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Titel Flow around the Tibetan Plateau: A shallow water model approach
VerfasserIn T. Frisius, K. Fraedrich, H. Borth, O. Bothe, X. Zhu
Konferenz EGU General Assembly 2009
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 11 (2009)
Datensatznummer 250025502
 
Zusammenfassung
A global high resolution shallow water model is used to simulate the atmospheric flow regimes around the Tibetan Plateau as a response to large scale forcing. The Tibetan Plateau is introduced as an isolated large scale topographic obstacle affecting the large scale flow anomalies prescribed by up- and downstream vorticity sources, which are related to low frequency teleconnection patterns (like North Atlantic Oscillation or Pacific-North America pattern). The response regimes are associated with dry and wet conditions observed over the eastern Tibetan Plateau. In this sense we aim at a minimum complexity model of interactions between large scale atmospheric flow anomalies and the Tibetan Plateau.