YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Journal of Applied Meteorology
    • View Item
    •   YE&T Library
    • AMS
    • Journal of Applied Meteorology
    • View Item
    • All Fields
    • Source Title
    • Year
    • Publisher
    • Title
    • Subject
    • Author
    • DOI
    • ISBN
    Advanced Search
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Archive

    Spectral Retrieval of Latent Heating Profiles from TRMM PR Data. Part I: Development of a Model-Based Algorithm

    Source: Journal of Applied Meteorology:;2004:;volume( 043 ):;issue: 008::page 1095
    Author:
    Shige, Shoichi
    ,
    Takayabu, Yukari N.
    ,
    Tao, Wei-Kuo
    ,
    Johnson, Daniel E.
    DOI: 10.1175/1520-0450(2004)043<1095:SROLHP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: An algorithm, the spectral latent heating (SLH) algorithm, has been developed to estimate latent heating profiles for the Tropical Rainfall Measuring Mission precipitation radar with a cloud-resolving model (CRM). Heating-profile lookup tables for the three rain types?convective, shallow stratiform, and anvil rain (deep stratiform with a melting level)?were produced with numerical simulations of tropical cloud systems in the Tropical Ocean and Global Atmosphere Coupled Ocean?Atmosphere Response Experiment. For convective and shallow stratiform regions, the lookup table refers to the precipitation-top height (PTH). For the anvil region, on the other hand, the lookup table refers to the precipitation rate at the melting level instead of PTH. A consistency check of the SLH algorithm was also done with the CRM-simulated outputs. The first advantage of this algorithm is that differences of heating profiles between the shallow convective stage and the deep convective stage can be retrieved. This is a result of the utilization of observed information, not only on precipitation type and intensity, but also on the precipitation depth. The second advantage is that heating profiles in the decaying stage with no surface rain can also be retrieved. This comes from utilization of the precipitation rate at the melting level for anvil regions.
    • Download: (996.2Kb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      Spectral Retrieval of Latent Heating Profiles from TRMM PR Data. Part I: Development of a Model-Based Algorithm

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4148837
    Collections
    • Journal of Applied Meteorology

    Show full item record

    contributor authorShige, Shoichi
    contributor authorTakayabu, Yukari N.
    contributor authorTao, Wei-Kuo
    contributor authorJohnson, Daniel E.
    date accessioned2017-06-09T14:09:14Z
    date available2017-06-09T14:09:14Z
    date copyright2004/08/01
    date issued2004
    identifier issn0894-8763
    identifier otherams-13392.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148837
    description abstractAn algorithm, the spectral latent heating (SLH) algorithm, has been developed to estimate latent heating profiles for the Tropical Rainfall Measuring Mission precipitation radar with a cloud-resolving model (CRM). Heating-profile lookup tables for the three rain types?convective, shallow stratiform, and anvil rain (deep stratiform with a melting level)?were produced with numerical simulations of tropical cloud systems in the Tropical Ocean and Global Atmosphere Coupled Ocean?Atmosphere Response Experiment. For convective and shallow stratiform regions, the lookup table refers to the precipitation-top height (PTH). For the anvil region, on the other hand, the lookup table refers to the precipitation rate at the melting level instead of PTH. A consistency check of the SLH algorithm was also done with the CRM-simulated outputs. The first advantage of this algorithm is that differences of heating profiles between the shallow convective stage and the deep convective stage can be retrieved. This is a result of the utilization of observed information, not only on precipitation type and intensity, but also on the precipitation depth. The second advantage is that heating profiles in the decaying stage with no surface rain can also be retrieved. This comes from utilization of the precipitation rate at the melting level for anvil regions.
    publisherAmerican Meteorological Society
    titleSpectral Retrieval of Latent Heating Profiles from TRMM PR Data. Part I: Development of a Model-Based Algorithm
    typeJournal Paper
    journal volume43
    journal issue8
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(2004)043<1095:SROLHP>2.0.CO;2
    journal fristpage1095
    journal lastpage1113
    treeJournal of Applied Meteorology:;2004:;volume( 043 ):;issue: 008
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian