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    Thermography for Estimating Near-Surface Soil Moisture under Developing Crop Canopies

    Source: Journal of Applied Meteorology:;1979:;volume( 019 ):;issue: 003::page 324
    Author:
    Heilman, J. L.
    ,
    Moore, D. G.
    DOI: 10.1175/1520-0450(1980)019<0324:TFENSS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Previous investigations of thermal infrared techniques using remote sensors (thermography) for estimating soil water content have been limited primarily to bare soil. Ground-based and aircraft investigations were conducted to evaluate the potential for extending the thermography approach to developing crop canopies. A significant exponential relationship was found between the volumetric soil water content in the 0?4 cm soil layer and the diurnal difference between surface soil temperature measured at 0230 and 1330 LST (satellite overpass times of NASA's Heat Capacity Mapping Mission-HCMM). Surface soil temperatures were estimated using minimum air temperature, percent cover of the canopy and remote measurements of canopy temperature. Results of the investigation demonstrated that thermography can potentially be used to estimate soil temperature and soil moisture throughout a complete growing season for a number of different crops and soils.
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      Thermography for Estimating Near-Surface Soil Moisture under Developing Crop Canopies

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4233410
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    • Journal of Applied Meteorology

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    contributor authorHeilman, J. L.
    contributor authorMoore, D. G.
    date accessioned2017-06-09T17:40:24Z
    date available2017-06-09T17:40:24Z
    date copyright1980/03/01
    date issued1979
    identifier issn0021-8952
    identifier otherams-9874.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4233410
    description abstractPrevious investigations of thermal infrared techniques using remote sensors (thermography) for estimating soil water content have been limited primarily to bare soil. Ground-based and aircraft investigations were conducted to evaluate the potential for extending the thermography approach to developing crop canopies. A significant exponential relationship was found between the volumetric soil water content in the 0?4 cm soil layer and the diurnal difference between surface soil temperature measured at 0230 and 1330 LST (satellite overpass times of NASA's Heat Capacity Mapping Mission-HCMM). Surface soil temperatures were estimated using minimum air temperature, percent cover of the canopy and remote measurements of canopy temperature. Results of the investigation demonstrated that thermography can potentially be used to estimate soil temperature and soil moisture throughout a complete growing season for a number of different crops and soils.
    publisherAmerican Meteorological Society
    titleThermography for Estimating Near-Surface Soil Moisture under Developing Crop Canopies
    typeJournal Paper
    journal volume19
    journal issue3
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1980)019<0324:TFENSS>2.0.CO;2
    journal fristpage324
    journal lastpage328
    treeJournal of Applied Meteorology:;1979:;volume( 019 ):;issue: 003
    contenttypeFulltext
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