Different trends in Antarctic temperature and atmospheric CO 2 during the last glacial
We analyze the past 67,000years of climate using Antarctic ice-core records to constrain the mechanisms involved in (a) the bipolar seesaw relationship between Greenland and Antarctic surface temperature variations, and (b) mechanisms of millennial-scale atmospheric CO 2 concentration variations. Sp...
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Online Access: | https://doi.org/10.1029/2021GL093868 http://ecite.utas.edu.au/151696 |
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ftunivtasecite:oai:ecite.utas.edu.au:151696 2023-05-15T13:42:40+02:00 Different trends in Antarctic temperature and atmospheric CO 2 during the last glacial Zheng, P Pedro, JB Jochum, M Rasmussen, SO Lai, Z 2021 https://doi.org/10.1029/2021GL093868 http://ecite.utas.edu.au/151696 en eng Amer Geophysical Union http://dx.doi.org/10.1029/2021GL093868 Zheng, P and Pedro, JB and Jochum, M and Rasmussen, SO and Lai, Z, Different trends in Antarctic temperature and atmospheric CO 2 during the last glacial, Geophysical Research Letters, 48, (14) Article e2021GL093868. ISSN 0094-8276 (2021) [Refereed Article] http://ecite.utas.edu.au/151696 Earth Sciences Physical geography and environmental geoscience Palaeoclimatology Refereed Article PeerReviewed 2021 ftunivtasecite https://doi.org/10.1029/2021GL093868 2022-10-31T23:17:10Z We analyze the past 67,000years of climate using Antarctic ice-core records to constrain the mechanisms involved in (a) the bipolar seesaw relationship between Greenland and Antarctic surface temperature variations, and (b) mechanisms of millennial-scale atmospheric CO 2 concentration variations. Specifically, we determine for each Greenland Stadial the rate of Antarctic temperature and atmospheric CO 2 rise. We find that Antarctic warming rates significantly decrease as the climate cools during the glacial period, whereas the rate of atmospheric CO 2 rise does not significantly change. Also, we find that the rates of Antarctic warming and atmospheric CO 2 rise are both insensitive to whether a given stadial contains a Heinrich event. These results challenge the view that a single Southern-Ocean-based mechanism dominates the observed glacial variability in Antarctic temperature and atmospheric CO 2 . Instead, our results are consistent with an important contribution of low- and mid-latitude processes to millennial-scale atmospheric CO 2 changes. Article in Journal/Newspaper Antarc* Antarctic Greenland ice core Southern Ocean eCite UTAS (University of Tasmania) Antarctic Greenland Southern Ocean Geophysical Research Letters 48 14 |
institution |
Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Physical geography and environmental geoscience Palaeoclimatology |
spellingShingle |
Earth Sciences Physical geography and environmental geoscience Palaeoclimatology Zheng, P Pedro, JB Jochum, M Rasmussen, SO Lai, Z Different trends in Antarctic temperature and atmospheric CO 2 during the last glacial |
topic_facet |
Earth Sciences Physical geography and environmental geoscience Palaeoclimatology |
description |
We analyze the past 67,000years of climate using Antarctic ice-core records to constrain the mechanisms involved in (a) the bipolar seesaw relationship between Greenland and Antarctic surface temperature variations, and (b) mechanisms of millennial-scale atmospheric CO 2 concentration variations. Specifically, we determine for each Greenland Stadial the rate of Antarctic temperature and atmospheric CO 2 rise. We find that Antarctic warming rates significantly decrease as the climate cools during the glacial period, whereas the rate of atmospheric CO 2 rise does not significantly change. Also, we find that the rates of Antarctic warming and atmospheric CO 2 rise are both insensitive to whether a given stadial contains a Heinrich event. These results challenge the view that a single Southern-Ocean-based mechanism dominates the observed glacial variability in Antarctic temperature and atmospheric CO 2 . Instead, our results are consistent with an important contribution of low- and mid-latitude processes to millennial-scale atmospheric CO 2 changes. |
format |
Article in Journal/Newspaper |
author |
Zheng, P Pedro, JB Jochum, M Rasmussen, SO Lai, Z |
author_facet |
Zheng, P Pedro, JB Jochum, M Rasmussen, SO Lai, Z |
author_sort |
Zheng, P |
title |
Different trends in Antarctic temperature and atmospheric CO 2 during the last glacial |
title_short |
Different trends in Antarctic temperature and atmospheric CO 2 during the last glacial |
title_full |
Different trends in Antarctic temperature and atmospheric CO 2 during the last glacial |
title_fullStr |
Different trends in Antarctic temperature and atmospheric CO 2 during the last glacial |
title_full_unstemmed |
Different trends in Antarctic temperature and atmospheric CO 2 during the last glacial |
title_sort |
different trends in antarctic temperature and atmospheric co 2 during the last glacial |
publisher |
Amer Geophysical Union |
publishDate |
2021 |
url |
https://doi.org/10.1029/2021GL093868 http://ecite.utas.edu.au/151696 |
geographic |
Antarctic Greenland Southern Ocean |
geographic_facet |
Antarctic Greenland Southern Ocean |
genre |
Antarc* Antarctic Greenland ice core Southern Ocean |
genre_facet |
Antarc* Antarctic Greenland ice core Southern Ocean |
op_relation |
http://dx.doi.org/10.1029/2021GL093868 Zheng, P and Pedro, JB and Jochum, M and Rasmussen, SO and Lai, Z, Different trends in Antarctic temperature and atmospheric CO 2 during the last glacial, Geophysical Research Letters, 48, (14) Article e2021GL093868. ISSN 0094-8276 (2021) [Refereed Article] http://ecite.utas.edu.au/151696 |
op_doi |
https://doi.org/10.1029/2021GL093868 |
container_title |
Geophysical Research Letters |
container_volume |
48 |
container_issue |
14 |
_version_ |
1766171457940881408 |