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    Layer Cloud Amounts for January and July 1979 from 3D-Nephanalysis

    Source: Journal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 002::page 118
    Author:
    Henderson-Sellers, A.
    DOI: 10.1175/1520-0450(1986)025<0118:LCAFJA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Layer 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.
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      Layer Cloud Amounts for January and July 1979 from 3D-Nephanalysis

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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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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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