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    MODIS Consistent Vegetation Parameter Specifications and Their Impacts on Regional Climate Simulations

    Source: Journal of Climate:;2014:;volume( 027 ):;issue: 022::page 8578
    Author:
    Xu, Min
    ,
    Liang, Xin-Zhong
    ,
    Samel, Arthur
    ,
    Gao, Wei
    DOI: 10.1175/JCLI-D-14-00082.1
    Publisher: American Meteorological Society
    Abstract: consistent set of Moderate Resolution Imaging Spectroradiometer (MODIS) vegetation parameters, including leaf and stem area index (LAI and SAI, respectively), land-cover category (LCC), fractional vegetation cover (FVC), and albedo parameterization are developed, and their impacts on North American regional climate are evaluated based on 10-yr Climate?Weather and Research Forecasting Model (CWRF) simulations. As compared with the previous Advanced Very High Resolution Radiometer (AVHRR) set, MODIS LCC increases grassland and cropland fractions in the central Great Plains and Midwest, respectively. Evergreen needleleaf forest converts to mixed forest in the Southeast, and mixed forest converts to evergreen needleleaf in Canada. FVC decreases by 0.05?0.3 over the central Great Plains but increases by 0.1?0.35 over the northern Rocky Mountains, Canada, and the U.S. Southeast. MODIS LAI is less than AVHRR by 2?6, except in the central Great Plains, eastern Rocky Mountains, and central Mexico. LCC and FVC changes over the central Great Plains reduce CWRF warm biases by 0.71°C and wet biases by 0.36 mm day?1. Large LAI reductions cause latent and sensible heat fluxes to decrease by 0.78?5.81 and 0.91?6.54 W m?2, respectively. They also lessen cold biases over the Gulf States and Southeast and wet biases over the North American monsoon region and Canada during summer. In densely vegetated regions including eastern Canada, the Ohio Valley, and the mid-Atlantic region, spring and summer precipitation decreases and temperature increases result from LAI reductions that cause positive evapotranspiration?precipitation?soil moisture feedbacks. Conversely, precipitation and temperature decreases in sparely vegetated regions, such as the Great Plains, result from FVC reductions that cause negative albedo?evapotranspiration?precipitation?soil moisture feedbacks.
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      MODIS Consistent Vegetation Parameter Specifications and Their Impacts on Regional Climate Simulations

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4223337
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    contributor authorXu, Min
    contributor authorLiang, Xin-Zhong
    contributor authorSamel, Arthur
    contributor authorGao, Wei
    date accessioned2017-06-09T17:10:02Z
    date available2017-06-09T17:10:02Z
    date copyright2014/11/01
    date issued2014
    identifier issn0894-8755
    identifier otherams-80444.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4223337
    description abstractconsistent set of Moderate Resolution Imaging Spectroradiometer (MODIS) vegetation parameters, including leaf and stem area index (LAI and SAI, respectively), land-cover category (LCC), fractional vegetation cover (FVC), and albedo parameterization are developed, and their impacts on North American regional climate are evaluated based on 10-yr Climate?Weather and Research Forecasting Model (CWRF) simulations. As compared with the previous Advanced Very High Resolution Radiometer (AVHRR) set, MODIS LCC increases grassland and cropland fractions in the central Great Plains and Midwest, respectively. Evergreen needleleaf forest converts to mixed forest in the Southeast, and mixed forest converts to evergreen needleleaf in Canada. FVC decreases by 0.05?0.3 over the central Great Plains but increases by 0.1?0.35 over the northern Rocky Mountains, Canada, and the U.S. Southeast. MODIS LAI is less than AVHRR by 2?6, except in the central Great Plains, eastern Rocky Mountains, and central Mexico. LCC and FVC changes over the central Great Plains reduce CWRF warm biases by 0.71°C and wet biases by 0.36 mm day?1. Large LAI reductions cause latent and sensible heat fluxes to decrease by 0.78?5.81 and 0.91?6.54 W m?2, respectively. They also lessen cold biases over the Gulf States and Southeast and wet biases over the North American monsoon region and Canada during summer. In densely vegetated regions including eastern Canada, the Ohio Valley, and the mid-Atlantic region, spring and summer precipitation decreases and temperature increases result from LAI reductions that cause positive evapotranspiration?precipitation?soil moisture feedbacks. Conversely, precipitation and temperature decreases in sparely vegetated regions, such as the Great Plains, result from FVC reductions that cause negative albedo?evapotranspiration?precipitation?soil moisture feedbacks.
    publisherAmerican Meteorological Society
    titleMODIS Consistent Vegetation Parameter Specifications and Their Impacts on Regional Climate Simulations
    typeJournal Paper
    journal volume27
    journal issue22
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-14-00082.1
    journal fristpage8578
    journal lastpage8596
    treeJournal of Climate:;2014:;volume( 027 ):;issue: 022
    contenttypeFulltext
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