globalchange  > 影响、适应和脆弱性
项目编号: 1341311
项目名称:
Collaborative Research: Bipolar Coupling of late Quaternary Ice Sheet Variability
作者: Axel Timmermann
承担单位: University of Hawaii
批准年: 2013
开始日期: 2014-03-01
结束日期: 2018-02-28
资助金额: USD380684
资助来源: US-NSF
项目类别: Standard Grant
国家: US
语种: 英语
特色学科分类: Geosciences - Polar
英文关键词: ice-sheet ; earth-system ; research team ; wais ; west antarctic ice sheet ; project ; joint variability ; individual ice-sheet ; ice-sheet sensitivity ; ice-core datum ; northern hemisphere ice sheet ; glacial-scale variability ; east antarctic ice sheet ; asia pacific data research center ; antarctic ice sheet ; postdoctoral researcher ; southern hemisphere ice-sheet variation ; past antarctic ice-volume change ; long-term ice volume variability ; ice-sheet climate system ; numerical ice-sheet earth-system model ; ice core ; antarctic ice-sheet ; ice-sheet modeling
英文摘要: Timmerman/1341311

This award supports a project to study the physical processes that synchronize glacial-scale variability between the Northern Hemisphere ice sheets and the Antarctic ice-sheet. Using a coupled numerical ice-sheet earth-system model, the research team will explore the cryospheric responses to past changes in greenhouse gas concentrations and variations in earth's orbit and tilt. First capturing the sensitivity of each individual ice-sheet to these forcings and then determining their joint variability induced by changes in sea level, ocean temperatures and atmospheric circulation, the researchers will quantify the relative roles of local versus remote effects on long-term ice volume variability. The numerical experiments will provide deeper physical insights into the underlying dynamics of past Antarctic ice-volume changes and their contribution to global sea level. Output from the transient earth system model simulations will be directly compared with ice-core data from previous and ongoing drilling efforts, such as West Antarctic Ice Sheet (WAIS) Divide. Specific questions that will be addressed include: 1) Did the high-latitude Southern Hemispheric atmospheric and oceanic climate, relevant to Antarctic ice sheet forcing, respond to local insolation variations, CO2, Northern Hemispheric changes, or a combination thereof?; 2) How did WAIS and East Antarctic Ice Sheet (EAIS) vary through the Last Glacial Termination and into the Holocene (21 ka- present)?; 3) Did the WAIS (or EAIS) contribute to rapid sea-level fluctuations during this period, such as Meltwater Pulse 1A? 4) Did WAIS collapse fully at Stage 5e (~ 125 ka), and what was its timing relative to the maximum Greenland retreat?; and 5) How did the synchronized behavior of Northern Hemisphere and Southern Hemisphere ice-sheet variations affect the strength of North Atlantic Deep Water and Antarctic Bottom Water formation and the respective overturning cells? The transient earth-system model simulations conducted as part of this project will be closely compared with paleo-climate reconstructions from ice cores, sediment cores and terrestrial data. This will generate an integrated understanding of the hemispheric contributions of deglacial climate change, the origin of meltwater pulses, and potential thresholds in the coupled ice-sheet climate system in response to different types of forcings. A well-informed long-term societal response to sea level rise requires a detailed understanding of ice-sheet sensitivities to external forcing. The proposed research will strongly contribute to this task through numerical modeling and paleo-data analysis. The research team will make the resulting model simulations available on the web-based data server at the Asia Pacific Data Research Center (APDRC) to enable further analysis by the scientific community. As part of this project a female graduate student and a postdoctoral researcher will receive training in earth-system and ice-sheet modeling and paleo-climate dynamics. This award has no field work in Antarctica.
资源类型: 项目
标识符: http://119.78.100.158/handle/2HF3EXSE/97266
Appears in Collections:影响、适应和脆弱性
气候减缓与适应

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Recommended Citation:
Axel Timmermann. Collaborative Research: Bipolar Coupling of late Quaternary Ice Sheet Variability. 2013-01-01.
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