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    Determination of Ice Water Path and Mass Median Particle Size Using Multichannel Microwave Measurements

    Source: Journal of Applied Meteorology:;2000:;volume( 039 ):;issue: 008::page 1318
    Author:
    Liu, Guosheng
    ,
    Curry, Judith A.
    DOI: 10.1175/1520-0450(2000)039<1318:DOIWPA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The method of simultaneously retrieving ice water path and mass median diameter using microwave data at two frequencies is examined and implemented for tropical nonprecipitating clouds. To develop the retrieval algorithm, the authors first derived a bulk mass?size relation for ice particles in tropical clouds based on microphysical data collected during the Central Equatorial Pacific Experiment. This relation effectively allows ice particle density to decrease with particle size. In implementing the retrieval algorithm, 150- and 220-GHz Millimeter-Wave Imaging Radiometer data collected during the Tropical Ocean and Global Atmosphere Coupled Ocean?Atmosphere Response Experiment were used. Ice water path and mass median diameter are determined based on a lookup table generated by a radiative transfer model. The lookup table depends on cloud type, cloud liquid water path, and atmospheric temperature and humidity profiles. Only nonprecipitating clouds are studied in this paper. Error analyses were performed by a Monte Carlo procedure in which atmospheric profiles, ice cloud height, liquid water content, surface temperature, and instrument noise vary randomly within their uncertainty range through a Latin hypercube sampling scheme. The rms error in the retrievals is then assessed and presented in a two-dimensional diagram of ice water path and mass median diameter. It is shown that the simultaneous retrieval method using 150 and 220 GHz may be used for clouds with ice water path larger than 200 g m?2 and mass median diameter larger than 200 ?m. To obtain meaningful retrievals for ?thinner? clouds, higher microwave frequencies are needed. It is also shown that liquid water clouds that are at the same altitude as ice clouds interfere with the retrievals to a significant degree. To obtain reasonable ice water path and mass median size retrievals, it is necessary first to group clouds into several classes, then to apply separate algorithms to the different classes. The accuracy of the retrievals also depends on cloud type, with the best accuracy for cirrus and the worst for the midtop mixed-phase cloud among the clouds investigated in this study.
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      Determination of Ice Water Path and Mass Median Particle Size Using Multichannel Microwave Measurements

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4148269
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    contributor authorLiu, Guosheng
    contributor authorCurry, Judith A.
    date accessioned2017-06-09T14:07:31Z
    date available2017-06-09T14:07:31Z
    date copyright2000/08/01
    date issued2000
    identifier issn0894-8763
    identifier otherams-12881.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148269
    description abstractThe method of simultaneously retrieving ice water path and mass median diameter using microwave data at two frequencies is examined and implemented for tropical nonprecipitating clouds. To develop the retrieval algorithm, the authors first derived a bulk mass?size relation for ice particles in tropical clouds based on microphysical data collected during the Central Equatorial Pacific Experiment. This relation effectively allows ice particle density to decrease with particle size. In implementing the retrieval algorithm, 150- and 220-GHz Millimeter-Wave Imaging Radiometer data collected during the Tropical Ocean and Global Atmosphere Coupled Ocean?Atmosphere Response Experiment were used. Ice water path and mass median diameter are determined based on a lookup table generated by a radiative transfer model. The lookup table depends on cloud type, cloud liquid water path, and atmospheric temperature and humidity profiles. Only nonprecipitating clouds are studied in this paper. Error analyses were performed by a Monte Carlo procedure in which atmospheric profiles, ice cloud height, liquid water content, surface temperature, and instrument noise vary randomly within their uncertainty range through a Latin hypercube sampling scheme. The rms error in the retrievals is then assessed and presented in a two-dimensional diagram of ice water path and mass median diameter. It is shown that the simultaneous retrieval method using 150 and 220 GHz may be used for clouds with ice water path larger than 200 g m?2 and mass median diameter larger than 200 ?m. To obtain meaningful retrievals for ?thinner? clouds, higher microwave frequencies are needed. It is also shown that liquid water clouds that are at the same altitude as ice clouds interfere with the retrievals to a significant degree. To obtain reasonable ice water path and mass median size retrievals, it is necessary first to group clouds into several classes, then to apply separate algorithms to the different classes. The accuracy of the retrievals also depends on cloud type, with the best accuracy for cirrus and the worst for the midtop mixed-phase cloud among the clouds investigated in this study.
    publisherAmerican Meteorological Society
    titleDetermination of Ice Water Path and Mass Median Particle Size Using Multichannel Microwave Measurements
    typeJournal Paper
    journal volume39
    journal issue8
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(2000)039<1318:DOIWPA>2.0.CO;2
    journal fristpage1318
    journal lastpage1329
    treeJournal of Applied Meteorology:;2000:;volume( 039 ):;issue: 008
    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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