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    A Real–Time Global Half–Hourly Pixel–Resolution Infrared Dataset and Its Applications

    Source: Bulletin of the American Meteorological Society:;2001:;volume( 082 ):;issue: 002::page 205
    Author:
    Janowiak, John E.
    ,
    Joyce, Robert J.
    ,
    Yarosh, Yelena
    DOI: 10.1175/1520-0477(2001)082<0205:ARTGHH>2.3.CO;2
    Publisher: American Meteorological Society
    Abstract: A system has been developed and implemented that merges pixel resolution (~4 km) infrared (IR) satellite data from all available geostationary meteorological satellites into a global (60°N?60°S) product. The resulting research?quality, nearly seamless global array of information is made possible by recent work by Joyce et al., who developed a technique to correct IR temperatures at targets far from satellite nadir. At such locations, IR temperatures are colder than if identical features were measured at a target near satellite nadir. This correction procedure yields a dataset that is considerably more amenable to quantitative manipulation than if the data from the individual satellites were merely spliced together. Several unique features of this product exist. First, the data from individual geostationary satellites have been merged to form nearly seamless maps after correcting the IR brightness temperatures for viewing angle effects. Second, with the availability of IR data from the Meteosat?5 satellite (currently positioned at a subsatellite longitude of 63°E), globally complete (60°N?60°S) fields can be produced. Third, the data have been transformed from the native satellite projection of each individual geostationary satellite and have been remapped to a uniform latitude/longitude grid. Fourth, globally merged datasets of full resolution IR brightness temperature have been produced routinely every half hour since November 1998. Fifth, seven days of globally merged, half?hourly data are available on a rotating archive that is maintained by the Climate Prediction Center Web page (http: /www.cpc.ncep.noaa.gov/products/global?precip/html/web.html). Unfortunately, international agreement prevents us from distributing Meteosat data within three days of real time, so the data availability is delayed appropriately. Finally, these data are permanently saved at the National Climatic Data Center in Asheville, North Carolina, beginning with data in mid?September of 1999. In this paper, the authors briefly describe the merging methodology and describe key aspects of the merged product. Present and potential applications of this dataset are also discussed. Applications include near?real time global disaster monitoring and mitigation and assimilation of these data into numerical weather prediction models and research, among others.
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      A Real–Time Global Half–Hourly Pixel–Resolution Infrared Dataset and Its Applications

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4161808
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    • Bulletin of the American Meteorological Society

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    contributor authorJanowiak, John E.
    contributor authorJoyce, Robert J.
    contributor authorYarosh, Yelena
    date accessioned2017-06-09T14:42:56Z
    date available2017-06-09T14:42:56Z
    date copyright2001/02/01
    date issued2001
    identifier issn0003-0007
    identifier otherams-25066.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4161808
    description abstractA system has been developed and implemented that merges pixel resolution (~4 km) infrared (IR) satellite data from all available geostationary meteorological satellites into a global (60°N?60°S) product. The resulting research?quality, nearly seamless global array of information is made possible by recent work by Joyce et al., who developed a technique to correct IR temperatures at targets far from satellite nadir. At such locations, IR temperatures are colder than if identical features were measured at a target near satellite nadir. This correction procedure yields a dataset that is considerably more amenable to quantitative manipulation than if the data from the individual satellites were merely spliced together. Several unique features of this product exist. First, the data from individual geostationary satellites have been merged to form nearly seamless maps after correcting the IR brightness temperatures for viewing angle effects. Second, with the availability of IR data from the Meteosat?5 satellite (currently positioned at a subsatellite longitude of 63°E), globally complete (60°N?60°S) fields can be produced. Third, the data have been transformed from the native satellite projection of each individual geostationary satellite and have been remapped to a uniform latitude/longitude grid. Fourth, globally merged datasets of full resolution IR brightness temperature have been produced routinely every half hour since November 1998. Fifth, seven days of globally merged, half?hourly data are available on a rotating archive that is maintained by the Climate Prediction Center Web page (http: /www.cpc.ncep.noaa.gov/products/global?precip/html/web.html). Unfortunately, international agreement prevents us from distributing Meteosat data within three days of real time, so the data availability is delayed appropriately. Finally, these data are permanently saved at the National Climatic Data Center in Asheville, North Carolina, beginning with data in mid?September of 1999. In this paper, the authors briefly describe the merging methodology and describe key aspects of the merged product. Present and potential applications of this dataset are also discussed. Applications include near?real time global disaster monitoring and mitigation and assimilation of these data into numerical weather prediction models and research, among others.
    publisherAmerican Meteorological Society
    titleA Real–Time Global Half–Hourly Pixel–Resolution Infrared Dataset and Its Applications
    typeJournal Paper
    journal volume82
    journal issue2
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(2001)082<0205:ARTGHH>2.3.CO;2
    journal fristpage205
    journal lastpage217
    treeBulletin of the American Meteorological Society:;2001:;volume( 082 ):;issue: 002
    contenttypeFulltext
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