Identifying the relationship between buried ice and the persistence of snow cover in the Dry Andes of Argentina
In the Dry Andes of Argentina, rock glaciers and buried ice play a fundamental role in the regional water budget. However, the driving forces for growing and sustaining these ice features are not readily understood. This study aims to explore potential climate forcing by investigating snow distribut...
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ftunivdelaware:oai:udspace.udel.edu:19716/28160 2023-06-11T04:12:33+02:00 Identifying the relationship between buried ice and the persistence of snow cover in the Dry Andes of Argentina MacDonald, Claire 2020-09-17T22:07:38Z application/pdf https://udspace.udel.edu/handle/19716/28160 en eng University of Delaware https://login.udel.idm.oclc.org/login?url=https://www.proquest.com/docview/2452128310?accountid=10457 1222906384 https://udspace.udel.edu/handle/19716/28160 Buried Ice Dry Andes Rock Glaciers Snow Accumulation Thesis 2020 ftunivdelaware 2023-05-01T12:53:30Z In the Dry Andes of Argentina, rock glaciers and buried ice play a fundamental role in the regional water budget. However, the driving forces for growing and sustaining these ice features are not readily understood. This study aims to explore potential climate forcing by investigating snow distribution over time and comparing it with maps of known rock glaciers and modeled zones of permafrost in the El Altar valley of San Juan, Argentina. Using remotely sensed imagery from LandSat satellites, data were converted to snow extent using the Normalized Difference Snow Index model. Results indicate a strong seasonal cycle of snow cover, with peak coverage in July or August, and snow completely melting during the austral summer months. Statistical analysis of snow cover with known rock glaciers suggests a relationship between their location and higher levels of snow accumulation. However, when comparing the average snow accumulation for areas designated as containing or possibly containing permafrost, no such relationship was found. Tritium data taken from ice samples suggest that the rock glaciers either have not been accumulating new ice since the 1950s, or that any recent accumulation since that time has already melted in the prevailing climate. Thus, we are able to infer that the snow gathering on the glaciers is not feeding them at this time. However, it is still possible that the higher levels of snow accumulation found on glaciers compared to areas outside their boundaries indicate that the snow is insulating them from further melting and sustaining them even if it is not contributing to their long-term growth. O'Neal, Michael A. Hanson, Brian M.S. University of Delaware, Department of Earth Sciences Thesis Ice permafrost The University of Delaware Library Institutional Repository Austral San Juan Argentina |
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The University of Delaware Library Institutional Repository |
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ftunivdelaware |
language |
English |
topic |
Buried Ice Dry Andes Rock Glaciers Snow Accumulation |
spellingShingle |
Buried Ice Dry Andes Rock Glaciers Snow Accumulation MacDonald, Claire Identifying the relationship between buried ice and the persistence of snow cover in the Dry Andes of Argentina |
topic_facet |
Buried Ice Dry Andes Rock Glaciers Snow Accumulation |
description |
In the Dry Andes of Argentina, rock glaciers and buried ice play a fundamental role in the regional water budget. However, the driving forces for growing and sustaining these ice features are not readily understood. This study aims to explore potential climate forcing by investigating snow distribution over time and comparing it with maps of known rock glaciers and modeled zones of permafrost in the El Altar valley of San Juan, Argentina. Using remotely sensed imagery from LandSat satellites, data were converted to snow extent using the Normalized Difference Snow Index model. Results indicate a strong seasonal cycle of snow cover, with peak coverage in July or August, and snow completely melting during the austral summer months. Statistical analysis of snow cover with known rock glaciers suggests a relationship between their location and higher levels of snow accumulation. However, when comparing the average snow accumulation for areas designated as containing or possibly containing permafrost, no such relationship was found. Tritium data taken from ice samples suggest that the rock glaciers either have not been accumulating new ice since the 1950s, or that any recent accumulation since that time has already melted in the prevailing climate. Thus, we are able to infer that the snow gathering on the glaciers is not feeding them at this time. However, it is still possible that the higher levels of snow accumulation found on glaciers compared to areas outside their boundaries indicate that the snow is insulating them from further melting and sustaining them even if it is not contributing to their long-term growth. O'Neal, Michael A. Hanson, Brian M.S. University of Delaware, Department of Earth Sciences |
format |
Thesis |
author |
MacDonald, Claire |
author_facet |
MacDonald, Claire |
author_sort |
MacDonald, Claire |
title |
Identifying the relationship between buried ice and the persistence of snow cover in the Dry Andes of Argentina |
title_short |
Identifying the relationship between buried ice and the persistence of snow cover in the Dry Andes of Argentina |
title_full |
Identifying the relationship between buried ice and the persistence of snow cover in the Dry Andes of Argentina |
title_fullStr |
Identifying the relationship between buried ice and the persistence of snow cover in the Dry Andes of Argentina |
title_full_unstemmed |
Identifying the relationship between buried ice and the persistence of snow cover in the Dry Andes of Argentina |
title_sort |
identifying the relationship between buried ice and the persistence of snow cover in the dry andes of argentina |
publisher |
University of Delaware |
publishDate |
2020 |
url |
https://udspace.udel.edu/handle/19716/28160 |
geographic |
Austral San Juan Argentina |
geographic_facet |
Austral San Juan Argentina |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_relation |
https://login.udel.idm.oclc.org/login?url=https://www.proquest.com/docview/2452128310?accountid=10457 1222906384 https://udspace.udel.edu/handle/19716/28160 |
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1768388487945388032 |