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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

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_4543934

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

About this item

Full title

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

Publisher

London: Nature Publishing Group UK

Journal title

Scientific reports, 2015-08, Vol.5 (1), p.13318-13318, Article 13318

Language

English

Formats

Publication information

Publisher

London: Nature Publishing Group UK

More information

Scope and Contents

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...

Alternative Titles

Full title

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

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_4543934

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_4543934

Other Identifiers

ISSN

2045-2322

E-ISSN

2045-2322

DOI

10.1038/srep13318

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