Collaborative Research: Mode Water Formation in the Lofoten Basin: A Key Element in the Meridional Overturning Circulation

合作研究：罗弗敦盆地的水形成模式：经向翻转环流的关键要素

• 批准号: 0850609
• 负责人: H. Thomas Rossby
• 金额: $ 37.46万
• 依托单位: University of Rhode Island
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2009
• 资助国家: 美国
• 起止时间: 2009-06-15 至 2013-05-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0850609&HistoricalAwards=false
• 关键词: Collaborative; Research; Mode; Water; Formation

This award is funded under the American Recovery and Reinvestment Act of 2009 (Public Law 111-5).The traditionally central role played by the deep convective regions of the North Atlantic - the Labrador Sea and the Greenland Sea - in driving the Atlantic Meridional Overturning Circulation (AMOC) and its associated poleward heat transport has been severely questioned over the last decade. In particular, it is now known that relatively little sinking and only a limited surface buoyancy loss occurs in these regions and, furthermore, that the dense water masses feeding the AMOC are not a direct product of these regions. In the case of the Nordic Seas, the Greenland-Scotland overflow waters comprising the deepest branch of the AMOC contain only small amounts of Greenland Sea Water, and are instead largely the product of the progressive transformation of the circulating warm, salty Atlantic Waters. Yet the pathways and processes through which this transformation occurs are largely unknown. Emerging as playing a central role in this transformation is the Lofoten Basin, which sits adjacent to the Greenland Sea between the two main branches of the Atlantic inflow. The warm, salty Atlantic waters are strongly modified as they transit through this basin, which alone accounts for a substantial fraction of the surface buoyancy loss over the Nordic Seas. This leads to the formation of an intermediate convected product, the Lofoten Basin Mode Water. Unlike Labrador Sea Water and Greenland Sea Water, the Lofoten Basin Mode Water can be rapidly exported from the basin, and is a direct source for the overflows waters. Despite its importance, however, the basic dynamical features of this basin and of its intermediate water mass formation have yet to be addressed. Intellectual MeritThe principal intellectual merit of this project is its importance for elucidating a key facet of the AMOC, namely, mode water formation in the Lofoten Basin and its role in the Nordic Seas transformation pathway. The project is timely since there is growing evidence that the Greenland Sea's deep convection by itself has a limited impact on the AMOC and, at the same time, our understanding of intermediate/dense transformation pathways has greatly improved. By using the Labrador Sea as a reference point, the investigators anticipate contributing to a more universal understanding of convective transformation in the presence of varied topography and an unstable boundary current. The combined observational and modeling study will investigate mode water formation in the Lofoten Basin and its eventual export. A profiling mooring together with RAFOS floats deployed directly within the basin will clarify the annual cycle of transformation, restratification, and dispersal. Analysis of existing hydrographic, float, and remote sensing data will help to guide the field work, and will enable the investigation of larger-scale and longer-term variability. A variety of models will be employed to study the dynamics of the transformation process in the Lofoten Basin and elsewhere in the Nordic Seas. The net result will be a new understanding of the interaction between air-sea fluxes and ocean dynamics along this crucial branch of the AMOC. Broader ImpactsThis project seeks to increase our understanding of a key process in the Earth's climate system, the Nordic Seas transformation pathway, which affects not only the AMOC but, also, the warm inflow into the Arctic Ocean, a region currently undergoing rapid change. The project has been carefully planned in collaboration with several Norwegian and other European groups so as to optimize resources and foster international collaboration. It includes two workshops, as well as exchange of data, ideas, and personnel throughout the project. Finally, it brings together a group of diverse PIs, who will bring complementary skills to this problem, and includes training of a post-doc who will greatly benefit from the diverse and international scientific environment of this project.

该奖项根据 2009 年美国复苏和再投资法案（公法 111-5）提供资金。北大西洋深对流区域（拉布拉多海和格陵兰海）传统上在驱动大西洋经向翻转环流 (AMOC) 及其相关的极地热传输方面发挥的核心作用在过去十年中受到了严重质疑。特别是，现在已知这些区域发生的下沉相对较小，并且仅发生有限的表面浮力损失，此外，供给 AMOC 的密集水团并不是这些区域的直接产物。就北欧海而言，构成AMOC最深分支的格陵兰-苏格兰溢流水域仅含有少量格陵兰海水，而主要是循环的温暖、咸咸的大西洋水域逐渐转变的产物。然而，这种转变发生的途径和过程在很大程度上是未知的。在这一转变中发挥核心作用的是罗弗敦盆地，它毗邻格陵兰海，位于大西洋流入的两个主要分支之间。温暖、咸的大西洋水域在经过这个盆地时发生了强烈的变化，仅这个盆地就占了北欧海域表面浮力损失的很大一部分。这导致中间对流产物的形成，即罗弗敦盆地模式水。与拉布拉多海水和格陵兰海水不同，罗弗敦盆地模式水可以快速从盆地输出，是溢流水的直接来源。然而，尽管它很重要，但该盆地及其中间水团形成的基本动力学特征尚未得到解决。智力优点 该项目的主要智力优点是它对于阐明 AMOC 的一个关键方面的重要性，即罗弗敦盆地的模式水形成及其在北欧海洋转变路径中的作用。该项目是及时的，因为越来越多的证据表明格陵兰海的深层对流本身对 AMOC 的影响有限，同时，我们对中/密集转化路径的理解也大大提高了。通过使用拉布拉多海作为参考点，研究人员预计将有助于对存在不同地形和不稳定边界流的情况下对流转换的更普遍的理解。观测和建模相结合的研究将调查罗弗敦盆地的水形成模式及其最终的出口。剖面系泊装置与直接部署在盆地内的 RAFOS 浮标一起将阐明每年的转变、重新分层和扩散周期。对现有水文、浮标和遥感数据的分析将有助于指导实地工作，并使调查更大规模和更长期的变化成为可能。将采用各种模型来研究罗弗敦盆地和北欧海域其他地方的转变过程的动态。最终结果将是对AMOC这一重要分支的海气通量和海洋动力学之间的相互作用有了新的认识。更广泛的影响该项目旨在加深我们对地球气候系统中一个关键过程的了解，即北欧海洋转变路径，该路径不仅影响AMOC，而且还影响流入北冰洋的暖流，而北冰洋目前正在经历快速变化。该项目是与多个挪威和其他欧洲团体合作精心策划的，以优化资源并促进国际合作。它包括两个研讨会，以及整个项目中的数据、想法和人员的交流。最后，它汇集了一群不同的 PI，他们将为解决这个问题带来互补的技能，并包括培训一名博士后，他将从该项目的多元化和国际科学环境中受益匪浅。