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    A Midlatitude Precipitating Cloud Database Validated with Satellite Observations

    Source: Journal of Applied Meteorology and Climatology:;2008:;volume( 047 ):;issue: 005::page 1337
    Author:
    Chaboureau, Jean-Pierre
    ,
    Söhne, Nathalie
    ,
    Pinty, Jean-Pierre
    ,
    Meirold-Mautner, Ingo
    ,
    Defer, Eric
    ,
    Prigent, Catherine
    ,
    Pardo, Juan R.
    ,
    Mech, Mario
    ,
    Crewell, Susanne
    DOI: 10.1175/2007JAMC1731.1
    Publisher: American Meteorological Society
    Abstract: The simulations of five midlatitude precipitating events by the nonhydrostatic mesoscale model Méso-NH are analyzed. These cases cover contrasted precipitation situations from 30° to 60°N, which are typical of midlatitudes. They include a frontal case with light precipitation over the Rhine River area (10 February 2000), a long-lasting precipitation event at Hoek van Holland, Netherlands (19 September 2001), a moderate rain case over the Elbe (12 August 2002), an intense rain case over Algiers (10 November 2001), and the ?millennium storm? in the United Kingdom (30 October 2000). The physically consistent hydrometeor and thermodynamic outputs are used to generate a database for cloud and precipitation retrievals. The hydrometeor vertical profiles that were generated vary mostly with the 0°C isotherm, located between 1 and 3 km in height depending on the case. The characteristics of this midlatitude database are complementary to the GPROF database, which mostly concentrates on tropical situations. The realism of the simulations is evaluated against satellite observations by comparing synthetic brightness temperatures (BTs) with Advanced Microwave Sounding Unit (AMSU), Special Sensor Microwave Imager (SSM/I), and Meteosat observations. The good reproduction of the BT distributions by the model is exploited by calculating categorical scores for verification purposes. The comparison with 3-hourly Meteosat observations demonstrates the ability of the model to forecast the time evolution of the cloud cover, the latter being better predicted for the stratiform cases than for others. The comparison with AMSU-B measurements shows the skill of the model to predict rainfall at the correct location.
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      A Midlatitude Precipitating Cloud Database Validated with Satellite Observations

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4206624
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    • Journal of Applied Meteorology and Climatology

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    contributor authorChaboureau, Jean-Pierre
    contributor authorSöhne, Nathalie
    contributor authorPinty, Jean-Pierre
    contributor authorMeirold-Mautner, Ingo
    contributor authorDefer, Eric
    contributor authorPrigent, Catherine
    contributor authorPardo, Juan R.
    contributor authorMech, Mario
    contributor authorCrewell, Susanne
    date accessioned2017-06-09T16:18:21Z
    date available2017-06-09T16:18:21Z
    date copyright2008/05/01
    date issued2008
    identifier issn1558-8424
    identifier otherams-65402.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4206624
    description abstractThe simulations of five midlatitude precipitating events by the nonhydrostatic mesoscale model Méso-NH are analyzed. These cases cover contrasted precipitation situations from 30° to 60°N, which are typical of midlatitudes. They include a frontal case with light precipitation over the Rhine River area (10 February 2000), a long-lasting precipitation event at Hoek van Holland, Netherlands (19 September 2001), a moderate rain case over the Elbe (12 August 2002), an intense rain case over Algiers (10 November 2001), and the ?millennium storm? in the United Kingdom (30 October 2000). The physically consistent hydrometeor and thermodynamic outputs are used to generate a database for cloud and precipitation retrievals. The hydrometeor vertical profiles that were generated vary mostly with the 0°C isotherm, located between 1 and 3 km in height depending on the case. The characteristics of this midlatitude database are complementary to the GPROF database, which mostly concentrates on tropical situations. The realism of the simulations is evaluated against satellite observations by comparing synthetic brightness temperatures (BTs) with Advanced Microwave Sounding Unit (AMSU), Special Sensor Microwave Imager (SSM/I), and Meteosat observations. The good reproduction of the BT distributions by the model is exploited by calculating categorical scores for verification purposes. The comparison with 3-hourly Meteosat observations demonstrates the ability of the model to forecast the time evolution of the cloud cover, the latter being better predicted for the stratiform cases than for others. The comparison with AMSU-B measurements shows the skill of the model to predict rainfall at the correct location.
    publisherAmerican Meteorological Society
    titleA Midlatitude Precipitating Cloud Database Validated with Satellite Observations
    typeJournal Paper
    journal volume47
    journal issue5
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/2007JAMC1731.1
    journal fristpage1337
    journal lastpage1353
    treeJournal of Applied Meteorology and Climatology:;2008:;volume( 047 ):;issue: 005
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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