The role that trace substances play in the radiant energy balance of the atmosphere
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Los gases y las partículas y/o líquidos suspendidos en la atmósfera existen en cantidades muy pequeñas, sin embargo, absorben, tanto radiación solar como terrestre. En consecuencia, generan divergencias del flujo radiante que influyen en el perfil vertical de la temperatura. En este trabajo se presenta una comparación de la eficiencia de los diferentes absorbedores H₂O vapor de agua (H₂ O)₂, CO₂,O₃ y aerosoles.
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