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    Verification of General Circulation Models Applied to the Hamburg University GCM. Part I: Test of Individual Climate States

    Source: Monthly Weather Review:;1983:;volume( 111 ):;issue: 010::page 1965
    Author:
    von Storch, Hans
    ,
    Roeckner, Erich
    DOI: 10.1175/1520-0493(1983)111<1965:VOGCMA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: One objective of general circulation models is to simulate, e.g., a ?January? which is not distinguishable from observed Januaries. A strategy to verify an individual simulated state is proposed. Its main elements are: data compression by means of EOFS, performance of a multivariate parametric test, and a subsequent univariate analysis. The suggested technique is applied to four January simulations perforated with the Hamburg University GCM. The meteorological parameters treated are the zonally averaged January mean of the geopotential itself and of the intensity of transient and stationary eddies of geopotential height at 300, 500 and 8 50 mb. The comparison is based on daily observations from 15 Januaries (1967?81). It turns out that the midlatitudinal meridional gradient of geopotential height is significantly overestimated at all levels. The intensity of the transient eddies is significantly overestimated at 850 mb at practically all latitudes and at 300 and 500 mb at midlatitudes.
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      Verification of General Circulation Models Applied to the Hamburg University GCM. Part I: Test of Individual Climate States

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4200987
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    • Monthly Weather Review

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    contributor authorvon Storch, Hans
    contributor authorRoeckner, Erich
    date accessioned2017-06-09T16:04:32Z
    date available2017-06-09T16:04:32Z
    date copyright1983/10/01
    date issued1983
    identifier issn0027-0644
    identifier otherams-60329.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4200987
    description abstractOne objective of general circulation models is to simulate, e.g., a ?January? which is not distinguishable from observed Januaries. A strategy to verify an individual simulated state is proposed. Its main elements are: data compression by means of EOFS, performance of a multivariate parametric test, and a subsequent univariate analysis. The suggested technique is applied to four January simulations perforated with the Hamburg University GCM. The meteorological parameters treated are the zonally averaged January mean of the geopotential itself and of the intensity of transient and stationary eddies of geopotential height at 300, 500 and 8 50 mb. The comparison is based on daily observations from 15 Januaries (1967?81). It turns out that the midlatitudinal meridional gradient of geopotential height is significantly overestimated at all levels. The intensity of the transient eddies is significantly overestimated at 850 mb at practically all latitudes and at 300 and 500 mb at midlatitudes.
    publisherAmerican Meteorological Society
    titleVerification of General Circulation Models Applied to the Hamburg University GCM. Part I: Test of Individual Climate States
    typeJournal Paper
    journal volume111
    journal issue10
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1983)111<1965:VOGCMA>2.0.CO;2
    journal fristpage1965
    journal lastpage1976
    treeMonthly Weather Review:;1983:;volume( 111 ):;issue: 010
    contenttypeFulltext
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