Metadata
Author: WikiMatrix
Data
English[en]
This can be refined in the vertical to a one-dimensional radiative-convective model, which considers two processes of energy transport: upwelling and downwelling radiative transfer through atmospheric layers that both absorb and emit infrared radiation upward transport of heat by convection (especially important in the lower troposphere).
Spanish[es]
Esto puede ser refinado en vertical a un modelo radiativos-convectivos adimensional, que considera dos procesos de transporte de energía: Transferencia radiativa subiendo y bajando a través de las capas de la atmósfera, absorbiendo y emitiendo radiación infrarroja en ambos casos.