Cargando…
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...
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: | |
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 |
Ejemplares similares
-
Recent Wetting and Glacier Expansion in the Northwest Himalaya and Karakoram
por: Yadav, Ram R., et al.
Publicado: (2017) -
Surface mass balance analysis at Naradu Glacier, Western Himalaya, India
por: Kumar, Rajesh, et al.
Publicado: (2021) -
Assessing controls on mass budget and surface velocity variations of glaciers in Western Himalaya
por: Bhushan, Shashank, et al.
Publicado: (2018) -
Modelling evolution of a large, glacier-fed lake in the Western Indian Himalaya
por: Gantayat, Prateek, et al.
Publicado: (2023) -
Climate projections for glacier change modelling over the Himalayas
por: Jury, Martin W., et al.
Publicado: (2019)