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    A Multisensor Approach Toward a Better Understanding of Snowfall Microphysics: The TOSCA Project

    Source: Bulletin of the American Meteorological Society:;2011:;volume( 092 ):;issue: 005::page 613
    Author:
    Löhnert, U.
    ,
    Kneifel, S.
    ,
    Battaglia, A.
    ,
    Hagen, M.
    ,
    Hirsch, L.
    ,
    Crewell, S.
    DOI: 10.1175/2010BAMS2909.1
    Publisher: American Meteorological Society
    Abstract: ds an Optimal estimation based Snow Characterization Algorithm (TOSCA) project addresses possible novel measurement synergies for deriving snowfall microphysical parameters from the ground by combining the unique information obtained from a suite of ground-based sensors: microwave radiometers (22?150 GHz), 24- and 36-GHz radar, lidar, and in situ optical disdrometer methods. During the winter of 2008/09, such instruments were deployed at the Environmental Research Station Schneefernerhaus (UFS; at 2650 m MSL) at the Zugspitze Mountain in Germany for deriving microphysical properties of snowfall. This contribution gives an overview of the measurements carried out and discusses the potential for the developments of synergetic retrieval algorithms for deriving snow water content within the vertical column. The identification of potentially valuable ground-based instrument synergy for the retrieval of snowfall parameters from the surface will also be of importance for the development of new space-borne observational techniques. Microwave radiometer measurements show that brightness temperature enhancements at 90 and 150 GHz are correlated with the radar-derived snow water path, which is supported by radiative transfer simulations. The synergy of these measurements toward an improved snow mass content, however, needs to be augmented by knowledge on water vapor, supercooled liquid water, particle size distribution, and shape, thus making clear the necessity of synergetic remote sensing and in situ measurements. The radiometric measurements also reveal the very frequent presence of supercooled water within snow clouds and its importance to microphysical diffusion and aggregation growth of snow crystals. Analysis of the disdrometer measurements shows a ?secondary aggregation peak? around ?12° to ?15°C, a temperature range where the Wegener?Bergeron?Findeisen process is most effective and typically dendrite snow crystals forms dominate.
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      A Multisensor Approach Toward a Better Understanding of Snowfall Microphysics: The TOSCA Project

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4211556
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    contributor authorLöhnert, U.
    contributor authorKneifel, S.
    contributor authorBattaglia, A.
    contributor authorHagen, M.
    contributor authorHirsch, L.
    contributor authorCrewell, S.
    date accessioned2017-06-09T16:33:05Z
    date available2017-06-09T16:33:05Z
    date copyright2011/05/01
    date issued2011
    identifier issn0003-0007
    identifier otherams-69842.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4211556
    description abstractds an Optimal estimation based Snow Characterization Algorithm (TOSCA) project addresses possible novel measurement synergies for deriving snowfall microphysical parameters from the ground by combining the unique information obtained from a suite of ground-based sensors: microwave radiometers (22?150 GHz), 24- and 36-GHz radar, lidar, and in situ optical disdrometer methods. During the winter of 2008/09, such instruments were deployed at the Environmental Research Station Schneefernerhaus (UFS; at 2650 m MSL) at the Zugspitze Mountain in Germany for deriving microphysical properties of snowfall. This contribution gives an overview of the measurements carried out and discusses the potential for the developments of synergetic retrieval algorithms for deriving snow water content within the vertical column. The identification of potentially valuable ground-based instrument synergy for the retrieval of snowfall parameters from the surface will also be of importance for the development of new space-borne observational techniques. Microwave radiometer measurements show that brightness temperature enhancements at 90 and 150 GHz are correlated with the radar-derived snow water path, which is supported by radiative transfer simulations. The synergy of these measurements toward an improved snow mass content, however, needs to be augmented by knowledge on water vapor, supercooled liquid water, particle size distribution, and shape, thus making clear the necessity of synergetic remote sensing and in situ measurements. The radiometric measurements also reveal the very frequent presence of supercooled water within snow clouds and its importance to microphysical diffusion and aggregation growth of snow crystals. Analysis of the disdrometer measurements shows a ?secondary aggregation peak? around ?12° to ?15°C, a temperature range where the Wegener?Bergeron?Findeisen process is most effective and typically dendrite snow crystals forms dominate.
    publisherAmerican Meteorological Society
    titleA Multisensor Approach Toward a Better Understanding of Snowfall Microphysics: The TOSCA Project
    typeJournal Paper
    journal volume92
    journal issue5
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/2010BAMS2909.1
    journal fristpage613
    journal lastpage628
    treeBulletin of the American Meteorological Society:;2011:;volume( 092 ):;issue: 005
    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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