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...
| Main Authors: | , , , , , , |
|---|---|
| Format: | Article |
| Published: |
American Geophysical Union
2014
|
| Subjects: | |
| Online Access: | https://eprints.nottingham.ac.uk/47240/ |