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    On the Use of GOES Thermal Data to Study Effects of Land Use on Diurnal Temperature Fluctuation

    Source: Journal of Climate and Applied Meteorology:;1984:;volume( 023 ):;issue: 003::page 426
    Author:
    Shih, S. F.
    ,
    Chen, E.
    DOI: 10.1175/1520-0450(1984)023<0426:OTUOGT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Geostationary Operational Environmental Satellite (GOES) infrared data were used to study the effect of land use on the diurnal surface temperature fluctuation. Five major land use types in southern Florida: the sandy soil agricultural area; the Everglades Agricultural Area (EAA); the conservation areas; the Natural Everglades Area (NEA); and Lake Okeechobee; were observed. The average daytime and nocturnal surface temperatures of sandy soil in agricultural areas was lower than that of organic soil in agricultural areas. The average temperature of organic soil in agricultural areas was lower than that of organic soil in conservation areas. The surface temperature in the wet marsh area was much lower than that in a large water-storage lake. A land use change in the EAA, and an increase in the water storage in Lake Okeechobee and the conservation areas could influence the microclimate.
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      On the Use of GOES Thermal Data to Study Effects of Land Use on Diurnal Temperature Fluctuation

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4145824
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    • Journal of Climate and Applied Meteorology

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    contributor authorShih, S. F.
    contributor authorChen, E.
    date accessioned2017-06-09T14:00:04Z
    date available2017-06-09T14:00:04Z
    date copyright1984/03/01
    date issued1984
    identifier issn0733-3021
    identifier otherams-10680.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145824
    description abstractGeostationary Operational Environmental Satellite (GOES) infrared data were used to study the effect of land use on the diurnal surface temperature fluctuation. Five major land use types in southern Florida: the sandy soil agricultural area; the Everglades Agricultural Area (EAA); the conservation areas; the Natural Everglades Area (NEA); and Lake Okeechobee; were observed. The average daytime and nocturnal surface temperatures of sandy soil in agricultural areas was lower than that of organic soil in agricultural areas. The average temperature of organic soil in agricultural areas was lower than that of organic soil in conservation areas. The surface temperature in the wet marsh area was much lower than that in a large water-storage lake. A land use change in the EAA, and an increase in the water storage in Lake Okeechobee and the conservation areas could influence the microclimate.
    publisherAmerican Meteorological Society
    titleOn the Use of GOES Thermal Data to Study Effects of Land Use on Diurnal Temperature Fluctuation
    typeJournal Paper
    journal volume23
    journal issue3
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1984)023<0426:OTUOGT>2.0.CO;2
    journal fristpage426
    journal lastpage433
    treeJournal of Climate and Applied Meteorology:;1984:;volume( 023 ):;issue: 003
    contenttypeFulltext
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