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.
(A1) to substitute for 8 ⟨Slm(t0)S∗ lm(t0 + t)⟩ on the left-hand side, and noticing that the forcing is symmetric such that ⟨Slm(t0)S∗ lm(t0 + t)⟩ = ⟨Slm(t0)S∗ lm(t0 − t)⟩
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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.