Howard Barker
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A Functionalized Monte Carlo 3D Radiative Transfer Model: Radiative Effects of Clouds Over Reflecting Surfaces
A Simple FMC Algorithm: Flux as a Function of Surface Albedo This section develops an FMC algorithm that gets employed later to illustrate estimation of radiative quantities for cloud fields above reflecting surfaces. More specifically, this FMC uses a standard 3D MC RT model to compute solar cloud radiative effects as a function of surface albedo for a planar, uniform, Lambertian surface. For clarity, it is assumed that underlying surface albedos are spectrally and spatially constant.
Scaling Properties of Observed and Simulated Satellite Visible Radiances
Structure functions S , which are related to power spectra and used to study turbulence, were computed for GOES-13 visible radiances measured on 16-May-2015 over French Guiana and adjacent Atlantic Ocean. The nested Global Environmental Multiscale (GEM) numerical weather prediction (NWP) model was run for the same time and area.
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