Structure and evolution of the drainage system of a Himalayan debris-covered glacier, and its relationship with patterns of mass loss
Funding for Sarah Thompson as provided by the European Commission FP7-MC-IEF grant PIEF-GA-2012-330805, and for Lindsey Nicholson by the Austrian Science Fund (FWF) Elise Richter Grant (V309-N26). Financial support for fieldwork in 2009 was provided by the University Centre in Svalbard and a Royal G...
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Online Access: | http://hdl.handle.net/10023/11733 https://doi.org/10.5194/tc-11-2247-2017 |
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ftstandrewserep:oai:research-repository.st-andrews.ac.uk:10023/11733 2023-07-02T03:32:20+02:00 Structure and evolution of the drainage system of a Himalayan debris-covered glacier, and its relationship with patterns of mass loss Benn, Douglas I. Thompson, Sarah Gulley, Jason Mertes, Jordan Luckman, Adrian Nicholson, Lindsey University of St Andrews. School of Geography & Sustainable Development University of St Andrews. Bell-Edwards Geographic Data Institute 2017-09-25T08:30:15Z 18 application/pdf http://hdl.handle.net/10023/11733 https://doi.org/10.5194/tc-11-2247-2017 eng eng The Cryosphere Benn , D I , Thompson , S , Gulley , J , Mertes , J , Luckman , A & Nicholson , L 2017 , ' Structure and evolution of the drainage system of a Himalayan debris-covered glacier, and its relationship with patterns of mass loss ' , The Cryosphere , vol. 11 , pp. 2247-2264 . https://doi.org/10.5194/tc-11-2247-2017 1994-0416 PURE: 251137684 PURE UUID: 01cd1713-b0c9-4e5c-bcf6-9c7bf58b1af4 Scopus: 85029794101 WOS: 000411471000001 ORCID: /0000-0002-3604-0886/work/64697385 http://hdl.handle.net/10023/11733 https://doi.org/10.5194/tc-11-2247-2017 © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Glacier change Himalayan Glaciation Debris-covered glaciers GE Environmental Sciences DAS BDC GE Journal article 2017 ftstandrewserep https://doi.org/10.5194/tc-11-2247-2017 2023-06-13T18:30:41Z Funding for Sarah Thompson as provided by the European Commission FP7-MC-IEF grant PIEF-GA-2012-330805, and for Lindsey Nicholson by the Austrian Science Fund (FWF) Elise Richter Grant (V309-N26). Financial support for fieldwork in 2009 was provided by the University Centre in Svalbard and a Royal Geographical Society fieldwork grant to Sarah Thompson. TerraSAR-X data were kindly provided by the German Aerospace Center (DLR) under project HYD0178. The meteorological data were collected within the Ev-K2-CNR SHARE Project, funded by contributions from the Italian National Research Council and the Italian Ministry of Foreign Affairs. We provide the first synoptic view of the drainage system of a Himalayan debris-covered glacier and its evolution through time, based on speleological exploration and satellite image analysis of Ngozumpa Glacier, Nepal. The drainage system has several linked components: 1) a seasonal subglacial drainage system below the upper ablation zone; 2) supraglacial channels allowing efficient meltwater transport across parts of the upper ablation zone; 3) sub-marginal channels, allowing long-distance transport of meltwater; 4) perched ponds, which intermittently store meltwater prior to evacuation via the englacial drainage system; 5) englacial cut-and-closure conduits, which may undergo repeated cycles of abandonment and reactivation; 6) a 'base-level' lake system (Spillway Lake) dammed behind the terminal moraine. The distribution and relative importance of these elements has evolved through time, in response to sustained negative mass balance. The area occupied by perched ponds has expanded upglacier at the expense of supraglacial channels, and Spillway Lake has grown as more of the glacier surface ablates to base level. Subsurface processes play a governing role in creating, maintaining and shutting down exposures of ice at the glacier surface, with a major impact on spatial patterns and rates of surface mass loss. Comparison of our results with observations on other glaciers indicate ... Article in Journal/Newspaper glacier Svalbard The Cryosphere University Centre in Svalbard University of St Andrews: Digital Research Repository Level Lake ENVELOPE(-101.227,-101.227,56.457,56.457) Nicholson ENVELOPE(78.236,78.236,-68.612,-68.612) Svalbard The Cryosphere 11 5 2247 2264 |
institution |
Open Polar |
collection |
University of St Andrews: Digital Research Repository |
op_collection_id |
ftstandrewserep |
language |
English |
topic |
Glacier change Himalayan Glaciation Debris-covered glaciers GE Environmental Sciences DAS BDC GE |
spellingShingle |
Glacier change Himalayan Glaciation Debris-covered glaciers GE Environmental Sciences DAS BDC GE Benn, Douglas I. Thompson, Sarah Gulley, Jason Mertes, Jordan Luckman, Adrian Nicholson, Lindsey Structure and evolution of the drainage system of a Himalayan debris-covered glacier, and its relationship with patterns of mass loss |
