Twentieth-century surface temperature trends in the western Ross Sea, Antarctica: Evidence from a high-resolution ice core
A 125-yr ice core record of climate from the Whitehall Glacier ice divide provides exceptionally high-resolution stable isotope data from the northwest margin of the Ross Sea, Antarctica. This is the only proxy data available to extend the instrumental record of temperature in this region, where lit...
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ftunivtasecite:oai:ecite.utas.edu.au:80555 2023-05-15T14:02:30+02:00 Twentieth-century surface temperature trends in the western Ross Sea, Antarctica: Evidence from a high-resolution ice core Sinclair, KE Bertler, NAN van Ommen, TD 2012 application/pdf https://doi.org/10.1175/JCLI-D-11-00496.1 http://ecite.utas.edu.au/80555 en eng Amer Meteorological Soc http://ecite.utas.edu.au/80555/1/Sinclair_etal_2012_JournalClimate.pdf http://dx.doi.org/10.1175/JCLI-D-11-00496.1 Sinclair, KE and Bertler, NAN and van Ommen, TD, Twentieth-century surface temperature trends in the western Ross Sea, Antarctica: Evidence from a high-resolution ice core, Journal of Climate, 25, (10) pp. 3629-3636. ISSN 0894-8755 (2012) [Refereed Article] http://ecite.utas.edu.au/80555 Earth Sciences Physical Geography and Environmental Geoscience Glaciology Refereed Article PeerReviewed 2012 ftunivtasecite https://doi.org/10.1175/JCLI-D-11-00496.1 2019-12-13T21:45:47Z A 125-yr ice core record of climate from the Whitehall Glacier ice divide provides exceptionally high-resolution stable isotope data from the northwest margin of the Ross Sea, Antarctica. This is the only proxy data available to extend the instrumental record of temperature in this region, where little is known about climate variability over the past two centuries. Using ECMWF Interim Re-Analysis (ERA-Interim) data, this study develops a precipitation-weighted δ 18 O-temperature transfer function of 0.62 C −1 , which is comparable to other proximal ice cores, such as Taylor, Talos, and Law Domes. Reconstructed mean annual temperatures show no significant change between 1882 and 2006. However, a decrease in cold season [AprilSeptember (AMJJAS)] temperatures of −1.59 0.84C decade −1 (at 90% confidence) is observed since 1979. This cooling trend is in contrast to a surface temperature record from Ross Island (Scott Base) where significant spring warming is observed. It is also coincident with a positive trend in the southern annular mode, which is linked to stronger southerly winds and increased sea ice extent and duration in the western Ross Sea. Article in Journal/Newspaper Antarc* Antarctica ice core Ross Island Ross Sea Sea ice eCite UTAS (University of Tasmania) Ross Sea Ross Island Scott Base ENVELOPE(166.766,166.766,-77.849,-77.849) Whitehall Glacier ENVELOPE(169.417,169.417,-72.717,-72.717) Journal of Climate 25 10 3629 3636 |
institution |
Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Physical Geography and Environmental Geoscience Glaciology |
spellingShingle |
Earth Sciences Physical Geography and Environmental Geoscience Glaciology Sinclair, KE Bertler, NAN van Ommen, TD Twentieth-century surface temperature trends in the western Ross Sea, Antarctica: Evidence from a high-resolution ice core |
topic_facet |
Earth Sciences Physical Geography and Environmental Geoscience Glaciology |
description |
A 125-yr ice core record of climate from the Whitehall Glacier ice divide provides exceptionally high-resolution stable isotope data from the northwest margin of the Ross Sea, Antarctica. This is the only proxy data available to extend the instrumental record of temperature in this region, where little is known about climate variability over the past two centuries. Using ECMWF Interim Re-Analysis (ERA-Interim) data, this study develops a precipitation-weighted δ 18 O-temperature transfer function of 0.62 C −1 , which is comparable to other proximal ice cores, such as Taylor, Talos, and Law Domes. Reconstructed mean annual temperatures show no significant change between 1882 and 2006. However, a decrease in cold season [AprilSeptember (AMJJAS)] temperatures of −1.59 0.84C decade −1 (at 90% confidence) is observed since 1979. This cooling trend is in contrast to a surface temperature record from Ross Island (Scott Base) where significant spring warming is observed. It is also coincident with a positive trend in the southern annular mode, which is linked to stronger southerly winds and increased sea ice extent and duration in the western Ross Sea. |
format |
Article in Journal/Newspaper |
author |
Sinclair, KE Bertler, NAN van Ommen, TD |
author_facet |
Sinclair, KE Bertler, NAN van Ommen, TD |
author_sort |
Sinclair, KE |
title |
Twentieth-century surface temperature trends in the western Ross Sea, Antarctica: Evidence from a high-resolution ice core |
title_short |
Twentieth-century surface temperature trends in the western Ross Sea, Antarctica: Evidence from a high-resolution ice core |
title_full |
Twentieth-century surface temperature trends in the western Ross Sea, Antarctica: Evidence from a high-resolution ice core |
title_fullStr |
Twentieth-century surface temperature trends in the western Ross Sea, Antarctica: Evidence from a high-resolution ice core |
title_full_unstemmed |
Twentieth-century surface temperature trends in the western Ross Sea, Antarctica: Evidence from a high-resolution ice core |
title_sort |
twentieth-century surface temperature trends in the western ross sea, antarctica: evidence from a high-resolution ice core |
publisher |
Amer Meteorological Soc |
publishDate |
2012 |
url |
https://doi.org/10.1175/JCLI-D-11-00496.1 http://ecite.utas.edu.au/80555 |
long_lat |
ENVELOPE(166.766,166.766,-77.849,-77.849) ENVELOPE(169.417,169.417,-72.717,-72.717) |
geographic |
Ross Sea Ross Island Scott Base Whitehall Glacier |
geographic_facet |
Ross Sea Ross Island Scott Base Whitehall Glacier |
genre |
Antarc* Antarctica ice core Ross Island Ross Sea Sea ice |
genre_facet |
Antarc* Antarctica ice core Ross Island Ross Sea Sea ice |
op_relation |
http://ecite.utas.edu.au/80555/1/Sinclair_etal_2012_JournalClimate.pdf http://dx.doi.org/10.1175/JCLI-D-11-00496.1 Sinclair, KE and Bertler, NAN and van Ommen, TD, Twentieth-century surface temperature trends in the western Ross Sea, Antarctica: Evidence from a high-resolution ice core, Journal of Climate, 25, (10) pp. 3629-3636. ISSN 0894-8755 (2012) [Refereed Article] http://ecite.utas.edu.au/80555 |
op_doi |
https://doi.org/10.1175/JCLI-D-11-00496.1 |
container_title |
Journal of Climate |
container_volume |
25 |
container_issue |
10 |
container_start_page |
3629 |
op_container_end_page |
3636 |
_version_ |
1766272809064988672 |