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- W2173926365 abstract "AbstractEvaporation from water or soil surfaces and transpiration from plants combine to return available water at the surface layer back to the bulk atmosphere in a process called evapotranspiration. Much of our understanding of the complex feedback mechanisms between the Earth’s surface and the surrounding atmosphere is focused on quantifying this process. At its most fundamental level, evapotranspiration is the loss of water from a surface to the atmosphere, achieved through vaporization. The complex nature of the evaporative process, however, includes mechanisms such as turbulent transport, feedback between the surface and atmosphere, and the biophysical nature of transpiration – all of which combine to make both measurement and estimation a difficult task.KeywordsRoot Mean Square ErrorNormalize Difference Vegetation IndexLeaf Area IndexLatent Heat FluxLand Surface TemperatureThese keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves." @default.
- W2173926365 created "2016-06-24" @default.
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- W2173926365 date "2010-01-01" @default.
- W2173926365 modified "2023-09-26" @default.
- W2173926365 title "Multisensor Global Retrievals of Evapotranspiration for Climate Studies Using the Surface Energy Budget System" @default.
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- W2173926365 doi "https://doi.org/10.1007/978-1-4419-6749-7_33" @default.
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