Simulation of the annual cycle of climate with a thermodynamic numerical model
Contenido principal del artículo
Resumen
Se presenta un modelo hemisférico numérico termodinámico en el que el ciclo anual del albedo de superficie se genera internamente, junto con la temperatura troposferica media, la temperatura en la superficie de los continentes, y la radiación de onda corta y larga. El modelo también incluye como variables las anomalias de la temperatura de la superficie de los oceanos, la evaporaci6n en la superficie, el calor sensible cedido por la superficie a la atm6sfera, el calor de condensaci6n de vapor de agua en las nubes, la extension horizontal de la nubosidad y la componente horizontal del viento. Los valores calculados del ciclo anual del albedo de superficie, de la temperatura a los 700 mb y de las componentes de la radiaci6n muestran, en general, buena concordancia con los valores observados.
Detalles del artículo
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