Reliability of a Fjord Glacier's Fluctuations for Paleoclimatic Reconstructions
Historical observations of fjord glaciers in southern Alaska suggest that their fluctuations may be asynchronous with one another and with climate. Possible causes for anomalous fjord glacier response to climatic changes involve the instabilities inherent in a calving terminus, the interaction of fj...
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Cambridge University Press (CUP)
1986
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crcambridgeupr:10.1016/0033-5894(86)90040-2 2024-06-09T07:46:07+00:00 Reliability of a Fjord Glacier's Fluctuations for Paleoclimatic Reconstructions Mann, Daniel H. 1986 http://dx.doi.org/10.1016/0033-5894(86)90040-2 http://api.elsevier.com/content/article/PII:0033589486900402?httpAccept=text/xml http://api.elsevier.com/content/article/PII:0033589486900402?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400022754 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Quaternary Research volume 25, issue 1, page 10-24 ISSN 0033-5894 1096-0287 journal-article 1986 crcambridgeupr https://doi.org/10.1016/0033-5894(86)90040-2 2024-05-15T13:04:58Z Historical observations of fjord glaciers in southern Alaska suggest that their fluctuations may be asynchronous with one another and with climate. Possible causes for anomalous fjord glacier response to climatic changes involve the instabilities inherent in a calving terminus, the interaction of fjord geometry with the extent of the calving terminus, and the intersection of low-lying snow line by a thickening glacier. The Lituya glacier system in southeast Alaska is analyzed with reference to these phenomena to test the reliability of its Holocene glacial deposits as paleoclimatic records. This fjord glacier is shown to have been probably free of major, nonclimatic responses during the Holocene except for an insensitive period of up to 1000 yr that followed calving retreats. The insensitive period has no functional effect on how the relatively coarse geologic record is interpreted in terms of paleoclimate. However, it makes impossible any inference of climatic trends from this glacier's behavior in historical times. Fjord glacier deposits can be dependable records of paleoclimate but each glacier requires careful scrutiny. Anomalous glacier responses to climate are most likely to occur in fjords of complex geometry, in regions of relatively low snow line, and where glaciers terminate at fjord mouths bordering the open sea. Article in Journal/Newspaper glacier glaciers Alaska Cambridge University Press Quaternary Research 25 1 10 24 |
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English |
description |
Historical observations of fjord glaciers in southern Alaska suggest that their fluctuations may be asynchronous with one another and with climate. Possible causes for anomalous fjord glacier response to climatic changes involve the instabilities inherent in a calving terminus, the interaction of fjord geometry with the extent of the calving terminus, and the intersection of low-lying snow line by a thickening glacier. The Lituya glacier system in southeast Alaska is analyzed with reference to these phenomena to test the reliability of its Holocene glacial deposits as paleoclimatic records. This fjord glacier is shown to have been probably free of major, nonclimatic responses during the Holocene except for an insensitive period of up to 1000 yr that followed calving retreats. The insensitive period has no functional effect on how the relatively coarse geologic record is interpreted in terms of paleoclimate. However, it makes impossible any inference of climatic trends from this glacier's behavior in historical times. Fjord glacier deposits can be dependable records of paleoclimate but each glacier requires careful scrutiny. Anomalous glacier responses to climate are most likely to occur in fjords of complex geometry, in regions of relatively low snow line, and where glaciers terminate at fjord mouths bordering the open sea. |
format |
Article in Journal/Newspaper |
author |
Mann, Daniel H. |
spellingShingle |
Mann, Daniel H. Reliability of a Fjord Glacier's Fluctuations for Paleoclimatic Reconstructions |
author_facet |
Mann, Daniel H. |
author_sort |
Mann, Daniel H. |
title |
Reliability of a Fjord Glacier's Fluctuations for Paleoclimatic Reconstructions |
title_short |
Reliability of a Fjord Glacier's Fluctuations for Paleoclimatic Reconstructions |
title_full |
Reliability of a Fjord Glacier's Fluctuations for Paleoclimatic Reconstructions |
title_fullStr |
Reliability of a Fjord Glacier's Fluctuations for Paleoclimatic Reconstructions |
title_full_unstemmed |
Reliability of a Fjord Glacier's Fluctuations for Paleoclimatic Reconstructions |
title_sort |
reliability of a fjord glacier's fluctuations for paleoclimatic reconstructions |
publisher |
Cambridge University Press (CUP) |
publishDate |
1986 |
url |
http://dx.doi.org/10.1016/0033-5894(86)90040-2 http://api.elsevier.com/content/article/PII:0033589486900402?httpAccept=text/xml http://api.elsevier.com/content/article/PII:0033589486900402?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400022754 |
genre |
glacier glaciers Alaska |
genre_facet |
glacier glaciers Alaska |
op_source |
Quaternary Research volume 25, issue 1, page 10-24 ISSN 0033-5894 1096-0287 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1016/0033-5894(86)90040-2 |
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Quaternary Research |
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25 |
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10 |
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24 |
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1801375870817927168 |