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    COSMIC GPS Radio Occultation Temperature Profiles in Clouds

    Source: Monthly Weather Review:;2009:;volume( 138 ):;issue: 004::page 1104
    Author:
    Lin, L.
    ,
    Zou, X.
    ,
    Anthes, R.
    ,
    Kuo, Y-H.
    DOI: 10.1175/2009MWR2986.1
    Publisher: American Meteorological Society
    Abstract: Thermodynamic states in clouds are closely related to physical processes such as phase changes of water and longwave and shortwave radiation. Global Positioning System (GPS) radio occultation (RO) data are not affected by clouds and have high vertical resolution, making them ideally suited to cloud profiling on a global basis. By comparing the Constellation Observing System for Meteorology, Ionosphere, and Climate (COSMIC) RO refractivity data with those of the National Centers for Environmental Prediction?National Center for Atmospheric Research (NCEP?NCAR) reanalysis and ECMWF analysis for soundings in clouds and clear air separately, a systematic bias of opposite sign was found between large-scale global analyses and the GPS RO observations under cloudy and clear-sky conditions. As a modification to the standard GPS RO wet temperature retrieval that does not distinguish between cloudy- and clear-sky conditions, a new cloudy retrieval algorithm is proposed to incorporate the knowledge that in-cloud specific humidity (which affects the GPS refractivities) should be close to saturation. To implement this new algorithm, a linear regression model for a sounding-dependent relative humidity parameter α is first developed based on a high correlation between relative humidity and ice water content. In the absence of ice water content information, α takes an empirical value of 85%. The in-cloud temperature profile is then retrieved from GPS RO data modeled by a weighted sum of refractivities with and without the assumption of saturation. Compared to the standard wet retrieval, the cloudy temperature retrieval is consistently warmer within clouds by ?2 K and slightly colder near the cloud top (?1 K) and cloud base (1.5 K), leading to a more rapid increase of the lapse rate with height in the upper half of the cloud, from a nearly constant moist lapse rate below and at the cloud middle (?6°C km?1) to a value of 7.7°C km?1, which must be closer to the dry lapse rate than the standard wet retrieval.
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      COSMIC GPS Radio Occultation Temperature Profiles in Clouds

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4211282
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    • Monthly Weather Review

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    contributor authorLin, L.
    contributor authorZou, X.
    contributor authorAnthes, R.
    contributor authorKuo, Y-H.
    date accessioned2017-06-09T16:32:15Z
    date available2017-06-09T16:32:15Z
    date copyright2010/04/01
    date issued2009
    identifier issn0027-0644
    identifier otherams-69596.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4211282
    description abstractThermodynamic states in clouds are closely related to physical processes such as phase changes of water and longwave and shortwave radiation. Global Positioning System (GPS) radio occultation (RO) data are not affected by clouds and have high vertical resolution, making them ideally suited to cloud profiling on a global basis. By comparing the Constellation Observing System for Meteorology, Ionosphere, and Climate (COSMIC) RO refractivity data with those of the National Centers for Environmental Prediction?National Center for Atmospheric Research (NCEP?NCAR) reanalysis and ECMWF analysis for soundings in clouds and clear air separately, a systematic bias of opposite sign was found between large-scale global analyses and the GPS RO observations under cloudy and clear-sky conditions. As a modification to the standard GPS RO wet temperature retrieval that does not distinguish between cloudy- and clear-sky conditions, a new cloudy retrieval algorithm is proposed to incorporate the knowledge that in-cloud specific humidity (which affects the GPS refractivities) should be close to saturation. To implement this new algorithm, a linear regression model for a sounding-dependent relative humidity parameter α is first developed based on a high correlation between relative humidity and ice water content. In the absence of ice water content information, α takes an empirical value of 85%. The in-cloud temperature profile is then retrieved from GPS RO data modeled by a weighted sum of refractivities with and without the assumption of saturation. Compared to the standard wet retrieval, the cloudy temperature retrieval is consistently warmer within clouds by ?2 K and slightly colder near the cloud top (?1 K) and cloud base (1.5 K), leading to a more rapid increase of the lapse rate with height in the upper half of the cloud, from a nearly constant moist lapse rate below and at the cloud middle (?6°C km?1) to a value of 7.7°C km?1, which must be closer to the dry lapse rate than the standard wet retrieval.
    publisherAmerican Meteorological Society
    titleCOSMIC GPS Radio Occultation Temperature Profiles in Clouds
    typeJournal Paper
    journal volume138
    journal issue4
    journal titleMonthly Weather Review
    identifier doi10.1175/2009MWR2986.1
    journal fristpage1104
    journal lastpage1118
    treeMonthly Weather Review:;2009:;volume( 138 ):;issue: 004
    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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