Collaborative Research: The Timing and Spatial Expression of the Bipolar Seesaw in Antarctica from Synchronized Ice Cores

合作研究：从同步冰芯观察南极洲双极跷跷板的时间和空间表达

• 批准号: 1643394
• 负责人: Christo Buizert
• 金额: $ 22.99万
• 依托单位: Oregon State University
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2017
• 资助国家: 美国
• 起止时间: 2017-02-01 至 2022-01-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1643394&HistoricalAwards=false
• 关键词: Collaborative; Research; Timing; Spatial; Expression

Buizert/1643394This award supports a project to use ice cores to study teleconnections between the northern hemisphere, tropics, and Antarctica during very abrupt climate events that occurred during the last ice age (from 70,000 to 11,000 years ago). The observations can be used to test scientific theories about the role of the westerly winds on atmospheric carbon dioxide. In a warming world, snow fall in Antarctica is expected to increase, which can reduce the Antarctic contribution to sea level rise, all else being equal. The study will investigate how snow fall changed in the past in response to changes in temperature and atmospheric circulation, which can help improve projections of future sea level rise. Antarctica is important for the future evolution of our planet in several ways; it has the largest inventory of land-based ice, equivalent to about 58 m of global sea level and currently contributes about 0.3 mm per year to global sea level rise, which is expected to increase in the future due to global warming. The oceans surrounding Antarctica help regulate the uptake of human-produced carbon dioxide. Shifts in the position and strength of the southern hemisphere westerly winds could change the amount of carbon dioxide that is absorbed by the ocean, which will influence the rate of global warming. The climate and winds near and over Antarctica are linked to the rest of our planet via so-called climatic teleconnections. This means that climate changes in remote places can influence the climate of Antarctica. Understanding how these climatic teleconnections work in both the ocean and atmosphere is an important goal of climate research. The funds will further contribute towards training of a postdoctoral researcher and an early-career researcher; outreach to public schools; and the communication of research findings to the general public via the media, local events, and a series of Wikipedia articles. The project will help to fully characterize the timing and spatial pattern of millennial-scale Antarctic climate change during the deglaciation and Dansgaard-Oeschger (DO) cycles using multiple synchronized Antarctic ice cores. The phasing of Antarctic climate change relative to Greenland DO events can distinguish between fast atmospheric teleconnections on sub-decadal timescales, and slow oceanic ones on centennial time scales. Preliminary work suggests that the spatial pattern of Antarctic change can fingerprint specific changes to the atmospheric circulation; in particular, the proposed work will clarify past movements of the Southern Hemisphere westerly winds during the DO cycle, which have been hypothesized. The project will help resolve a discrepancy between two previous seminal studies on the precise timing of interhemispheric coupling between ice cores in both hemispheres. The study will further provide state-of-the-art, internally-consistent ice core chronologies for all US Antarctic ice cores, as well as stratigraphic ties that can be used to integrate them into a next-generation Antarctic-wide ice core chronological framework. Combined with ice-flow modeling, these chronologies will be used for a continent-wide study of the relationship between ice sheet accumulation and temperature during the last deglaciation.

