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contributor authorBetts, Alan K.
contributor authorMinnis, Patrick
contributor authorRidgway, W.
contributor authorYoung, David F.
date accessioned2017-06-09T14:03:51Z
date available2017-06-09T14:03:51Z
date copyright1992/04/01
date issued1992
identifier issn0894-8763
identifier otherams-11771.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147036
description abstractA mixing-line boundary-layer model is used to retrieve cloud-top height from satellite-derived cloud-top temperature using 700-hPa National Meteorological Center (NMC) analyses and the Comprehensive Ocean and Atmosphere Data Set (COADS) surface data as supporting datasets. Results are compared with the fixed-lapse-rate method of retrieving boundary-layer depth from sea surface temperatures (SST) and cloud-top temperatures. A radiative-convective equilibrium boundary-layer model is used to retrieve boundary-layer structure given SST and surface wind, satellite cloud-top temperatures and cloud fraction, and the 700-hPa NMC thermodynamic analyses. Good agreement is found between the COADS data and the model solutions for low-level temperature and moisture. This suggests that equilibrium boundary-layer models may be of use over remote oceans in the retrieval of boundary-layer structure.
publisherAmerican Meteorological Society
titleIntegration of Satellite and Surface Data Using a Radiative–Convective Oceanic Boundary-Layer Model
typeJournal Paper
journal volume31
journal issue4
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1992)031<0340:IOSASD>2.0.CO;2
journal fristpage340
journal lastpage350
treeJournal of Applied Meteorology:;1992:;volume( 031 ):;issue: 004
contenttypeFulltext


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