Reconstruction of recent climate change in Alaska from the Aurora Peak ice core, central Alaska
A 180.17 m ice core was drilled at Aurora Peak in the central part of the Alaska Range, Alaska, in 2008 to allow reconstruction of centennial-scale climate change in the northern North Pacific. The 10 m depth temperature in the borehole was −2.2 °C, which corresponded to the annual mean air temperat...
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ftdoajarticles:oai:doaj.org/article:e0ee8e7b46a04ade9add48770f2c6c0f 2023-05-15T13:09:47+02:00 Reconstruction of recent climate change in Alaska from the Aurora Peak ice core, central Alaska A. Tsushima S. Matoba T. Shiraiwa S. Okamoto H. Sasaki D. J. Solie K. Yoshikawa 2015-02-01T00:00:00Z https://doi.org/10.5194/cp-11-217-2015 https://doaj.org/article/e0ee8e7b46a04ade9add48770f2c6c0f EN eng Copernicus Publications http://www.clim-past.net/11/217/2015/cp-11-217-2015.pdf https://doaj.org/toc/1814-9324 https://doaj.org/toc/1814-9332 1814-9324 1814-9332 doi:10.5194/cp-11-217-2015 https://doaj.org/article/e0ee8e7b46a04ade9add48770f2c6c0f Climate of the Past, Vol 11, Iss 2, Pp 217-226 (2015) Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 article 2015 ftdoajarticles https://doi.org/10.5194/cp-11-217-2015 2022-12-31T12:54:32Z A 180.17 m ice core was drilled at Aurora Peak in the central part of the Alaska Range, Alaska, in 2008 to allow reconstruction of centennial-scale climate change in the northern North Pacific. The 10 m depth temperature in the borehole was −2.2 °C, which corresponded to the annual mean air temperature at the drilling site. In this ice core, there were many melt–refreeze layers due to high temperature and/or strong insolation during summer seasons. We analyzed stable hydrogen isotopes (δD) and chemical species in the ice core. The ice core age was determined by annual counts of δD and seasonal cycles of Na + , and we used reference horizons of tritium peaks in 1963 and 1964, major volcanic eruptions of Mount Spurr in 1992 and Mount Katmai in 1912, and a large forest fire in 2004 as age controls. Here, we show that the chronology of the Aurora Peak ice core from 95.61 m to the top corresponds to the period from 1900 to the summer season of 2008, with a dating error of ± 3 years. We estimated that the mean accumulation rate from 1997 to 2007 (except for 2004) was 2.04 m w.eq. yr -1 . Our results suggest that temporal variations in δD and annual accumulation rates are strongly related to shifts in the Pacific Decadal Oscillation index (PDOI). The remarkable increase in annual precipitation since the 1970s has likely been the result of enhanced storm activity associated with shifts in the PDOI during winter in the Gulf of Alaska. Article in Journal/Newspaper alaska range ice core Alaska Directory of Open Access Journals: DOAJ Articles Gulf of Alaska Pacific Aurora Peak ENVELOPE(144.200,144.200,-67.383,-67.383) Climate of the Past 11 2 217 226 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 |
spellingShingle |
Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 A. Tsushima S. Matoba T. Shiraiwa S. Okamoto H. Sasaki D. J. Solie K. Yoshikawa Reconstruction of recent climate change in Alaska from the Aurora Peak ice core, central Alaska |
topic_facet |
Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 |
description |
A 180.17 m ice core was drilled at Aurora Peak in the central part of the Alaska Range, Alaska, in 2008 to allow reconstruction of centennial-scale climate change in the northern North Pacific. The 10 m depth temperature in the borehole was −2.2 °C, which corresponded to the annual mean air temperature at the drilling site. In this ice core, there were many melt–refreeze layers due to high temperature and/or strong insolation during summer seasons. We analyzed stable hydrogen isotopes (δD) and chemical species in the ice core. The ice core age was determined by annual counts of δD and seasonal cycles of Na + , and we used reference horizons of tritium peaks in 1963 and 1964, major volcanic eruptions of Mount Spurr in 1992 and Mount Katmai in 1912, and a large forest fire in 2004 as age controls. Here, we show that the chronology of the Aurora Peak ice core from 95.61 m to the top corresponds to the period from 1900 to the summer season of 2008, with a dating error of ± 3 years. We estimated that the mean accumulation rate from 1997 to 2007 (except for 2004) was 2.04 m w.eq. yr -1 . Our results suggest that temporal variations in δD and annual accumulation rates are strongly related to shifts in the Pacific Decadal Oscillation index (PDOI). The remarkable increase in annual precipitation since the 1970s has likely been the result of enhanced storm activity associated with shifts in the PDOI during winter in the Gulf of Alaska. |
format |
Article in Journal/Newspaper |
author |
A. Tsushima S. Matoba T. Shiraiwa S. Okamoto H. Sasaki D. J. Solie K. Yoshikawa |
author_facet |
A. Tsushima S. Matoba T. Shiraiwa S. Okamoto H. Sasaki D. J. Solie K. Yoshikawa |
author_sort |
A. Tsushima |
title |
Reconstruction of recent climate change in Alaska from the Aurora Peak ice core, central Alaska |
title_short |
Reconstruction of recent climate change in Alaska from the Aurora Peak ice core, central Alaska |
title_full |
Reconstruction of recent climate change in Alaska from the Aurora Peak ice core, central Alaska |
title_fullStr |
Reconstruction of recent climate change in Alaska from the Aurora Peak ice core, central Alaska |
title_full_unstemmed |
Reconstruction of recent climate change in Alaska from the Aurora Peak ice core, central Alaska |
title_sort |
reconstruction of recent climate change in alaska from the aurora peak ice core, central alaska |
publisher |
Copernicus Publications |
publishDate |
2015 |
url |
https://doi.org/10.5194/cp-11-217-2015 https://doaj.org/article/e0ee8e7b46a04ade9add48770f2c6c0f |
long_lat |
ENVELOPE(144.200,144.200,-67.383,-67.383) |
geographic |
Gulf of Alaska Pacific Aurora Peak |
geographic_facet |
Gulf of Alaska Pacific Aurora Peak |
genre |
alaska range ice core Alaska |
genre_facet |
alaska range ice core Alaska |
op_source |
Climate of the Past, Vol 11, Iss 2, Pp 217-226 (2015) |
op_relation |
http://www.clim-past.net/11/217/2015/cp-11-217-2015.pdf https://doaj.org/toc/1814-9324 https://doaj.org/toc/1814-9332 1814-9324 1814-9332 doi:10.5194/cp-11-217-2015 https://doaj.org/article/e0ee8e7b46a04ade9add48770f2c6c0f |
op_doi |
https://doi.org/10.5194/cp-11-217-2015 |
container_title |
Climate of the Past |
container_volume |
11 |
container_issue |
2 |
container_start_page |
217 |
op_container_end_page |
226 |
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1766199117725302784 |