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contributor authorHenderson-Sellers, A.
date accessioned2017-06-09T14:00:57Z
date available2017-06-09T14:00:57Z
date copyright1986/02/01
date issued1986
identifier issn0733-3021
identifier otherams-10949.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146122
description abstractLayer cloud amounts for the months of January and July 1979 have been extracted from a compressed version of the U.S. Air Force's 3D-nephanalysis. These layer cloud amounts are discussed in the context of the total cloud amount climatology described by Hughes and Henderson-Sellers. Low cloud (?2000 m) is the predominant cloud type in most regions. High cloud (?6000 m) amounts are generally less than ?10% and amounts are significantly smaller than the cirrus cloud amounts of London. It seems likely that some high level cloud has been incorrectly archived as middle level cloud as a result of: (i) the assumption of cloud emissivities of one in the retrieval algorithm and (ii) the latitudinally-invarient definition of the middle/high cloud boundary. There is a reasonable level of agreement between zonally averaged low level and total cloud amounts derived here and those of London. West coast stratus is correctly identified as low cloud but the polar cloud amounts exhibit a seasonal cycle opposite to that seen in traditional climatologies.
publisherAmerican Meteorological Society
titleLayer Cloud Amounts for January and July 1979 from 3D-Nephanalysis
typeJournal Paper
journal volume25
journal issue2
journal titleJournal of Climate and Applied Meteorology
identifier doi10.1175/1520-0450(1986)025<0118:LCAFJA>2.0.CO;2
journal fristpage118
journal lastpage132
treeJournal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 002
contenttypeFulltext


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