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    A TRMM-Based Tropical Cyclone Cloud and Precipitation Feature Database

    Source: Journal of Applied Meteorology and Climatology:;2011:;volume( 050 ):;issue: 006::page 1255
    Author:
    Jiang, Haiyan
    ,
    Liu, Chuntao
    ,
    Zipser, Edward J.
    DOI: 10.1175/2011JAMC2662.1
    Publisher: American Meteorological Society
    Abstract: he Tropical Rainfall Measuring Mission (TRMM) satellite has provided invaluable data for tropical cyclone (TC) research since December 1997. The challenge, however, is how to analyze and efficiently utilize all of the information from several instruments on TRMM that observe the same target. In this study, a tropical cyclone precipitation, cloud, and convective cell feature (TCPF) database has been developed by using observations of the TRMM precipitation radar (PR), Microwave Imager (TMI), Visible and Infrared Scanner (VIRS), Lightning Imaging System (LIS), and the TRMM 3B42 rainfall product. The database is based on an event-based method that analyzes the measurements from multiple sensors. This method condenses the original information of pixel-level measurements into the properties of events, which can significantly increase the efficiency of searching and sorting the observed historical TCs. With both convective and rainfall properties included, the database offers the potential to aid the research aiming to improve both TC intensification and rainfall forecasts. Using the TRMM TCPF database, regional variations of TC convection and diurnal variations of TC rainfall are examined. In terms of absolute number, the northwest Pacific Ocean basin has the deepest and most intense TCPFs according to IR, radar, and 85-GHz microwave measurements. However, the North Atlantic TCPFs appear to have the highest lightning production. Globally, TC rainfall has a maximum at 0430?0730 local solar time (LST) and a minimum around 1930?2230 LST. However, after separating ocean from land, a distinct difference is seen. Over land, the diurnal variation of TC rainfall shows double peaks: one around 0130?0730 LST and the other at 1630?1930 LST. The minimum is at 1030?1330 LST.
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      A TRMM-Based Tropical Cyclone Cloud and Precipitation Feature Database

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4213575
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    contributor authorJiang, Haiyan
    contributor authorLiu, Chuntao
    contributor authorZipser, Edward J.
    date accessioned2017-06-09T16:39:20Z
    date available2017-06-09T16:39:20Z
    date copyright2011/06/01
    date issued2011
    identifier issn1558-8424
    identifier otherams-71659.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4213575
    description abstracthe Tropical Rainfall Measuring Mission (TRMM) satellite has provided invaluable data for tropical cyclone (TC) research since December 1997. The challenge, however, is how to analyze and efficiently utilize all of the information from several instruments on TRMM that observe the same target. In this study, a tropical cyclone precipitation, cloud, and convective cell feature (TCPF) database has been developed by using observations of the TRMM precipitation radar (PR), Microwave Imager (TMI), Visible and Infrared Scanner (VIRS), Lightning Imaging System (LIS), and the TRMM 3B42 rainfall product. The database is based on an event-based method that analyzes the measurements from multiple sensors. This method condenses the original information of pixel-level measurements into the properties of events, which can significantly increase the efficiency of searching and sorting the observed historical TCs. With both convective and rainfall properties included, the database offers the potential to aid the research aiming to improve both TC intensification and rainfall forecasts. Using the TRMM TCPF database, regional variations of TC convection and diurnal variations of TC rainfall are examined. In terms of absolute number, the northwest Pacific Ocean basin has the deepest and most intense TCPFs according to IR, radar, and 85-GHz microwave measurements. However, the North Atlantic TCPFs appear to have the highest lightning production. Globally, TC rainfall has a maximum at 0430?0730 local solar time (LST) and a minimum around 1930?2230 LST. However, after separating ocean from land, a distinct difference is seen. Over land, the diurnal variation of TC rainfall shows double peaks: one around 0130?0730 LST and the other at 1630?1930 LST. The minimum is at 1030?1330 LST.
    publisherAmerican Meteorological Society
    titleA TRMM-Based Tropical Cyclone Cloud and Precipitation Feature Database
    typeJournal Paper
    journal volume50
    journal issue6
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/2011JAMC2662.1
    journal fristpage1255
    journal lastpage1274
    treeJournal of Applied Meteorology and Climatology:;2011:;volume( 050 ):;issue: 006
    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