Delayed and rapid deglaciation of alpine valleys in the Sawatch Range, southern Rocky Mountains, USA
We quantify retreat rates for three alpine glaciers in the Sawatch Range of the southern Rocky Mountains following the Last Glacial Maximum using 10 Be ages from ice-sculpted, valley-floor bedrock transects and statistical analysis via the BACON program in R. Glacier retreat in the Sawatch Range fro...
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ftcopernicus:oai:publications.copernicus.org:gchrond85279 2023-05-15T16:41:08+02:00 Delayed and rapid deglaciation of alpine valleys in the Sawatch Range, southern Rocky Mountains, USA Tulenko, Joseph P. Caffee, William Schweinsberg, Avriel D. Briner, Jason P. Leonard, Eric M. 2020-05-12 application/pdf https://doi.org/10.5194/gchron-2020-13 https://gchron.copernicus.org/preprints/gchron-2020-13/ eng eng doi:10.5194/gchron-2020-13 https://gchron.copernicus.org/preprints/gchron-2020-13/ eISSN: 2628-3719 Text 2020 ftcopernicus https://doi.org/10.5194/gchron-2020-13 2020-07-20T16:22:11Z We quantify retreat rates for three alpine glaciers in the Sawatch Range of the southern Rocky Mountains following the Last Glacial Maximum using 10 Be ages from ice-sculpted, valley-floor bedrock transects and statistical analysis via the BACON program in R. Glacier retreat in the Sawatch Range from at (100 %) or near (~ 83 %) Last Glacial Maximum extents initiated between 16.3 and 15.6 ka and was complete by 14.2–13.7 ka at rates ranging between 9.9 and 19.8 m a −1 . Deglaciation in the Sawatch Range commenced ~ 2–3 kyr later than the onset of rising global CO 2 , but approximately in-step with rising temperatures observed in the North Atlantic region at the Heinrich Stadial 1/Bølling transition. Our results highlight a possible teleconnection between the North Atlantic sector and the southern Rocky Mountains. However, deglaciation in the Sawatch Range also approximately aligns with the timing of Great Basin pluvial lake lowering. Recent data-modeling comparison efforts highlight the influence of the large North American ice sheets on climate in the western United States, and we hypothesize that recession of the North American ice sheets may have influenced the timing and rate of deglaciation in the Sawatch Range. While we cannot definitively argue for exclusively North Atlantic forcing or North American ice sheet forcing, our data demonstrate the importance of regional forcing mechanisms on past climate records. Text Ice Sheet North Atlantic Copernicus Publications: E-Journals |
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English |
description |
We quantify retreat rates for three alpine glaciers in the Sawatch Range of the southern Rocky Mountains following the Last Glacial Maximum using 10 Be ages from ice-sculpted, valley-floor bedrock transects and statistical analysis via the BACON program in R. Glacier retreat in the Sawatch Range from at (100 %) or near (~ 83 %) Last Glacial Maximum extents initiated between 16.3 and 15.6 ka and was complete by 14.2–13.7 ka at rates ranging between 9.9 and 19.8 m a −1 . Deglaciation in the Sawatch Range commenced ~ 2–3 kyr later than the onset of rising global CO 2 , but approximately in-step with rising temperatures observed in the North Atlantic region at the Heinrich Stadial 1/Bølling transition. Our results highlight a possible teleconnection between the North Atlantic sector and the southern Rocky Mountains. However, deglaciation in the Sawatch Range also approximately aligns with the timing of Great Basin pluvial lake lowering. Recent data-modeling comparison efforts highlight the influence of the large North American ice sheets on climate in the western United States, and we hypothesize that recession of the North American ice sheets may have influenced the timing and rate of deglaciation in the Sawatch Range. While we cannot definitively argue for exclusively North Atlantic forcing or North American ice sheet forcing, our data demonstrate the importance of regional forcing mechanisms on past climate records. |
format |
Text |
author |
Tulenko, Joseph P. Caffee, William Schweinsberg, Avriel D. Briner, Jason P. Leonard, Eric M. |
spellingShingle |
Tulenko, Joseph P. Caffee, William Schweinsberg, Avriel D. Briner, Jason P. Leonard, Eric M. Delayed and rapid deglaciation of alpine valleys in the Sawatch Range, southern Rocky Mountains, USA |
author_facet |
Tulenko, Joseph P. Caffee, William Schweinsberg, Avriel D. Briner, Jason P. Leonard, Eric M. |
author_sort |
Tulenko, Joseph P. |
title |
Delayed and rapid deglaciation of alpine valleys in the Sawatch Range, southern Rocky Mountains, USA |
title_short |
Delayed and rapid deglaciation of alpine valleys in the Sawatch Range, southern Rocky Mountains, USA |
title_full |
Delayed and rapid deglaciation of alpine valleys in the Sawatch Range, southern Rocky Mountains, USA |
title_fullStr |
Delayed and rapid deglaciation of alpine valleys in the Sawatch Range, southern Rocky Mountains, USA |
title_full_unstemmed |
Delayed and rapid deglaciation of alpine valleys in the Sawatch Range, southern Rocky Mountains, USA |
title_sort |
delayed and rapid deglaciation of alpine valleys in the sawatch range, southern rocky mountains, usa |
publishDate |
2020 |
url |
https://doi.org/10.5194/gchron-2020-13 https://gchron.copernicus.org/preprints/gchron-2020-13/ |
genre |
Ice Sheet North Atlantic |
genre_facet |
Ice Sheet North Atlantic |
op_source |
eISSN: 2628-3719 |
op_relation |
doi:10.5194/gchron-2020-13 https://gchron.copernicus.org/preprints/gchron-2020-13/ |
op_doi |
https://doi.org/10.5194/gchron-2020-13 |
_version_ |
1766031575291527168 |