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contributor authorSikora, Todd D.
contributor authorYoung, George S.
contributor authorShirer, Hampton N.
contributor authorChapman, Rick D.
date accessioned2017-06-09T14:06:18Z
date available2017-06-09T14:06:18Z
date copyright1997/07/01
date issued1997
identifier issn0894-8763
identifier otherams-12497.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147842
description abstractKilometer-scale mottling seen on real and synthetic aperture radar imagery of the sea surface can be linked to the presence of microscale cellular convection (thermals) spanning the marine atmospheric boundary layer. In the current study, it is hypothesized that the typical scale of the mottling, found via standard Fourier spectral analysis, can be used to estimate the depth of the convective marine atmospheric boundary layer (zi) using a modified form of traditional mixed-layer similarity theory for these thermals? aspect ratio. The hypothesis linking the typical scale of mottling to zi is substantiated using previously published boundary layer results and supporting meteorological and oceanographic data from a number of case studies.
publisherAmerican Meteorological Society
titleEstimating Convective Atmospheric Boundary Layer Depth from Microwave Radar Imagery of the Sea Surface
typeJournal Paper
journal volume36
journal issue7
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1997)036<0833:ECABLD>2.0.CO;2
journal fristpage833
journal lastpage845
treeJournal of Applied Meteorology:;1997:;volume( 036 ):;issue: 007
contenttypeFulltext


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