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...

Descripción completa

Detalles Bibliográficos
Autores principales: Zhu, Liping, Lü, Xinmiao, Wang, Junbo, Peng, Ping, Kasper, Thomas, Daut, Gerhard, Haberzettl, Torsten, Frenzel, Peter, Li, Quan, Yang, Ruimin, Schwalb, Antje, Mäusbacher, Roland
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4543934/
https://www.ncbi.nlm.nih.gov/pubmed/26294226
http://dx.doi.org/10.1038/srep13318

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4543934/
https://www.ncbi.nlm.nih.gov/pubmed/26294226
http://dx.doi.org/10.1038/srep13318

Ejemplares similares