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    An Improved Microwave Radiative Transfer Model for Tropical Oceanic Precipitation

    Source: Journal of the Atmospheric Sciences:;1998:;Volume( 055 ):;issue: 009::page 1674
    Author:
    Tesmer, Jeffrey R.
    ,
    Wilheit, Thomas T.
    DOI: 10.1175/1520-0469(1998)055<1674:AIMRTM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In preparation for the launch of TRMM, new algorithms must be created that take advantage of the combined data from radar and microwave radiometers that will be on board the satellite. A microwave radiative transfer algorithm with a one-dimensional cloud model is created that incorporates data from radar and radiometers using data obtained from TCM-90 and TOGA COARE flown over the western Pacific in 1990 and 1993, respectively. A hybrid cloud model (HCM) was developed using observations from TOGA COARE, TCM-90, and other field projects. The HCM is a physically based model that is not ?tuned? by limited ?ground truth.? Therefore, the HCM incorporated new microphysical data based on observations of clouds. Cloud observations changed the HCM in four ways. First, stratiform clouds with low rain rates were shown to have a low cloud liquid water content (<0.1 g m?3). Second, radar data showed a linear decrease in the logarithm of the backscatter of ice particles above the freezing level. Third, tropical clouds contained more small drops and fewer large drops than predicted by the Marshall?Palmer drop size distribution. Last, the angular distribution of reflected radiation from ocean surface appears to be specular. The HCM is compared to the Wilheit et al. model (WILM). The HCM differs from the WILM at low rain rates by as much as 10 K. At high rain rates, the HCM and the WILM produce similar brightness temperatures. However, this result is fortuitous because both models have substantially different thermodynamics and microphysics incorporated into them. Next, the brightness temperatures generated by the HCM are compared to observations from TOGA COARE. It is found that the brightness temperatures produced by the HCM closely agree with the observations. This study shows that a plane-parallel microwave radiative transfer algorithm coupled with a cloud model based on microphysical observations can accurately simulate rainfall observed in the Tropics.
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      An Improved Microwave Radiative Transfer Model for Tropical Oceanic Precipitation

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4158602
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    • Journal of the Atmospheric Sciences

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    contributor authorTesmer, Jeffrey R.
    contributor authorWilheit, Thomas T.
    date accessioned2017-06-09T14:35:01Z
    date available2017-06-09T14:35:01Z
    date copyright1998/05/01
    date issued1998
    identifier issn0022-4928
    identifier otherams-22180.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4158602
    description abstractIn preparation for the launch of TRMM, new algorithms must be created that take advantage of the combined data from radar and microwave radiometers that will be on board the satellite. A microwave radiative transfer algorithm with a one-dimensional cloud model is created that incorporates data from radar and radiometers using data obtained from TCM-90 and TOGA COARE flown over the western Pacific in 1990 and 1993, respectively. A hybrid cloud model (HCM) was developed using observations from TOGA COARE, TCM-90, and other field projects. The HCM is a physically based model that is not ?tuned? by limited ?ground truth.? Therefore, the HCM incorporated new microphysical data based on observations of clouds. Cloud observations changed the HCM in four ways. First, stratiform clouds with low rain rates were shown to have a low cloud liquid water content (<0.1 g m?3). Second, radar data showed a linear decrease in the logarithm of the backscatter of ice particles above the freezing level. Third, tropical clouds contained more small drops and fewer large drops than predicted by the Marshall?Palmer drop size distribution. Last, the angular distribution of reflected radiation from ocean surface appears to be specular. The HCM is compared to the Wilheit et al. model (WILM). The HCM differs from the WILM at low rain rates by as much as 10 K. At high rain rates, the HCM and the WILM produce similar brightness temperatures. However, this result is fortuitous because both models have substantially different thermodynamics and microphysics incorporated into them. Next, the brightness temperatures generated by the HCM are compared to observations from TOGA COARE. It is found that the brightness temperatures produced by the HCM closely agree with the observations. This study shows that a plane-parallel microwave radiative transfer algorithm coupled with a cloud model based on microphysical observations can accurately simulate rainfall observed in the Tropics.
    publisherAmerican Meteorological Society
    titleAn Improved Microwave Radiative Transfer Model for Tropical Oceanic Precipitation
    typeJournal Paper
    journal volume55
    journal issue9
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1998)055<1674:AIMRTM>2.0.CO;2
    journal fristpage1674
    journal lastpage1689
    treeJournal of the Atmospheric Sciences:;1998:;Volume( 055 ):;issue: 009
    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
    yabeshDSpacePersian