Climatic limits to headwall retreat in the Khumbu Himalaya, eastern Nepal

Ice-free bedrock headwalls are widespread landforms of many glacial landscapes, but their formation and evolution are not well understood. Here, I present observations from the Khumbu Himalaya, eastern Nepal, of a distinct elevation zone that aligns the base of many steep headwalls with the highest...

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Published in:Geology
Main Author: Scherler, Dirk
Format: Article in Journal/Newspaper
Language:unknown
Published: Geological Society of America 2014
Subjects:
Ice
Online Access:https://doi.org/10.1130/G35975.1
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spelling ftcaltechauth:oai:authors.library.caltech.edu:7bb59-xxs02 2023-12-31T10:07:53+01:00 Climatic limits to headwall retreat in the Khumbu Himalaya, eastern Nepal Scherler, Dirk 2014-11 https://doi.org/10.1130/G35975.1 unknown Geological Society of America https://doi.org/10.1130/G35975.1 oai:authors.library.caltech.edu:7bb59-xxs02 eprintid:53169 resolverid:CaltechAUTHORS:20150105-101146422 info:eu-repo/semantics/closedAccess Other Geology, 42(11), 1019-1022, (2014-11) info:eu-repo/semantics/article 2014 ftcaltechauth https://doi.org/10.1130/G35975.1 2023-12-01T11:40:48Z Ice-free bedrock headwalls are widespread landforms of many glacial landscapes, but their formation and evolution are not well understood. Here, I present observations from the Khumbu Himalaya, eastern Nepal, of a distinct elevation zone that aligns the base of many steep headwalls with the highest predicted frost-cracking intensity (FCI). Below this zone, median ice-free hillslope angles are ≤40° and similar to those of other areas in the Himalaya, where threshold hillslopes that are close to the critical angle of stability have been inferred. At higher elevations, ice-free hillslopes of different rock types have median slope angles of ∼50°–55°, suggesting threshold hillslopes with higher rock mass strength, possibly related to the presence of deep-reaching permafrost. High-altitude meteorological data combined with FCI models support frost cracking as a mechanism for headwall retreat by undercutting of threshold headwalls, while glacial transport inhibits the accumulation of scree deposits at their base. This mechanism could account for continued headwall retreat as long as climatic conditions enable frost cracking near the base of headwalls that are high enough to sustain glaciers at their base, even if subglacial erosion is minor. © 2014 Geological Society of America. First published online September 26, 2014. Meteorological data were provided by the National Center for Atmospheric Research (NCAR) Earth Observing Laboratory under sponsorship of the National Science Foundation (http://data.eol.ucar.edu/). Original meteorological data were collected and are provided within the framework of the Ev-K2-CNR and Nepal Academy of Science and Technology Joint Scientific and Technological Research Project, funded by Italian Ministries and National Research Council through the Ev-K2-CNR Committee. ASTER GDEM is a product of the Ministry of Economy, Trade, and Industry of Japan and of NASA. Constructive reviews by R.S. Anderson, T.C. Hales, and D. Burbank helped improve the manuscript. Article in Journal/Newspaper Ice permafrost Caltech Authors (California Institute of Technology) Geology 42 11 1019 1022
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
description Ice-free bedrock headwalls are widespread landforms of many glacial landscapes, but their formation and evolution are not well understood. Here, I present observations from the Khumbu Himalaya, eastern Nepal, of a distinct elevation zone that aligns the base of many steep headwalls with the highest predicted frost-cracking intensity (FCI). Below this zone, median ice-free hillslope angles are ≤40° and similar to those of other areas in the Himalaya, where threshold hillslopes that are close to the critical angle of stability have been inferred. At higher elevations, ice-free hillslopes of different rock types have median slope angles of ∼50°–55°, suggesting threshold hillslopes with higher rock mass strength, possibly related to the presence of deep-reaching permafrost. High-altitude meteorological data combined with FCI models support frost cracking as a mechanism for headwall retreat by undercutting of threshold headwalls, while glacial transport inhibits the accumulation of scree deposits at their base. This mechanism could account for continued headwall retreat as long as climatic conditions enable frost cracking near the base of headwalls that are high enough to sustain glaciers at their base, even if subglacial erosion is minor. © 2014 Geological Society of America. First published online September 26, 2014. Meteorological data were provided by the National Center for Atmospheric Research (NCAR) Earth Observing Laboratory under sponsorship of the National Science Foundation (http://data.eol.ucar.edu/). Original meteorological data were collected and are provided within the framework of the Ev-K2-CNR and Nepal Academy of Science and Technology Joint Scientific and Technological Research Project, funded by Italian Ministries and National Research Council through the Ev-K2-CNR Committee. ASTER GDEM is a product of the Ministry of Economy, Trade, and Industry of Japan and of NASA. Constructive reviews by R.S. Anderson, T.C. Hales, and D. Burbank helped improve the manuscript.
format Article in Journal/Newspaper
author Scherler, Dirk
spellingShingle Scherler, Dirk
Climatic limits to headwall retreat in the Khumbu Himalaya, eastern Nepal
author_facet Scherler, Dirk
author_sort Scherler, Dirk
title Climatic limits to headwall retreat in the Khumbu Himalaya, eastern Nepal
title_short Climatic limits to headwall retreat in the Khumbu Himalaya, eastern Nepal
title_full Climatic limits to headwall retreat in the Khumbu Himalaya, eastern Nepal
title_fullStr Climatic limits to headwall retreat in the Khumbu Himalaya, eastern Nepal
title_full_unstemmed Climatic limits to headwall retreat in the Khumbu Himalaya, eastern Nepal
title_sort climatic limits to headwall retreat in the khumbu himalaya, eastern nepal
publisher Geological Society of America
publishDate 2014
url https://doi.org/10.1130/G35975.1
genre Ice
permafrost
genre_facet Ice
permafrost
op_source Geology, 42(11), 1019-1022, (2014-11)
op_relation https://doi.org/10.1130/G35975.1
oai:authors.library.caltech.edu:7bb59-xxs02
eprintid:53169
resolverid:CaltechAUTHORS:20150105-101146422
op_rights info:eu-repo/semantics/closedAccess
Other
op_doi https://doi.org/10.1130/G35975.1
container_title Geology
container_volume 42
container_issue 11
container_start_page 1019
op_container_end_page 1022
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