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Damian J. Barrett and Luigi J. Renzullo

radiation by atmospheric water vapor in spectral bands centered approximately on 11 and 12 μ m, respectively. They are simple in form (representing linearizations of the thermal infrared radiative transfer equation) and are thus easy to implement operationally for large-scale estimation of LST. SWA performance is essentially governed by the way in which the algorithm handles atmospheric water concentration, satellite view angle, and surface emissivity effects. Atmospheric water vapor may be estimated

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