The calving glaciers of southern South America

Calving glaciers constitute a great majority of all glaciers in Patagonia and Tierra del Fuego, and are dynamically important elements of the southern South American icefields. Large numbers of tidewater glaciers calve into the Chilean fjords, and many outlet glaciers terminate in proglacial lakes....

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Main Authors: Warren, Charles Raymond, Aniya, M
Format: Article in Journal/Newspaper
Language:English
Published: 1999
Subjects:
Online Access:https://risweb.st-andrews.ac.uk/portal/en/researchoutput/the-calving-glaciers-of-southern-south-america(e1d1bfdd-e1e2-45bc-a718-a661d15a6cba).html
http://www.scopus.com/inward/record.url?scp=0033406256&partnerID=8YFLogxK
id ftunstandrewcris:oai:risweb.st-andrews.ac.uk:publications/e1d1bfdd-e1e2-45bc-a718-a661d15a6cba
record_format openpolar
spelling ftunstandrewcris:oai:risweb.st-andrews.ac.uk:publications/e1d1bfdd-e1e2-45bc-a718-a661d15a6cba 2023-05-15T18:33:04+02:00 The calving glaciers of southern South America Warren, Charles Raymond Aniya, M 1999-10 https://risweb.st-andrews.ac.uk/portal/en/researchoutput/the-calving-glaciers-of-southern-south-america(e1d1bfdd-e1e2-45bc-a718-a661d15a6cba).html http://www.scopus.com/inward/record.url?scp=0033406256&partnerID=8YFLogxK eng eng info:eu-repo/semantics/restrictedAccess Warren , C R & Aniya , M 1999 , ' The calving glaciers of southern South America ' , Global and Planetary Change , vol. 22 , pp. 59-77 . calving glaciers Patagonia South America CHILEAN PATAGONIA PIO-XI YOUNGER DRYAS SAN-RAFAEL RECENT FLUCTUATIONS LAST GLACIATION CLIMATIC-CHANGE ICEFIELD HOLOCENE ANDES article 1999 ftunstandrewcris 2021-12-26T14:10:18Z Calving glaciers constitute a great majority of all glaciers in Patagonia and Tierra del Fuego, and are dynamically important elements of the southern South American icefields. Large numbers of tidewater glaciers calve into the Chilean fjords, and many outlet glaciers terminate in proglacial lakes. Most probably, all are temperate and grounded, with steep mass balance gradients. A majority of these glaciers remained largely unknown to science until very recently. This paper reviews recent research in the region in the context of glaciological and Quaternary debates, and discusses current understanding and uncertainties. During the 20th century most glaciers have retreated, but the particular dynamics of calving glaciers have produced some striking exceptions to this regional trend, producing sustained advances (e.g., Glacier Pio XI, Glaciar Perito Moreno), accelerated retreats (e.g., Glaciar O'Higgins, Glaciar Marinelli), and long-maintained stillstands of glaciers with very high accumulation area ratios (e.g., Glaciar Calvo). The relative importance of climatic, topographic, and glaciodynamic controls on regional patterns of glacier fluctuation remain an enigma, especially in the Cordillera Darwin, but space-borne radar imagery is now yielding much information. Key research themes in recent years include: (1) glacier inventory work using remotely-sensed data; (2) calving rates and calving dynamics, particularly the contrast between calving rates in tidewater and freshwater; (3) glacier/climate relationships, both in historic and longer timeframes; and (4) geographic contrasts in glacier behaviour, especially the relative significance of precipitation and temperature for glacier mass balance in this region of steep climatic gradients. Many intriguing and important questions cannot presently be resolved due to the paucity of mass balance and climatic data, but current research is yielding data that have regional, interhemispheric and theoretical significance. (C) 1999 Elsevier Science B.V. All rights reserved. Article in Journal/Newspaper Tidewater Tierra del Fuego University of St Andrews: Research Portal Marinelli ENVELOPE(-62.900,-62.900,-64.267,-64.267) Moreno ENVELOPE(-62.300,-62.300,-64.083,-64.083) Patagonia
institution Open Polar
