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Antarctic surface temperature and elevation during the Last Glacial Maximum
Author(s) -
Christo Buizert,
T. J. Fudge,
William H. G. Roberts,
Eric J. Steig,
Sam SherriffTadano,
Catherine Ritz,
E. Lefèbvre,
Jon S. Edwards,
Kenji Kawamura,
Ikumi Oyabu,
Hideaki Motoyama,
Emma C. Kahle,
Tyler R. Jones,
Ayako AbeOuchi,
Takashi Obase,
Carlos Martín,
Hugh F. J. Corr,
Jeffrey P. Severinghaus,
Ross Beaudette,
Jenna Epifanio,
Edward J. Brook,
Kaden Martin,
J. Chappellaz,
Shuji Aoki,
Takakiyo Nakazawa,
Todd Sowers,
Richard B. Alley,
Jinho Ahn,
Michael Sigl,
Mirko Severi,
Nelia Dunbar,
Anders Svensson,
John M. Fegyveresi,
Chengfei He,
Zhengyu Liu,
Jiang Zhu,
Bette L. OttoBliesner,
V. Lipenkov,
Masa Kageyama,
Jakob Schwander
Publication year - 2021
Publication title -
science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 12.556
H-Index - 1186
eISSN - 1095-9203
pISSN - 0036-8075
DOI - 10.1126/science.abd2897
Subject(s) - firn , glacial period , geology , elevation (ballistics) , climate change , glacier , climatology , last glacial maximum , borehole , physical geography , oceanography , geomorphology , paleontology , geography , geometry , mathematics
Antarctic paleotemperatures It has been widely thought that East Antarctica was ∼9°C cooler during the Last Glacial Maximum, close to the ∼10°C difference between then and now determined independently for West Antarctica. Buizertet al. used borehole thermometry, firn density reconstructions, and climate modeling to show that the temperature in East Antarctica was actually only ∼4° to 7°C cooler during the Last Glacial Maximum. This result has important consequences for our understanding of Antarctic climate, polar amplification, and global climate change.Science , abd2897, this issue p.1097

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