Characterizes Earth's infrared background as isotropic fluctuations with upper-bound decorrelation scales of 400 km and 2.5 days from a fitted stochastic energy balance model.
Hasselmann, Stochastic climate models part I
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Earth's Infrared Background
Characterizes Earth's infrared background as isotropic fluctuations with upper-bound decorrelation scales of 400 km and 2.5 days from a fitted stochastic energy balance model.