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.
Masunaga, Seasonality and regionality of the Madden–Julian oscillation, Kelvin wave, and equatorial Rossby wave, Journal of the Atmospheric Sciences 64, 4400 (2007)
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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.