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contributor authorKaimal, J. C.
contributor authorAbshire, N. L.
contributor authorChadwick, R. B.
contributor authorDecker, M. T.
contributor authorHooke, W. H.
contributor authorKropfli, R. A.
contributor authorNeff, W. D.
contributor authorPasqualucci, F.
contributor authorHildebrand, P. H.
date accessioned2017-06-09T13:58:56Z
date available2017-06-09T13:58:56Z
date copyright1982/08/01
date issued1982
identifier issn0021-8952
identifier otherams-10318.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145422
description abstractThree in-situ and five remote sensing techniques for measuring the height of the daytime convective boundary layer were compared. There was, as a rule, good agreement between the different systems when the capping inversion was steep and well defined, and some variability when the stratification was not so sharply defined. Two indirect methods for estimating boundary-layer heights from the length scales of convective motions in the layer are also discussed.
publisherAmerican Meteorological Society
titleEstimating the Depth of the Daytime Convective Boundary Layer
typeJournal Paper
journal volume21
journal issue8
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1982)021<1123:ETDOTD>2.0.CO;2
journal fristpage1123
journal lastpage1129
treeJournal of Applied Meteorology:;1982:;volume( 021 ):;issue: 008
contenttypeFulltext


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