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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
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Medientyp |
Artikel
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Sprache |
Englisch
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Digitales Dokument |
PDF |
Erschienen |
In: GRA - Volume 11 (2009) |
Datensatznummer |
250025502
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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. |
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