Collaborative Research: CLIMODE

0424865智力优势：这个过程实验的重点是北大西洋副热带模式水18度水的形成、演化、储存、扩散和大范围后果。模式水是海-气交换的物理表现，通过连续的冬季暴露，构成了气候系统内的长期记忆。目前对这些水域的年更新率和相关物理机制的了解不足；从气候学海气通量推断的水团转化似乎与体积分析和估计的消散过程都不一致。假设目前的形成速度估计是不准确的，原因是：(1)对海-气通量的估计很差；(2)对侧向海洋过程的了解/描述很差。通过海洋-大气观测和模拟研究的综合，CLIMODE计划(CLIVAR模式水动力学实验)将：(I)调查世界海洋中所有副热带模式水域的共同过程，这些过程被发现向赤道方向的强纬向流(特别是墨西哥湾流、黑潮延伸、东澳大利亚流、阿古拉斯回流和南极绕极流)。(2)重点关注在海气交换中非常重要的区域，在分离的墨西哥湾流上发生了巨大的海洋到大气热损失，在那里通量估计的不确定性很大。(3)探讨与副热带气旋边缘冬季对流有关的水团形成、其向层结内部的俯冲以及其在气旋周围的扩散和消散之间的跨尺度联系。(4)处理气候模型中目前知之甚少、表现不足的一个关键过程--地转涡与混合层的相互作用。这是影响当代气候模型的最关键的参数之一。CLIMODE将提供涡旋和混合层相互作用的现场观测和分析，以支持CLIVAR海洋混合气候过程小组，负责开发/测试参数。更广泛的影响：CLIMODE将产生广泛的科学影响，因为它直接研究具有气候意义但在气候模型中没有充分反映的海洋现象和大气-海洋耦合。此外，通过对这些过程的气候模型参数进行评估/验证，气候变化和气候变化研究中心将产生相当大的社会影响。CLIMODE项目还将有助于参与这项研究的几名研究生和博士后研究人员的职业发展。在五年计划期间，CLIMODE每年将直接支持5名学生和4名博士后。

0424865Intellectual Merit: This process experiment is focused on the formation, evolution, storage, dispersal and large-scale consequences of Eighteen Degree Water, the subtropical mode water of the North Atlantic. Mode waters are a physical manifestation of air-sea exchange that, through successive wintertime exposure, constitute a long-term memory within the climate system. Present understanding of the annual renewal rate of these waters and the responsible physical mechanisms is deficient; water mass transformations inferred from climatological air-sea fluxes appear incompatible with both volumetric analyses and estimated dissipation processes. It is hypothesized that current formation rate estimates are inaccurate due to (i) poorly estimated air-sea fluxes and (ii) poorly understood/represented lateral ocean processes. Through a synthesis of ocean-atmosphere observations and modeling studies, the CLIMODE program (CLIvar MOde water Dynamics Experiment) will: (i) Investigate processes common to all subtropical mode waters in the world ocean, which are found equatorward of strong zonal flows (in particular the Gulf Stream, the Kuroshio Extension, the East Australian Current, the Agulhas Return Current and the Antarctic Circumpolar Current). (ii) Focus on a region of great importance in air-sea exchange huge ocean to atmosphere heat loss occurs over the separated Gulf Stream where uncertainties in flux estimates are large. (iii) Explore the cross-scale connection between water mass formation associated with wintertime convection on the rim of the subtropical gyre, its subduction into the stratified interior, and its dispersal and dissipation around the gyre. (iv) Address a key process that is presently poorly understood and inadequately represented in climate models - the interaction of geostrophic eddies with mixed layers. This is one of the most critical parameterizations that compromises the present generation of climate models. CLIMODE will provide field observations and analysis of the interaction of eddies and the mixed layer, in support of the CLIVAR Climate Process Team in ocean mixing responsible for developing/testing parameterizations. Broader Impact: CLIMODE will have broad scientific impact because it directly addresses oceanic phenomena and atmosphere-ocean coupling that have climatic significance but which are inadequately represented in climate models. Furthermore, through assessment/validation of the climate model parameterizations of these processes, CLIMODE will have considerable societal impact. The CLIMODE project will also contribute to the career advancement of several graduate students and postdoctoral investigators who will participate in the study. On average during the 5 year program, CLIMODE will directly support 5 students and 4 post-docs each year.