Climatology and energy budget of the northern hemisphere middle stratosphere durind 1972
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La capa atmosférica de 10-2 mb (~30-43 km) recibe en invierno energía de dos fuentes diferentes: energía mecánica es llevada hacia arriba desde la tropósfera y desde la estratósfera baja, mientras que energía es generada in situ por las gradientes de calentamientos y enfriamientos radiactivos. Demostramos aquí, según datos para 1972, que la última energía gobierna en forma primaria el balance de energía de la estratósfera media al principio del invierno, mientras que la primera llega a ser de tamaño comparable, y a menudo dominante, a la mitad y al final del invierno. Las fuentes de energía radiactiva para el hemisferio de verano son muy pequeñas, ya que hay considerable compensación entre el calentamiento solar a través de la absorción por ozono y enfriamiento infrarrojo par bióxido de carbono y ozono. Ondas estacionarias y en movimiento aparecen claramente a los 5 y a los 2 mb en invierno, ya que mucho del caos de regiones bajas se filtra en la estratósfera baja; las ondas estacionarias a los 2 mb reflejan propiedades de la superficie más efectivamente que las configuraciones de flujo en niveles más bajos. Una onda moviéndose hacia el oeste, con un período aproximado de un mes se manifestó a principios de 1972.
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