Climate change on the Tibetan Plateau in response to shifting atmospheric circulation since the LGM

The Tibetan Plateau (TP) is primarily influenced by the northern hemispheric middle latitude Westerlies and the Indian summer monsoon (ISM). The extent, long-distance effects and potential long-term changes of these two atmospheric circulations are not yet fully understood. Here, we analyse modern a...

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Pubblicato in:Sci Rep
Autori principali: Zhu, Liping, Lü, Xinmiao, Wang, Junbo, Peng, Ping, Kasper, Thomas, Daut, Gerhard, Haberzettl, Torsten, Frenzel, Peter, Li, Quan, Yang, Ruimin, Schwalb, Antje, Mäusbacher, Roland
Natura: Artigo
Lingua:Inglês
Pubblicazione: Nature Publishing Group 2015
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Article
Accesso online:https://ncbi.nlm.nih.gov/pmc/articles/PMC4543934/
https://ncbi.nlm.nih.gov/pubmed/26294226
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep13318
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