Climate Dynamics at Berkeley
Climate Dynamics at Berkeley
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Marysa M. Laguë
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Continental configuration controls the base-state water vapor greenhouse effect: lessons from half-land, half-water planets
Reduced terrestrial evaporation increases atmospheric water vapor by generating cloud feedbacks
Downwind control of oceanic air by land: the land wake and its sensitivity to CO2
Radiative feedbacks on land surface change and associated tropical precipitation shifts
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