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Investigating the Role of Ocean Circulation in Climate Change During the Last Ice Age Using 231Pa/230Th | |
项目编号 | 0937221 |
Jerry McManus | |
项目主持机构 | Columbia University |
开始日期 | 2009-04-01 |
结束日期 | 2010-03-31 |
英文摘要 | ABSTRACT 0602384 The last ice age was characterized by dramatic climate oscillations that appear to be linked to changes in the oceans meridional overturning circulation (MOC). Direct evidence for changes in the rate of MOC remains limited because traditional tracers can only provide snapshots of past water mass configurations without information about property transport. In this project, a new dynamical tracer of water circulation, Pa/Th, will be used to produce high-resolution, continuous 60,000-year record of MOC in the Atlantic Ocean during marine isotope stage 3. This research will be conducted on two high-quality cores from the subtropical and subpolar North Atlantic Ocean and will be carried out in parallel with complementary sedimentological and geochemical analyses as well as modeling studies. These data will explore linkages and phasing within the ocean-climate system and provide theoretical constraints on the interpretation of Pa/Th as a circulation proxy. This project will involve students in their research and in teaching at MIT/WHOI, and through NSF-funded and voluntary efforts to provide undergraduates with research experience in their studies. The PIs will continue outreach through presentations at college campuses and discussions in media such as newspapers and radio broadcasts. All data will be archived and made available to the scientific community as well as to the general public through web-based access at WHOI and NGDC. |
学科分类 | 08 - 地球科学;0806 - 海洋科学 |
资助机构 | US-NSF |
项目经费 | 104152 |
项目类型 | Standard Grant |
国家 | US |
语种 | 英语 |
文献类型 | 项目 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/72258 |
推荐引用方式 GB/T 7714 | Jerry McManus.Investigating the Role of Ocean Circulation in Climate Change During the Last Ice Age Using 231Pa/230Th.2009. |
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