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Titel Baroclinic closure and stratosphere-troposphere exchange
VerfasserIn M. Juckes
Konferenz EGU General Assembly 2009
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 11 (2009)
Datensatznummer 250028385
 
Zusammenfassung
Recent work which throws light on the role of water vapour in determining the mean state of the mid-latitude atmosphere will be reviewed. The dominance of the meridional heat flux by large scale eddies led to the neglect of water vapour in many attempts to explain the mean structure of the atmosphere in the baroclinic zone. Taking water vapour into account brings convection into the picture. The convection also impacts on stratosphere troposphere-exchange.