Three-months extended and seasonal forecast of sea surface temperature anomalies for thermodynamic climate prediction
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Resumen
La ecuación de conservación de energía térmica aplicada a la capa de mezcla oceánica se utiliza para la predicción de las anomalías de la temperatura de la superficie del mar y de sus cambios mensuales para periodos extendidos de tres meses, así como para la predicción estacional de estas anomalías en los océanos Pacífico y Atlántico del Hemisferio Norte. La ecuación incluye el transporte horizontal de calor por corrientes oceánicas y por remolinos turbulentos, así como calentamiento por radiación de onda corta y larga, evaporación y calor sensible cedido a la atmósfera por transporte turbulento vertical. En este trabajo llevamos a cabo una verificación de las predicciones para el periodo de junio 1980 a mayo 1984; los resultados muestran que este modelo tiene cierta habilidad en la predicción de las anomalías de la temperatura de la superficie del mar de gran escala y de sus cambios mensuales para periodos extendidos de tres meses, así como en la predicción estacional de estas anomalías.
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