The Cryosphere
The Cryosphere
TC
Articles | Volume 15, issue 1
Articles | Volume 15, issue 1
https://doi.org/10.5194/tc-15-95-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-15-95-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 15, issue 1
Research article
 | 
06 Jan 2021
Research article |  | 06 Jan 2021

Central Himalayan tree-ring isotopes reveal increasing regional heterogeneity and enhancement in ice mass loss since the 1960s

Nilendu Singh, Mayank Shekhar, Jayendra Singh, Anil K. Gupta, Achim Bräuning, Christoph Mayr, and Mohit Singhal

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Latest update: 20 Nov 2024
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Short summary
Tree-ring isotope records from the central Himalaya provided a basis for previously lacking regional multi-century glacier mass balance (MB) reconstruction. Isotopic and climate coherency analyses specify an eastward-declining influence of the westerlies, an increase in east–west climate heterogeneity, and an increase in ice mass loss since the 1960s. Reasons for this are attributed to anthropogenic climate change, including concurrent alterations in atmospheric circulation patterns.
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