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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| Format: | Article |
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American Geophysical Union
2014
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| Online Access: | https://eprints.nottingham.ac.uk/47240/ |
| _version_ | 1848797497656344576 |
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| author | Priyadarshi, Antra Hill-Falkenthal, Jason Thiemens, Mark Zhang, Zhisheng Lin, Mang Chan, Chuen-yu Kang, Shichang |
| author_facet | Priyadarshi, Antra Hill-Falkenthal, Jason Thiemens, Mark Zhang, Zhisheng Lin, Mang Chan, Chuen-yu Kang, Shichang |
| author_sort | Priyadarshi, Antra |
| building | Nottingham Research Data Repository |
| collection | Online Access |
| description | 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 measurements of ³⁵S in samples collected from the Tibetan Plateau during 2009–2012 with an aim to interpret ³⁵S in atmospheric particles and their deposition over glacier and snowmelts. Our measurements show that ³⁵S activity in the aerosol phase varies from 116 ± 13 to 2229 ± 52 atoms/m³ resulting in higher values during winter–spring and lower values during summer–autumn. This seasonality is likely due to higher mixing of ³⁵S-rich stratospheric air masses during winter–spring and ³⁵S-poor air masses from the Bay of Bengal during the Asian summer monsoon. The average ³⁵S activity in the Zhadang glacier was found to be 3–8 times higher relative to the nearby lake water. The main source of ³⁵S activity in the Zhadang glacier is atmospheric deposition, whereas both atmospheric deposition and glacier snowmelt are the primary sources in the Nam Co Lake. The focus of this study is to quantitatively determine the spatial and temporal variations in glacier snowmelt. In the future, extensive sampling of aerosols and snow is required for determining ³⁵S in combination with stable oxygen isotopes in sulfate to better understand the glacier melt process and hydrological cycle on the Tibetan Plateau. |
| first_indexed | 2025-11-14T20:04:49Z |
| format | Article |
| id | nottingham-47240 |
| institution | University of Nottingham Malaysia Campus |
| institution_category | Local University |
| last_indexed | 2025-11-14T20:04:49Z |
| publishDate | 2014 |
| publisher | American Geophysical Union |
| recordtype | eprints |
| repository_type | Digital Repository |
| spelling | nottingham-472402020-05-04T16:46:54Z https://eprints.nottingham.ac.uk/47240/ Cosmogenic ³⁵S measurements in the Tibetan Plateau to quantify glacier snowmelt Priyadarshi, Antra Hill-Falkenthal, Jason Thiemens, Mark Zhang, Zhisheng Lin, Mang Chan, Chuen-yu Kang, Shichang 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 measurements of ³⁵S in samples collected from the Tibetan Plateau during 2009–2012 with an aim to interpret ³⁵S in atmospheric particles and their deposition over glacier and snowmelts. Our measurements show that ³⁵S activity in the aerosol phase varies from 116 ± 13 to 2229 ± 52 atoms/m³ resulting in higher values during winter–spring and lower values during summer–autumn. This seasonality is likely due to higher mixing of ³⁵S-rich stratospheric air masses during winter–spring and ³⁵S-poor air masses from the Bay of Bengal during the Asian summer monsoon. The average ³⁵S activity in the Zhadang glacier was found to be 3–8 times higher relative to the nearby lake water. The main source of ³⁵S activity in the Zhadang glacier is atmospheric deposition, whereas both atmospheric deposition and glacier snowmelt are the primary sources in the Nam Co Lake. The focus of this study is to quantitatively determine the spatial and temporal variations in glacier snowmelt. In the future, extensive sampling of aerosols and snow is required for determining ³⁵S in combination with stable oxygen isotopes in sulfate to better understand the glacier melt process and hydrological cycle on the Tibetan Plateau. American Geophysical Union 2014-04-09 Article PeerReviewed Priyadarshi, Antra, Hill-Falkenthal, Jason, Thiemens, Mark, Zhang, Zhisheng, Lin, Mang, Chan, Chuen-yu and Kang, Shichang (2014) Cosmogenic ³⁵S measurements in the Tibetan Plateau to quantify glacier snowmelt. Journal of Geophysical Research: Atmospheres, 119 (7). pp. 4125-4135. ISSN 2169-8996 Cosmogenic Sulfur-35; Tibetan glacier melt; climate change; Nam Co lake http://onlinelibrary.wiley.com/doi/10.1002/2013JD019801/full doi:10.1002/2013jd019801 doi:10.1002/2013jd019801 |
| spellingShingle | Cosmogenic Sulfur-35; Tibetan glacier melt; climate change; Nam Co lake Priyadarshi, Antra Hill-Falkenthal, Jason Thiemens, Mark Zhang, Zhisheng Lin, Mang Chan, Chuen-yu Kang, Shichang Cosmogenic ³⁵S measurements in the Tibetan Plateau to quantify glacier snowmelt |
| title | Cosmogenic ³⁵S measurements in the Tibetan Plateau to quantify glacier snowmelt |
| title_full | Cosmogenic ³⁵S measurements in the Tibetan Plateau to quantify glacier snowmelt |
| title_fullStr | Cosmogenic ³⁵S measurements in the Tibetan Plateau to quantify glacier snowmelt |
| title_full_unstemmed | Cosmogenic ³⁵S measurements in the Tibetan Plateau to quantify glacier snowmelt |
| title_short | Cosmogenic ³⁵S measurements in the Tibetan Plateau to quantify glacier snowmelt |
| title_sort | cosmogenic ³⁵s measurements in the tibetan plateau to quantify glacier snowmelt |
| topic | Cosmogenic Sulfur-35; Tibetan glacier melt; climate change; Nam Co lake |
| url | https://eprints.nottingham.ac.uk/47240/ https://eprints.nottingham.ac.uk/47240/ https://eprints.nottingham.ac.uk/47240/ |