Cosmogenic ³⁵S measurements in the Tibetan Plateau to quantify glacier snowmelt

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Cosmogenic ³⁵S measurements in the Tibetan Plateau to quantify glacier snowmelt

The cosmogenic radionuclide ³⁵S (t₁/₂ ~ 87 days) is a unique tracer for high-altitude air mass and has been used extensively to understand stratospheric air mass mixing. In this paper, we investigate if ³⁵S can be utilized as an independent tracer to quantify glacier melt. We report the first measur...

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Bibliographic Details
Main Authors:	Priyadarshi, Antra, Hill-Falkenthal, Jason, Thiemens, Mark, Zhang, Zhisheng, Lin, Mang, Chan, Chuen-yu, Kang, Shichang
Format:	Article
Published:	American Geophysical Union 2014
Subjects:	Cosmogenic Sulfur-35; Tibetan glacier melt; climate change; Nam Co lake
Online Access:	https://eprints.nottingham.ac.uk/47240/

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