Collaborative Research: AnSlope Analysis

这项合作研究将分析为期三年的南极坡前项目（“AnSlope”）期间获得的南极海洋学数据集，该项目的目的是确定和量化制约南极密集陆架沃茨转移到邻近深海中层和深层的主要物理过程，以及开阔洋沃茨越过陆架断裂处的补偿性向极地流动。 研究活动将围绕以下内容组织：（i）罗斯海西北部坡锋区域的完整描述，包括坡锋的结构和密集陆棚水的充满活力的外流;和（ii）详细研究跨锋面交换的动态及其与环境强迫（海洋、海冰、大气）的关系。这项工作将评估源自不同陆架槽的密集外流下降的空间和时间尺度;卷吸、温压和底栖压力对外流稀释、下降和扩散的作用;以及驱动陆架侵入和跨等深线运动的主要机制。 最终，由数据解释指导的模拟研究将促进全球海洋模型中跨坡交换参数化的发展，虽然起源于南极的冷水团对全球海洋环流和气候的重要性是毋庸置疑的，但这些水团进入深海环流的过程却不是。 南极洲周围的上大陆坡已被确定为大陆架和深海沃茨交换的主要通道。 在这里，与几乎无处不在的锋面相关的地形、速度和密度场肯定会强烈影响陆棚和海洋状况之间水性质的平流和湍流传输。 这一门户的强度和可变性对于维持世界海洋的结构至关重要。

This collaborative study will analyze the antarctic oceanographic dataset obtained during the three-year Antarctic Slope Front Project ("AnSlope"), whose objective was to identify and quantify the principal physical processes governing the transfer of dense antarctic shelf waters into intermediate and deep layers of the adjacent deep ocean, and the compensatory poleward flow of open ocean waters across the shelf break. Research activities will be organized around: (i) a full description of the northwestern Ross Sea slope front region including the structure of the slope front and the energetic outflows of dense shelf water; and (ii) detailed study of the dynamics of cross-frontal exchange and their relationship to environmental forcing (ocean, sea ice, atmosphere). The work will evaluate the spatial and temporal scales of the descending dense outflows that originate in different shelf troughs; the roles of entrainment, thermobaricity, and benthic stress on the dilution, descent and spreading of the outflows; and the primary mechanisms driving on-shelf intrusions and cross-isobath motions. Ultimately, modeling studies guided by the data interpretation will facilitate the development of parameterizations of cross-slope exchanges in global ocean models.While the importance of cold water masses originating in the Antarctic to the global ocean circulation and climate is unquestioned, the processes by which these water masses enter the deep ocean circulation are not. The upper continental slope around Antarctica has been identified as the primary gateway for the exchange of shelf and deep ocean waters. Here the topography, velocity and density fields associated with the nearly ubiquitous front must strongly influence the advective and turbulent transfer of water properties between the shelf and oceanic regimes. The strength and variability of this gateway is critical in maintaining the structure of the world ocean.