Disentangling source of moisture driving glacier dynamics and identification of 8.2 ka event: evidence from pore water isotopes, Western Himalaya

Two atmospheric circulation patterns, the Indian Summer Monsoon (ISM) and mid-latitude Westerlies control precipitation and thus glacier variability in the Himalaya. However, the role of the ISM and westerlies in controlling climate and thus past glacier variability in the Himalaya is poorly underst...

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Detalles Bibliográficos
Autores principales: Kumar, Om, Ramanathan, A. L., Bakke, Jostein, Kotlia, B. S., Shrivastava, J. P.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7501258/
https://www.ncbi.nlm.nih.gov/pubmed/32948802
http://dx.doi.org/10.1038/s41598-020-71686-4

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7501258/
https://www.ncbi.nlm.nih.gov/pubmed/32948802
http://dx.doi.org/10.1038/s41598-020-71686-4

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