Tree-ring crossdates for a First Millennium AD advance of Tebenkof Glacier, southern Alaska
Abstract Tree-ring crossdates from glacially killed logs show that Tebenkof Glacier advanced into a forefield forest in the AD 710s and 720s. Recession from this First Millennium AD (FMA) advance occurred before the 950s, after which the ice margin readvanced in the 1280s to 1320s at the start of th...
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Cambridge University Press (CUP)
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crcambridgeupr:10.1016/j.yqres.2008.09.005 2024-09-15T18:07:32+00:00 Tree-ring crossdates for a First Millennium AD advance of Tebenkof Glacier, southern Alaska Barclay, David J. Wiles, Gregory C. Calkin, Parker E. 2009 http://dx.doi.org/10.1016/j.yqres.2008.09.005 http://api.elsevier.com/content/article/PII:S003358940800118X?httpAccept=text/xml http://api.elsevier.com/content/article/PII:S003358940800118X?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400014708 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Quaternary Research volume 71, issue 1, page 22-26 ISSN 0033-5894 1096-0287 journal-article 2009 crcambridgeupr https://doi.org/10.1016/j.yqres.2008.09.005 2024-08-28T04:03:10Z Abstract Tree-ring crossdates from glacially killed logs show that Tebenkof Glacier advanced into a forefield forest in the AD 710s and 720s. Recession from this First Millennium AD (FMA) advance occurred before the 950s, after which the ice margin readvanced in the 1280s to 1320s at the start of the Little Ice Age (LIA). A more extensive LIA advance was underway from the 1640s to 1670s, and the terminus stayed at or near its LIA maximum until the 1890s. These are the first absolute tree-ring crossdates for a FMA glacier advance in North America and support growing evidence from northwestern North America and Europe for a significant cool interval in the centuries around AD 500. Article in Journal/Newspaper glacier Alaska Cambridge University Press Quaternary Research 71 1 22 26 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Abstract Tree-ring crossdates from glacially killed logs show that Tebenkof Glacier advanced into a forefield forest in the AD 710s and 720s. Recession from this First Millennium AD (FMA) advance occurred before the 950s, after which the ice margin readvanced in the 1280s to 1320s at the start of the Little Ice Age (LIA). A more extensive LIA advance was underway from the 1640s to 1670s, and the terminus stayed at or near its LIA maximum until the 1890s. These are the first absolute tree-ring crossdates for a FMA glacier advance in North America and support growing evidence from northwestern North America and Europe for a significant cool interval in the centuries around AD 500. |
format |
Article in Journal/Newspaper |
author |
Barclay, David J. Wiles, Gregory C. Calkin, Parker E. |
spellingShingle |
Barclay, David J. Wiles, Gregory C. Calkin, Parker E. Tree-ring crossdates for a First Millennium AD advance of Tebenkof Glacier, southern Alaska |
author_facet |
Barclay, David J. Wiles, Gregory C. Calkin, Parker E. |
author_sort |
Barclay, David J. |
title |
Tree-ring crossdates for a First Millennium AD advance of Tebenkof Glacier, southern Alaska |
title_short |
Tree-ring crossdates for a First Millennium AD advance of Tebenkof Glacier, southern Alaska |
title_full |
Tree-ring crossdates for a First Millennium AD advance of Tebenkof Glacier, southern Alaska |
title_fullStr |
Tree-ring crossdates for a First Millennium AD advance of Tebenkof Glacier, southern Alaska |
title_full_unstemmed |
Tree-ring crossdates for a First Millennium AD advance of Tebenkof Glacier, southern Alaska |
title_sort |
tree-ring crossdates for a first millennium ad advance of tebenkof glacier, southern alaska |
publisher |
Cambridge University Press (CUP) |
publishDate |
2009 |
url |
http://dx.doi.org/10.1016/j.yqres.2008.09.005 http://api.elsevier.com/content/article/PII:S003358940800118X?httpAccept=text/xml http://api.elsevier.com/content/article/PII:S003358940800118X?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400014708 |
genre |
glacier Alaska |
genre_facet |
glacier Alaska |
op_source |
Quaternary Research volume 71, issue 1, page 22-26 ISSN 0033-5894 1096-0287 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1016/j.yqres.2008.09.005 |
container_title |
Quaternary Research |
container_volume |
71 |
container_issue |
1 |
container_start_page |
22 |
op_container_end_page |
26 |
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1810444918706929664 |