Articles | Volume 4, issue 3
https://doi.org/10.5194/wcd-4-809-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/wcd-4-809-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
15 Sep 2023
Research article |
| 15 Sep 2023
| 15 Sep 2023
Atmospheric response to cold wintertime Tibetan Plateau conditions over eastern Asia in climate models
Institute of Geography, Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland
Department of Earth and Environmental Sciences, University of Milano-Bicocca, Milan, Italy
Laboratoire de Météorologie Dynamique/IPSL, École Normale Supérieure, PSL Research University, Sorbonne Université, École Polytechnique, IP Paris, CNRS, Paris, France
Fabio D'Andrea
Laboratoire de Météorologie Dynamique/IPSL, École Normale Supérieure, PSL Research University, Sorbonne Université, École Polytechnique, IP Paris, CNRS, Paris, France
Paolo Davini
Istituto di Scienze dell'Atmosfera e del Clima (CNR-ISAC), Consiglio Nazionale delle Ricerche, Turin, Italy
Mostafa E. Hamouda
Astronomy and Meteorology Department, Faculty of Science, Cairo University, Cairo, Egypt
Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, Germany
Claudia Pasquero
Department of Earth and Environmental Sciences, University of Milano-Bicocca, Milan, Italy
Istituto di Scienze dell'Atmosfera e del Clima (CNR-ISAC), Consiglio Nazionale delle Ricerche, Turin, Italy
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Anna Napoli, Fabien Desbiolles, Antonio Parodi, and Claudia Pasquero
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Federico Fabiano, Virna L. Meccia, Paolo Davini, Paolo Ghinassi, and Susanna Corti
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Short summary
The differences between climate models can be exploited to infer how specific aspects of the climate influence the Earth system. This work analyses the effects of a negative temperature anomaly over the Tibetan Plateau on the winter atmospheric circulation. We show that models with a colder-than-average Tibetan Plateau present a reinforcement of the eastern Asian winter monsoon and discuss the atmospheric response to the enhanced transport of cold air from the continent toward the Pacific Ocean.
The differences between climate models can be exploited to infer how specific aspects of the...
