Characterizing the Formation, Nature, and Export of Weddell Sea Bottom Water using Noble Gases and Transient Tracers

学术价值：人们普遍认为，至少自末次盛冰期以来，全球气候的重大千年时间尺度变化是由海洋经向翻转环流（MOC）的突然变化引起的，或至少与之相关。有一种挥之不去的怀疑，也许气候瞬变的最终触发因素可能在南半球。在南极大陆架地区，由于浮力变化而形成的稠密沃茨离开大陆架下沉，构成了被称为南极底层水（AABW）的主要水团复合体。AABW是在MOC中发挥作用的最冷和最密集的水，反过来又进入所有主要的海洋盆地，从而关闭了MOC环路的南端。威德尔海在AABW的形成中具有突出的特征，海水和浮冰架之间的相互作用通过多种过程的组合产生了AABW的独特前体，包括：冰缘冰穴的强烈热提取，海冰的形成和输出，冰川冰在接地线处的融化，以及海底海冰的形成和沉积。这些过程不仅在海洋学和气候学上产生显著的淡水注入AABW前体，而且被假设对其溶解的惰性气体成分有重大影响。我们建议使用高精度的测量后者作为诊断工具的大小，这些过程。调查员将参加英国的研究巡航ANDREX，这是一个部分连接的CLIVAR（气候变化和可预测性计划）重复线I6 S与南极半岛在2009年初。巡航沿着威德尔海环流的北方边缘，是研究南极绕极流中水团交换的理想地点。惰性气体，瞬态示踪剂（氚和放射性碳）沿着与氯氟烃，稳定同位素，3He和传统的水文测量的组合将被用来放置在海洋和气候上的重要region.Broader影响的约束：该项目涉及开发和使用新的海洋示踪剂和应用更传统的示踪剂在新的方式来表征水团的转换过程，是在全球气候系统的运作具有根本的重要性。对这些过程的新见解将为下一代海洋-大气耦合气候模型的设计和构建提供有价值的指导，这对于应对气候变化带来的广泛经济、政策和社会问题具有战略意义。这项工作产生的数据集将提交给适当的数据中心/储存库，供建模人员和气候科学家使用，以指导未来的研究工作，并评估或测试现有和未来的气候模型。

Intellectual Merit:It is commonly accepted that since at least the last glacial maximum, the substantial millennial-timescale changes in global climate have been caused by, or at least associated with abrupt changes in the oceanic Meridional Overturning Circulation (MOC). There is the lingering suspicion that perhaps the ultimate trigger of the climate transients may lie in the southern hemisphere. Dense waters formed by buoyancy modification on Antarctic shelf regions leave the shelves and sink to comprise the major water mass complex known as Antarctic Bottom Water (AABW). AABW, the coldest and densest water to play a role in the MOC, in turn enters all of the major ocean basins and thereby closes the southern end of the MOC loop. The Weddell Sea features prominently in the production of AABW, where interaction between seawater and the floating ice-shelves produces a unique pre-cursor to AABW by a combination of processes, including) strong heat extraction at ice-edge polynyas, sea-ice formation and export, melting of glacial ice at the grounding line, and formation and deposition of sub-marine sea-ice. These processes not only produce oceanographically and climatically significant injections of fresh water into the AABW pre-cursor, but are hypothesized to have significant impact on its dissolved noble gas composition. We propose to use high precision measurements of the latter as a diagnostic tool of the magnitude of these processes.The investigator will participate in a British research cruise ANDREX which is a section connecting the CLIVAR (CLImate VARiability and predictability Program) repeat line I6S with the Antarctic Peninsula in early 2009. The cruise follows the northern rim of the Weddell Sea gyre, and is ideally situated to study the exchange of water masses across the Antarctic Circumpolar Current. A combination of noble gases, transient tracers (tritium and radiocarbon) along with CFCs, stable isotopes, 3He, and traditional hydrographic measurements will be used to place constraints on an oceanographically and climatically important region.Broader Impacts:This project involves the development and use of novel oceanographic tracers and the application of more traditional tracers in new ways to characterize water mass transformation processes that are of fundamental importance in the operation of the global climate system. The new insights into these processes will provide valuable guidance in the design and construction of the next generation of coupled ocean-atmosphere climate models, which will be of strategic importance in facing the broad range of economic, policy, and societal issues created by climate change. The data set produced in this work will be submitted to the appropriate data centers/repositories to be made available to modelers and climate scientists to guide future research efforts and to evaluate or test existing and future climate models.