An efficient implementation of the two-scale model of sea surface thermal emission and atmospheric reflection is described. The model is applied in a study of the reflection of downwelling atmospheric radiation. Results show that reflected downwelling radiation can increase azimuthal variations of total observed brightnesses.
No takes yet. Share an insight, caveat, or question.
Joel T. Johnson (2006) studied this question.
Synapse has enriched 5 related papers. Consider them for comparative context: