The last deglaciation of Alaska
We review available chronologies that constrain the timing of glacier fluctuations during the last deglaciation in Alaska. We address three questions relating to the last glacial termination: (i) How did the timing of glacier recession relate to buildup of global CO2, such as during the onset of CO2...
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Universidad de La Rioja
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ftunivriojaojs:oai:ojs.www.unirioja.es:article/3229 2024-10-13T14:06:24+00:00 The last deglaciation of Alaska La última deglaciación de Alaska Briner, J.P. Tulenko, J.P. kaufman, D.S. Young, N.E. Baichtal, J.F. Lesnek, A. 2017-09-15 application/pdf https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/3229 https://doi.org/10.18172/cig.3229 eng eng Universidad de La Rioja https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/3229/2906 https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/3229 doi:10.18172/cig.3229 Derechos de autor 2017 J.P. Briner, J.P. Tulenko, D.S. kaufman, N.E. Young, J.F. Baichtal, A. Lesnek Cuadernos de Investigación Geográfica; Vol. 43 No. 2 (2017); 429-448 Cuadernos de Investigación Geográfica; Vol. 43 Núm. 2 (2017); 429-448 1697-9540 0211-6820 10.18172/cig.vol43iss2 Alaska deglaciation glacier geochronology paleoclimate deglaciación glaciar geocronología paleoclima info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2017 ftunivriojaojs https://doi.org/10.18172/cig.322910.18172/cig.vol43iss2 2024-09-18T23:40:51Z We review available chronologies that constrain the timing of glacier fluctuations during the last deglaciation in Alaska. We address three questions relating to the last glacial termination: (i) How did the timing of glacier recession relate to buildup of global CO2, such as during the onset of CO2 rise at ~18 ka? (ii) Did glaciers fluctuate in synchrony with Heinrich Stadial 1 (18-14.6 ka)? And, (iii) what is the spatio-temporal pattern of glacier change during the climatically turbulent late glacial interval (14.6-11.7 ka)? The existing record is incomplete, yet reveals that most Alaskan glaciers experienced significant retreat (~40% of their Last Glacial Maximum lengths) prior to the onset of CO2 rise ~18 ka. This points to stronger insolation forcing of Alaskan glaciers compared to mid-latitude glaciers. Despite some glacier re-advances and standstills during Heinrich Stadial 1, most glaciers continued to recede. This suggests that glaciers in Alaska were relatively immune to the far-field effects of Atlantic meridional overturning circulation. Finally, the majority of glaciers (9 out of 14 available records) were up-valley of their late Holocene glacier extents during the Younger Dryas. Most of the sites with evidence for relatively extensive glaciers during the Younger Dryas are in southern Alaska, which may relate to moisture changes associated with the flooding of Bering Strait as much as it does to changes in North Atlantic Ocean circulation. Revisamos las cronologías disponibles que identifican la temporalidad de las fluctuaciones glaciares durante la última deglaciación en Alaska. Nos centramos en tres cuestiones relacionadas con el final de la última glaciación: (i) ¿Cómo se relaciona el momento de la recesión glaciar con el aumento global de CO2 hacia ~18ka? (ii) ¿Fluctuaron los glaciares en sincronía con el Stadial 1 de Heinrich (18-14.6 ka)? Y (iii) ¿Cuál es el patrón espacio-temporal del cambio glaciar durante el último intervalo glaciar climáticamente turbulento (14.6-11.7 ka)? El registro ... Article in Journal/Newspaper Bering Strait glacier glaciers North Atlantic Alaska Portal de Revistas de la Universidad de La Rioja Bering Strait Cuadernos de Investigación Geográfica 43 2 429 448 |
institution |
Open Polar |
collection |
Portal de Revistas de la Universidad de La Rioja |
op_collection_id |
ftunivriojaojs |
language |
English |
topic |
Alaska deglaciation glacier geochronology paleoclimate deglaciación glaciar geocronología paleoclima |
spellingShingle |
