Measuring interannual variability of the AMOC and meridional ocean heat transport at 26.5N: The RAPID-MOCHA Array

概述：气候模型表明，大西洋纬向翻转环流（AMOC）的变化与海表温度在年际到数十年时间尺度上的变化有关，这可能会产生深远的社会影响。此外，气候模型继续预测下一个世纪AMOC的大幅减弱，这可能通过减少北大西洋的二氧化碳吸收来反馈气候系统（2007年政府间气候变化专门委员会报告）。AMOC在气候系统中的具体作用一直难以确定，由于缺乏长期的测量其可变性。然而，美英联合海洋观测系统（沿沿着26.5°）（RAPID-MOCHA）现在已经提供了近十年来对AMOC的连续估计，揭示了其季节至年际变化的性质，这是目前唯一可用的全深度，全流域测量。RAPID-MOCHA计划已经为评估强迫、数据同化和耦合气候模式提供了一个关键的基准，并正在形成一个基本的构件，围绕该构件正在制定国际计划，以监测整个大西洋盆地的AMOC。该项目的目标是在2014年至2020年的6年内维持这一测量系统，量化AMOC的年际变化及其与北大西洋表面强迫变化的关系。还将监测26.5°N的海洋纬向热输送（MHT），包括热输送的翻转和环流分量的时变贡献。过去几年的时间序列显示出显着的年际时间尺度变化相对于前几年，这被认为是与北大西洋涛动（NAO）强迫的变化。中纬度北大西洋的海洋热含量和海表温度变化似乎也与最近的AMOC变化有关。RAPID-MOCHA项目的成果迄今主要集中在准确确定AMOC平均强度和垂直结构、其相关的热输送以及季节周期和短期变化的动态。未来的重点将是记录和了解年际变化的原因，并将在26.5°N观测到的AMOC变化与其他AMOC指数和大西洋盆地周围开发AMOC测量计划的结果联系起来。该项目的更广泛影响是为长期监测AMOC提供基础，以便了解其与观测到的气候波动的关系，我们评估气候模型预测的能力也可以得到提高。该项目将继续与来自英国的研究人员进行成功的国际合作。国家海洋学中心是联合王国的一部分。RAPID-WATCH程序美国对这一现场海洋观测系统的贡献包括：（1）利用运行中的海底电缆进行佛罗里达海流监测，并通过定期巡航进行校准，使用一次性温度下投式探空仪、船载声学多普勒海流剖面仪和水文/低层声学多普勒海流剖面仪测量，以及（2）在巴哈马以东的西部深海边界海流和安的列斯海流区域进行连续系泊时间序列测量，包括与美国国家海洋和大气管理局（NOAA）的科学家合作，每隔九个月进行一次水文/低层ADCP剖面测量。佛罗里达海流监测由NOAA独立支持。英国将为沿着26.5°N延伸的系泊阵列提供支持，以完成跨流域连续时间序列观测系统。该项目是根据美国CLIVAR（气候变化和可预测性）计划对美国AMOC的贡献，以维持从2014年3月到2020年3月的六年期间的系泊组件。

Overview: Climate models suggest that variability of the Atlantic meridional overturning circulation (AMOC) is linked to sea surface temperature changes on inter-annual to multi-decadal time scales that can have far reaching societal impacts. Additionally, climate models continue to project a substantial weakening of the AMOC over the next century that could feed back on the climate system through reduced carbon dioxide uptake in the North Atlantic (2007 Report from the Intergovernmental Panel on Climate Change). The specific role of the AMOC in the climate system has been difficult to determine due to a lack of long term measurements of its variability. However, the joint US-UK ocean observing system along 26.5°N (RAPID-MOCHA) has now provided continuous estimates of the AMOC for nearly a decade that have revealed the nature of its seasonal to inter-annual variability, the only such full-depth, basin-wide measurements currently available. The RAPID-MOCHA program has already provided a critical benchmark for evaluation of forced, data-assimilative, and coupled climate models, and is forming a fundamental building block around which international programs are being developed to monitor the AMOC throughout the Atlantic basin.Intellectual merit: The goal of this project is to maintain this measurement system for an additional 6 years, from 2014 to 2020, to quantify the inter-annual variability of the AMOC and its relationship to changes in surface forcing over the North Atlantic. The ocean meridional heat transport (MHT) at 26.5°N will also be monitored, including the time varying contributions by the overturning and gyre components of the heat transport. The last few years of the time series have shown significant inter-annual time-scale changes with respect to prior years, which are believed to be linked to changes in North Atlantic Oscillation (NAO) forcing. Ocean heat content and Sea Surface Temperature changes in the mid-latitude North Atlantic also appear to be linked to the recent AMOC changes. The results of the RAPID-MOCHA project thus far have been primarily focused on an accurate determination of the mean AMOC strength and vertical structure, its associated heat transport, and the dynamics of the seasonal cycle and shorter-term variations. The focus going forward will be to document and understand the causes of inter-annual variability and to link AMOC changes observed at 26.5°N to other AMOC indices and results from developing AMOC measurement programs around the Atlantic basin.The broader impacts of the project are to provide the basis for long-term monitoring of the AMOC, so that its relationship to observed climate fluctuations can be understood, and our ability to assess climate model predictions can be improved. This project will continue a successful international collaboration with investigators from the U.K. National Oceanography Centre as part of the U.K. RAPID-WATCH program. The U.S. contribution to this in-situ ocean observation system includes: (1) Florida Current monitoring using the operational submarine cable, calibrated by regular cruises with expendable temperature dropsondes, shipboard Acoustic Doppler Current Profiler (ADCP), and hydrographic/lowered-ADCP measurements, and (2) continuous moored time series measurements across the Deep Western Boundary Current and Antilles Current region east of the Bahamas, including hydrographic/lowered-ADCP sections at nine-month intervals in concert with scientists at the National Oceanic and Atmospheric Administration (NOAA. The Florida Current monitoring is independently supported by NOAA. The U.K. will provide support for the extended array of moorings along 26.5°N that completes the trans-basin continuous time series observing system.This project is a contribution to the US AMOC under the US CLIVAR (CLImate VARiability and predictability) program to maintain the moored component of element for a six-year period extending from March 2014 to March 2020.