Climate change on the Tibetan Plateau in response to shifting atmospheric circulation since the LGM
Climate change on the Tibetan Plateau in response to shifting atmospheric circulation since the LGM
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London: Nature Publishing Group UK
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Language
English
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London: Nature Publishing Group UK
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Contents
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 airborne pollen in a transition zone of seasonally...
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Climate change on the Tibetan Plateau in response to shifting atmospheric circulation since the LGM
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TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_4543934
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_4543934
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ISSN
2045-2322
E-ISSN
2045-2322
DOI
10.1038/srep13318