topic_facet |
Glacier change Himalayan Glaciation Debris-covered glaciers GE Environmental Sciences DAS BDC GE |
description |
Funding for Sarah Thompson as provided by the European Commission FP7-MC-IEF grant PIEF-GA-2012-330805, and for Lindsey Nicholson by the Austrian Science Fund (FWF) Elise Richter Grant (V309-N26). Financial support for fieldwork in 2009 was provided by the University Centre in Svalbard and a Royal Geographical Society fieldwork grant to Sarah Thompson. TerraSAR-X data were kindly provided by the German Aerospace Center (DLR) under project HYD0178. The meteorological data were collected within the Ev-K2-CNR SHARE Project, funded by contributions from the Italian National Research Council and the Italian Ministry of Foreign Affairs. We provide the first synoptic view of the drainage system of a Himalayan debris-covered glacier and its evolution through time, based on speleological exploration and satellite image analysis of Ngozumpa Glacier, Nepal. The drainage system has several linked components: 1) a seasonal subglacial drainage system below the upper ablation zone; 2) supraglacial channels allowing efficient meltwater transport across parts of the upper ablation zone; 3) sub-marginal channels, allowing long-distance transport of meltwater; 4) perched ponds, which intermittently store meltwater prior to evacuation via the englacial drainage system; 5) englacial cut-and-closure conduits, which may undergo repeated cycles of abandonment and reactivation; 6) a 'base-level' lake system (Spillway Lake) dammed behind the terminal moraine. The distribution and relative importance of these elements has evolved through time, in response to sustained negative mass balance. The area occupied by perched ponds has expanded upglacier at the expense of supraglacial channels, and Spillway Lake has grown as more of the glacier surface ablates to base level. Subsurface processes play a governing role in creating, maintaining and shutting down exposures of ice at the glacier surface, with a major impact on spatial patterns and rates of surface mass loss. Comparison of our results with observations on other glaciers indicate ... |
author2 |
University of St Andrews. School of Geography & Sustainable Development University of St Andrews. Bell-Edwards Geographic Data Institute |
format |
Article in Journal/Newspaper |
author |
Benn, Douglas I. Thompson, Sarah Gulley, Jason Mertes, Jordan Luckman, Adrian Nicholson, Lindsey |
author_facet |
Benn, Douglas I. Thompson, Sarah Gulley, Jason Mertes, Jordan Luckman, Adrian Nicholson, Lindsey |
author_sort |
Benn, Douglas I. |
title |
Structure and evolution of the drainage system of a Himalayan debris-covered glacier, and its relationship with patterns of mass loss |
title_short |
Structure and evolution of the drainage system of a Himalayan debris-covered glacier, and its relationship with patterns of mass loss |
title_full |
Structure and evolution of the drainage system of a Himalayan debris-covered glacier, and its relationship with patterns of mass loss |
title_fullStr |
Structure and evolution of the drainage system of a Himalayan debris-covered glacier, and its relationship with patterns of mass loss |
title_full_unstemmed |
Structure and evolution of the drainage system of a Himalayan debris-covered glacier, and its relationship with patterns of mass loss |
title_sort |
structure and evolution of the drainage system of a himalayan debris-covered glacier, and its relationship with patterns of mass loss |
publishDate |
2017 |
url |
http://hdl.handle.net/10023/11733 https://doi.org/10.5194/tc-11-2247-2017 |
long_lat |
ENVELOPE(-101.227,-101.227,56.457,56.457) ENVELOPE(78.236,78.236,-68.612,-68.612) |
geographic |
Level Lake Nicholson Svalbard |
geographic_facet |
Level Lake Nicholson Svalbard |
genre |
glacier Svalbard The Cryosphere University Centre in Svalbard |
genre_facet |
glacier Svalbard The Cryosphere University Centre in Svalbard |
op_relation |
The Cryosphere Benn , D I , Thompson , S , Gulley , J , Mertes , J , Luckman , A & Nicholson , L 2017 , ' Structure and evolution of the drainage system of a Himalayan debris-covered glacier, and its relationship with patterns of mass loss ' , The Cryosphere , vol. 11 , pp. 2247-2264 . https://doi.org/10.5194/tc-11-2247-2017 1994-0416 PURE: 251137684 PURE UUID: 01cd1713-b0c9-4e5c-bcf6-9c7bf58b1af4 Scopus: 85029794101 WOS: 000411471000001 ORCID: /0000-0002-3604-0886/work/64697385 http://hdl.handle.net/10023/11733 https://doi.org/10.5194/tc-11-2247-2017 |
op_rights |
© Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. |
op_doi |
https://doi.org/10.5194/tc-11-2247-2017 |
container_title |
The Cryosphere |
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11 |
container_issue |
5 |
container_start_page |
2247 |
op_container_end_page |
2264 |
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1770271879540506624 |