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    Estimation of Regional Surface Resistance to Evapotranspiration from NDVI and Thermal-IR AVHRR Data 

    Source: Journal of Applied Meteorology:;1989:;volume( 028 ):;issue: 004:;page 276
    Author(s): Nemani, Ramakrishna R.; Running, Steven W.
    Publisher: American Meteorological Society
    Abstract: Infrared surface temperatures from satellite sensors have been used to infer evaporation and soil moisture distribution over large areas. However, surface energy partitioning to latent versus sensible heat changes with ...
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    Parameterization and Sensitivity Analysis of the BIOME–BGC Terrestrial Ecosystem Model: Net Primary Production Controls 

    Source: Earth Interactions:;2000:;volume( 004 ):;issue: 003:;page 1
    Author(s): White, Michael A.; Thornton, Peter E.; Running, Steven W.; Nemani, Ramakrishna R.
    Publisher: American Meteorological Society
    Abstract: Ecosystem simulation models use descriptive input parameters to establish the physiology, biochemistry, structure, and allocation patterns of vegetation functional types, or biomes. For single-stand simulations it is ...
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    Why Is Remote Sensing of Amazon Forest Greenness So Challenging? 

    Source: Earth Interactions:;2012:;volume( 016 ):;issue: 007:;page 1
    Author(s): Samanta, Arindam; Ganguly, Sangram; Vermote, Eric; Nemani, Ramakrishna R.; Myneni, Ranga B.
    Publisher: American Meteorological Society
    Abstract: he prevalence of clouds and aerosols and their impact on satellite-measured greenness levels of forests in southern and central Amazonia are explored in this article using 10 years of NASA Moderate Resolution Imaging ...
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    Physical Climate Response to a Reduction of Anthropogenic Climate Forcing 

    Source: Earth Interactions:;2010:;volume( 014 ):;issue: 007:;page 1
    Author(s): Samanta, Arindam; Anderson, Bruce T.; Ganguly, Sangram; Knyazikhin, Yuri; Nemani, Ramakrishna R.; Myneni, Ranga B.
    Publisher: American Meteorological Society
    Abstract: Recent research indicates that the warming of the climate system resulting from increased greenhouse gas (GHG) emissions over the next century will persist for many centuries after the cessation of these emissions, principally ...
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