积雪
冰期
地质学
冰川
气候变化
气候学
末次冰期最大值
钻孔
自然地理学
仰角(弹道)
海洋学
地貌学
古生物学
地理
几何学
数学
作者
Christo Buizert,T. J. Fudge,William H. G. Roberts,Eric J. Steig,Sam Sherriff‐Tadano,Catherine Ritz,E. Lefèbvre,Jon S. Edwards,Kenji Kawamura,Ikumi Oyabu,Hideaki Motoyama,Emma C. Kahle,Tyler R. Jones,Ayako Abe‐Ouchi,Takashi Obase,Carlos Martín,Hugh F. J. Corr,Jeffrey P. Severinghaus,Ross Beaudette,Jenna Epifanio
出处
期刊:Science
[American Association for the Advancement of Science]
日期:2021-06-03
卷期号:372 (6546): 1097-1101
被引量:217
标识
DOI:10.1126/science.abd2897
摘要
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. Buizert et 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
科研通智能强力驱动
Strongly Powered by AbleSci AI