Buizert/1643394该奖项支持一个项目，利用冰芯来研究上一个冰河时期（70,000 至 11,000 年前）发生的非常突然的气候事件期间北半球、热带地区和南极洲之间的遥相关。这些观测结果可用于检验有关西风对大气二氧化碳作用的科学理论。在全球变暖的情况下，在其他条件相同的情况下，南极洲的降雪量预计会增加，这可以减少南极洲对海平面上升的贡献。该研究将调查过去降雪量如何随着温度和大气环流的变化而变化，这有助于改善对未来海平面上升的预测。 南极洲在几个方面对我们星球的未来演化非常重要；它拥有最大的陆基冰存量，相当于全球海平面约58 m，目前每年导致全球海平面上升约0.3毫米，由于全球变暖，预计未来还会增加。南极洲周围的海洋有助于调节人类产生的二氧化碳的吸收。南半球西风的位置和强度的变化可能会改变海洋吸收的二氧化碳量，从而影响全球变暖的速度。南极洲附近和上空的气候和风通过所谓的气候遥相关与地球其他地区联系起来。这意味着偏远地区的气候变化可以影响南极洲的气候。了解这些气候遥相关如何在海洋和大气中发挥作用是气候研究的一个重要目标。 这些资金将进一步用于培训一名博士后研究员和一名早期职业研究员；向公立学校推广；通过媒体、当地活动和一系列维基百科文章向公众传播研究成果。该项目将有助于利用多个同步的南极冰芯，全面描述冰消期和丹斯加德-厄施格（DO）循环期间千年规模的南极气候变化的时间和空间模式。相对于格陵兰溶解氧事件的南极气候变化的阶段可以区分亚十年时间尺度上的快速大气遥相关和百年时间尺度上的缓慢海洋遥相关。初步研究表明，南极变化的空间模式可以反映大气环流的具体变化；特别是，拟议的工作将澄清过去假设的溶解氧周期期间南半球西风的运动。该项目将有助于解决之前两项关于两个半球冰芯之间半球间耦合精确时间的开创性研究之间的差异。该研究将进一步提供所有美国南极冰芯最先进的、内部一致的冰芯年代学，以及可用于将它们整合到下一代全南极冰芯年代学框架中的地层关系。与冰流模型相结合，这些年表将用于在整个大陆范围内研究末次冰消期期间冰盖积累与温度之间的关系。

项目成果

A 2700-year annual timescale and accumulation history for an ice core from Roosevelt Island, West Antarctica

• DOI: 10.5194/cp-15-751-2019
• 发表时间: 2017-08
• 期刊: Climate of the Past
• 影响因子: 4.3
• 作者: Paul Kjaer;Helle A. Fudge;Tyler J. Lee;James E. Riis;M. Winstrup;P. Vallelonga;H. Kjær;T. Fudge;James E. Lee;Marie H. Riis;R. Edwards;N. Bertler;T. Blunier;E. Brook;C. Buizert;G. Ciobanu;H. Conway;D. Dahl-Jensen;Aja Ellis;B. D. Emanuelsson;R. Hindmarsh;E. Keller;A. Kurbatov;P. Mayewski;P. Neff;Rebecca L. Pyne;M. Simonsen;A. Svensson;Andrea Tuohy;E. Waddington;Sarah D. Wheatley

The Dome Fuji ice core DF2021 chronology (0–207 kyr BP)

• DOI: 10.1016/j.quascirev.2022.107754
• 发表时间: 2022-10
• 期刊: Quaternary Science Reviews
• 影响因子: 4
• 作者: Ikumi Oyabu;K. Kawamura;C. Buizert;F. Parrenin;A. Orsi;Kyotaro Kitamura;S. Aoki;T. Nakazawa

Beyond the bipolar seesaw: Toward a process understanding of interhemispheric coupling

• DOI: 10.1016/j.quascirev.2018.05.005
• 发表时间: 2018-07
• 期刊: Quaternary Science Reviews
• 影响因子: 4
• 作者: J. Pedro;M. Jochum;C. Buizert;F. He;S. Barker;S. Rasmussen

An 83 000-year-old ice core from Roosevelt Island, Ross Sea, Antarctica

来自南极洲罗斯海罗斯福岛的一个 83 万年前的冰芯

• DOI: 10.5194/cp-16-1691-2020
• 发表时间: 2020
• 期刊: Climate of the Past
• 影响因子: 4.3
• 作者: Lee, James E.;Brook, Edward J.;Bertler, Nancy A.;Buizert, Christo;Baisden, Troy;Blunier, Thomas;Ciobanu, V. Gabriela;Conway, Howard;Dahl-Jensen, Dorthe;Fudge, Tyler J.
• 通讯作者: Fudge, Tyler J.

Antarctic temperature and CO 2 : near-synchrony yet variable phasing during the last deglaciation

南极温度和CO 2 ：末次冰消期期间接近同步但变化的相位

• DOI: 10.5194/cp-15-913-2019
• 发表时间: 2019
• 期刊: Climate of the Past
• 影响因子: 4.3
• 作者: Chowdhry Beeman, Jai;Gest, Léa;Parrenin, Frédéric;Raynaud, Dominique;Fudge, Tyler J.;Buizert, Christo;Brook, Edward J.
• 通讯作者: Brook, Edward J.