Absorbing aerosols exert a warming or a cooling effect on the Earth’s system, depending on the ci...
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Measuring evaporation (E) with lysimeters is costly and prone to numerous errors. By comparing th...
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A potentially optimal description of the evolution of a simple model atmosphere is investigated. ...
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NRLMSIS® 2.0 is an empirical atmospheric model that extends from the ground to the exobase and de...
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The lower-thermosphere–ionosphere (LTI) system consists of the upper atmosphere and the lower par...
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