Alaska deglaciation glacier geochronology paleoclimate deglaciación glaciar geocronología paleoclima Briner, J.P. Tulenko, J.P. kaufman, D.S. Young, N.E. Baichtal, J.F. Lesnek, A. The last deglaciation of Alaska |
topic_facet |
Alaska deglaciation glacier geochronology paleoclimate deglaciación glaciar geocronología paleoclima |
description |
We review available chronologies that constrain the timing of glacier fluctuations during the last deglaciation in Alaska. We address three questions relating to the last glacial termination: (i) How did the timing of glacier recession relate to buildup of global CO2, such as during the onset of CO2 rise at ~18 ka? (ii) Did glaciers fluctuate in synchrony with Heinrich Stadial 1 (18-14.6 ka)? And, (iii) what is the spatio-temporal pattern of glacier change during the climatically turbulent late glacial interval (14.6-11.7 ka)? The existing record is incomplete, yet reveals that most Alaskan glaciers experienced significant retreat (~40% of their Last Glacial Maximum lengths) prior to the onset of CO2 rise ~18 ka. This points to stronger insolation forcing of Alaskan glaciers compared to mid-latitude glaciers. Despite some glacier re-advances and standstills during Heinrich Stadial 1, most glaciers continued to recede. This suggests that glaciers in Alaska were relatively immune to the far-field effects of Atlantic meridional overturning circulation. Finally, the majority of glaciers (9 out of 14 available records) were up-valley of their late Holocene glacier extents during the Younger Dryas. Most of the sites with evidence for relatively extensive glaciers during the Younger Dryas are in southern Alaska, which may relate to moisture changes associated with the flooding of Bering Strait as much as it does to changes in North Atlantic Ocean circulation. Revisamos las cronologías disponibles que identifican la temporalidad de las fluctuaciones glaciares durante la última deglaciación en Alaska. Nos centramos en tres cuestiones relacionadas con el final de la última glaciación: (i) ¿Cómo se relaciona el momento de la recesión glaciar con el aumento global de CO2 hacia ~18ka? (ii) ¿Fluctuaron los glaciares en sincronía con el Stadial 1 de Heinrich (18-14.6 ka)? Y (iii) ¿Cuál es el patrón espacio-temporal del cambio glaciar durante el último intervalo glaciar climáticamente turbulento (14.6-11.7 ka)? El registro ... |
format |
Article in Journal/Newspaper |
author |
Briner, J.P. Tulenko, J.P. kaufman, D.S. Young, N.E. Baichtal, J.F. Lesnek, A. |
author_facet |
Briner, J.P. Tulenko, J.P. kaufman, D.S. Young, N.E. Baichtal, J.F. Lesnek, A. |
author_sort |
Briner, J.P. |
title |
The last deglaciation of Alaska |
title_short |
The last deglaciation of Alaska |
title_full |
The last deglaciation of Alaska |
title_fullStr |
The last deglaciation of Alaska |
title_full_unstemmed |
The last deglaciation of Alaska |
title_sort |
last deglaciation of alaska |
publisher |
Universidad de La Rioja |
publishDate |
2017 |
url |
https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/3229 https://doi.org/10.18172/cig.3229 |
geographic |
Bering Strait |
geographic_facet |
Bering Strait |
genre |
Bering Strait glacier glaciers North Atlantic Alaska |
genre_facet |
Bering Strait glacier glaciers North Atlantic Alaska |
op_source |
Cuadernos de Investigación Geográfica; Vol. 43 No. 2 (2017); 429-448 Cuadernos de Investigación Geográfica; Vol. 43 Núm. 2 (2017); 429-448 1697-9540 0211-6820 10.18172/cig.vol43iss2 |
op_relation |
https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/3229/2906 https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/3229 doi:10.18172/cig.3229 |
op_rights |
Derechos de autor 2017 J.P. Briner, J.P. Tulenko, D.S. kaufman, N.E. Young, J.F. Baichtal, A. Lesnek |
op_doi |
https://doi.org/10.18172/cig.322910.18172/cig.vol43iss2 |
container_title |
Cuadernos de Investigación Geográfica |
container_volume |
43 |
container_issue |
2 |
container_start_page |
429 |
op_container_end_page |
448 |
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1812812550395396096 |