collection University of St Andrews: Research Portal
op_collection_id ftunstandrewcris
language English
topic calving glaciers
Patagonia
South America
CHILEAN PATAGONIA
PIO-XI
YOUNGER DRYAS
SAN-RAFAEL
RECENT FLUCTUATIONS
LAST GLACIATION
CLIMATIC-CHANGE
ICEFIELD
HOLOCENE
ANDES
spellingShingle calving glaciers
Patagonia
South America
CHILEAN PATAGONIA
PIO-XI
YOUNGER DRYAS
SAN-RAFAEL
RECENT FLUCTUATIONS
LAST GLACIATION
CLIMATIC-CHANGE
ICEFIELD
HOLOCENE
ANDES
Warren, Charles Raymond
Aniya, M
The calving glaciers of southern South America
topic_facet calving glaciers
Patagonia
South America
CHILEAN PATAGONIA
PIO-XI
YOUNGER DRYAS
SAN-RAFAEL
RECENT FLUCTUATIONS
LAST GLACIATION
CLIMATIC-CHANGE
ICEFIELD
HOLOCENE
ANDES
description Calving glaciers constitute a great majority of all glaciers in Patagonia and Tierra del Fuego, and are dynamically important elements of the southern South American icefields. Large numbers of tidewater glaciers calve into the Chilean fjords, and many outlet glaciers terminate in proglacial lakes. Most probably, all are temperate and grounded, with steep mass balance gradients. A majority of these glaciers remained largely unknown to science until very recently. This paper reviews recent research in the region in the context of glaciological and Quaternary debates, and discusses current understanding and uncertainties. During the 20th century most glaciers have retreated, but the particular dynamics of calving glaciers have produced some striking exceptions to this regional trend, producing sustained advances (e.g., Glacier Pio XI, Glaciar Perito Moreno), accelerated retreats (e.g., Glaciar O'Higgins, Glaciar Marinelli), and long-maintained stillstands of glaciers with very high accumulation area ratios (e.g., Glaciar Calvo). The relative importance of climatic, topographic, and glaciodynamic controls on regional patterns of glacier fluctuation remain an enigma, especially in the Cordillera Darwin, but space-borne radar imagery is now yielding much information. Key research themes in recent years include: (1) glacier inventory work using remotely-sensed data; (2) calving rates and calving dynamics, particularly the contrast between calving rates in tidewater and freshwater; (3) glacier/climate relationships, both in historic and longer timeframes; and (4) geographic contrasts in glacier behaviour, especially the relative significance of precipitation and temperature for glacier mass balance in this region of steep climatic gradients. Many intriguing and important questions cannot presently be resolved due to the paucity of mass balance and climatic data, but current research is yielding data that have regional, interhemispheric and theoretical significance. (C) 1999 Elsevier Science B.V. All rights reserved.
format Article in Journal/Newspaper
author Warren, Charles Raymond
Aniya, M
author_facet Warren, Charles Raymond
Aniya, M
author_sort Warren, Charles Raymond
title The calving glaciers of southern South America
title_short The calving glaciers of southern South America
title_full The calving glaciers of southern South America
title_fullStr The calving glaciers of southern South America
title_full_unstemmed The calving glaciers of southern South America
title_sort calving glaciers of southern south america
publishDate 1999
url https://risweb.st-andrews.ac.uk/portal/en/researchoutput/the-calving-glaciers-of-southern-south-america(e1d1bfdd-e1e2-45bc-a718-a661d15a6cba).html
http://www.scopus.com/inward/record.url?scp=0033406256&partnerID=8YFLogxK
long_lat ENVELOPE(-62.900,-62.900,-64.267,-64.267)
ENVELOPE(-62.300,-62.300,-64.083,-64.083)
geographic Marinelli
Moreno
Patagonia
geographic_facet Marinelli
Moreno
Patagonia
genre Tidewater
Tierra del Fuego
genre_facet Tidewater
Tierra del Fuego
op_source Warren , C R & Aniya , M 1999 , ' The calving glaciers of southern South America ' , Global and Planetary Change , vol. 22 , pp. 59-77 .
op_rights info:eu-repo/semantics/restrictedAccess
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