zones with strong vertical wind shears and low Richardson numbers. There is a tendency for the most severe turbulence to be located at the edges of the baroclinic zones.
publisherAmerican Meteorological Society
titleCase Studies of the Distribution of CAT in the Troposphere and Stratosphere
typeJournal Paper
journal volume7
journal issue3
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1968)007<0384:CSOTDO>2.0.CO;2
journal fristpage384
journal lastpage389
treeJournal of Applied Meteorology:;1968:;volume( 007 ):;issue: 003
contenttypeFulltext


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record