Line W: A Sustained Measurement Program Sampling the North Atlantic Deep Western Boundary Current and Gulf Stream at 39oN

W 线：对北大西洋深西边界流和北纬 39 度墨西哥湾流进行采样的持续测量计划

• 批准号: 0726720
• 负责人: John Toole
• 金额: $ 555万
• 依托单位: Woods Hole Oceanographic Institution
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2008
• 资助国家: 美国
• 起止时间: 2008-03-01 至 2015-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0726720&HistoricalAwards=false
• 关键词: Line; Sustained; Measurement; Program; Sampling

The meridional overturning circulation of the North Atlantic Ocean at mid-latitude principally involves poleward transport of warm water by the Gulf Stream and equatorward flow of colder intermediate and deep waters within a western-intensified boundary current. Comprehension of how these limbs of the global current system and their associated regional recirculations vary on decadal time scale is incomplete. In particular, very little is known on how inter-annual variations in air-sea exchange and water mass modification at high latitudes are transmitted equatorward, and what impacts or feedbacks such signals may have for the Atlantic-wide circulation. Limiting advance in understanding is the lack of long, well-resolved records to document inter-annual signals in water properties, stratification and transport of the Atlantic?s Deep Western Boundary Current (DWBC) system. Importantly, anomalies created at sub-polar latitudes may be profoundly altered or even blocked by the North Atlantic Current or Gulf Stream. Conversely, sub-polar anomalies may influence the position, strength, and/or stability of the Stream, and in turn affect patterns of air-sea exchange throughout the North Atlantic. These basic questions motivate the Line W program that is presently returning observations of the DWBC and Gulf Stream about 39 N between the Grand Banks and Cape Hatteras. Companion field programs are sampling the DWBC both north and south of our study region, and several complementary modeling programs are underway. Taken together, these studies will facilitate a comprehensive investigation of the mechanisms and rates of North Atlantic Deep Water export to lower latitudes and its relationships to the upper ocean circulation.Intellectual Merit: The proposed study will build understanding of the mechanisms and rates of North Atlantic Deep Water export to lower latitudes and the relationships of varying deep-water flow and stratification changes to the upper ocean circulation including the Gulf Stream. This knowledge will help clarify the response of the ocean to variations in air-sea exchange and ultimately, the ocean's role in global climate change. This project will extend the on-going observations of temperature, salinity, tracer and velocity variations of the DWBC and Gulf Stream through 2013, yielding a full 10-year record synchronous with the planned U.K.-U.S. observational program at 26 N. The Line W program consists of a moored array over the continental slope south of Woods Hole, and repeated occupations of a hydrographic section along the array and extending south into the Sargasso Sea. The high spatial resolution sampling possible from ship is verifying that the array is spatially resolving the inter-annual signals as well as returning water samples for tracer analysis. Equally important, the investigators will explore whether a subset of current Line W program is sufficient to index water property and transport variations in this area, setting the stage for a long-term ocean observing system. Broader Impacts: The observations proposed will explore and test theoretical ideas about the interaction of the Deep Western Boundary Current and Gulf Stream; this is the focus of a Ph.D. thesis under current Line W funding. MIT/WHOI Joint Program students enrolled in the introductory physical oceanography course will participate on the proposed cruises, introducing them to observational oceanography Moreover, the program will continue to support one Ph. D. student from an under-represented group whose dissertation research will focus on the acquired data. All observations and resulting data products will be made available to the community at the earliest possible time via the internet with the intention of fostering widespread use of these data so that any member of the community can utilize them in their own research program. As data are recovered and processed, the Line W observations are being made available for model validation and study of regional processes by any interested investigators. In addition to raw observations, value-added products such as time series of core properties and transport by water mass are being produced and distributed. Other researchers are also encouraged to build on the Line W infrastructure to augment the physical fields being sampled.This project is a contribution to the U.S. CLIVAR (CLImate VARiability and predictability) Program.

北大西洋中纬度经向翻转环流主要涉及湾流向极地输送暖水，以及在西向加强的边界流内向赤道方向输送较冷的中层和深水。对于全球电流系统的这些分支及其相关的区域再循环如何在十年时间尺度上变化的理解是不完整的。特别是，关于高纬度海-气交换和水团变化的年际变化如何向赤道传播，以及这种信号可能对整个大西洋环流产生什么影响或反馈，人们知之甚少。限制了解进展的是缺乏长的、分辨率良好的记录来记录关于大西洋-S深西部边界流系统的水性质、层结和输送的年际信号。重要的是，在亚极地纬度产生的异常可能会被北大西洋洋流或墨西哥湾流深刻地改变甚至阻止。相反，亚极地异常可能会影响气流的位置、强度和/或稳定性，进而影响整个北大西洋的海气交换模式。这些基本问题推动了W线计划，该计划目前正在返回对大浅滩和哈特拉斯角之间约39 N的DWBC和墨西哥湾流的观测。配套的野外项目正在对我们研究区域的北部和南部的DWBC进行采样，几个互补的建模项目正在进行中。综上所述，这些研究将有助于全面调查北大西洋深水向低纬度输出的机制和速率及其与上层海洋环流的关系。智力价值：拟议的研究将有助于理解北大西洋深水向低纬输出的机制和速率，以及变化的深水流量和层结变化与包括墨西哥湾流在内的上层海洋环流的关系。这一知识将有助于阐明海洋对海-气交换变化的反应，并最终阐明海洋在全球气候变化中的作用。该项目将对DWBC和墨西哥湾流的温度、盐度、示踪物和速度变化的持续观测延长到2013年，创造与计划中的26 N处的英美观测计划同步的整整10年的记录。W线计划包括伍兹霍尔以南大陆斜坡上的系泊阵列，以及沿着该阵列重复占据的水文部分，并向南延伸到马尾藻海。从船上可能进行的高空间分辨率采样正在验证阵列是否在空间上分辨年际信号以及返回用于示踪剂分析的水样。同样重要的是，调查人员将探索当前W线项目的一个子集是否足以索引该地区的水性质和交通变化，为建立长期海洋观测系统奠定基础。更广泛的影响：提出的观察将探索和测试关于西部深部边界流和墨西哥湾流相互作用的理论想法；这是当前W线资助下的一篇博士论文的重点。麻省理工学院/世界卫生组织联合计划注册的物理海洋学入门课程的学生将参加拟议的航海，向他们介绍观测海洋学。此外，该计划将继续支持一个代表性不足的小组的一名博士生，他们的论文研究将集中在获得的数据上。所有观测结果和产生的数据产品将尽快通过互联网向社区提供，目的是促进这些数据的广泛使用，以便社区的任何成员都可以在他们自己的研究计划中使用这些数据。随着数据的恢复和处理，W线观测数据可供任何感兴趣的调查人员进行模型验证和区域过程研究。除了原始观测之外，还正在制作和分发增值产品，如岩心性质的时间序列和水团运输。其他研究人员也被鼓励在W线基础设施上建设，以扩大正在采样的物理场。该项目是对美国CLIVAR(气候可变性和可预测性)计划的贡献。