Ice-Ocean Interactions on the Okhotsk Sea Shelf

0526011鄂霍次克海通过影响北太平洋中层水的形成，在北太平洋环流中起着重要作用。此外，它有一个高度可变的海冰覆盖，这不仅影响水团的形成，而且还影响了亚极地北太平洋上空的大气环流。密集的水形成的沿着鄂霍次克海陆架是这个NPIW的来源，并严重依赖于沿海冰穴和潮汐混合的细节，以及它们与分层和平均环流的关系。虽然最近的观测表明，盐水排斥海冰沉没在潮汐前沿的货架上，许多问题仍然是冰间湖开口，冰的生产，海洋冰热交换和货架动态之间的关系。智力成果：在本项目中，华盛顿大学的海洋学家将利用一个区域冰-海耦合模型进行一系列敏感性实验，以调查海冰和水团的形成及其年际变化。 除了耦合区域海洋模型系统（地形跟踪沿海海洋模型）和社区海冰模型（复杂的动力学-热力学海冰模型）外，研究人员还将采用新的高质量数据集进行模型强迫，初始化和验证。 这项工作的成果将包括将现有数据与鄂霍次克海模型相结合，该模型还将考虑到该区域重要的物理海洋学过程。还将对该区域的热量和淡水收支进行分析，重点是季节周期和年际变化。将对模型中密集水的形成进行量化，并测试模型对潮汐影响的敏感性。 除了区域模型之外，研究人员还将使用共同体气候系统模型（CCSM，全球气候模型）分析鄂霍次克海的影响。 区域海洋冰模式将用于估计CCSM中缺少的过程的重要性。 更广泛的影响：这项工作的结果不仅将提高对冰穴的认识，还将提高鄂霍次克海潜在的全球重要性。 除了培训研究生外，这项工作还将与NCAR的社区气候系统模型项目建立伙伴关系。在区域范围内使用CCSM海冰模式将有助于CCSM的未来发展，因为新一代超级计算机可以进行更高分辨率的气候模拟。

0526011The Okhotsk Sea plays an important role in the North Pacific Ocean circulation through its influence on the formation of the North Pacific Intermediate Water (NPIW). In addition, it has a highly variable sea ice cover, which influences not only water mass formation, but also the atmospheric circulation over the sub-polar North Pacific. The dense water formed along the Okhotsk Sea shelves is the source of this NPIW and depends critically on the details of the coastal polynyas and tidal mixing, and their relation to the stratification and mean circulation. Though recent observations have shown that brine rejection from sea ice sinks at the tidal front over the shelves, many questions remain as to the relationship among polynya openings, ice production, ocean-ice heat exchange, and shelf dynamics. Intellectual merit:In this project, oceanographers at the University of Washington will perform a series of sensitivity experiments with a regional coupled ice-ocean model to investigate the sea ice and water mass formation and their inter-annual variability. In addition to coupling the Regional Ocean Model System, a terrain following coastal ocean model, and the Community Sea Ice Model, a sophisticated dynamic-thermodynamic sea ice model, the researcher will also employ new, high quality datasets for model forcing, initialization, and verification. The outcomes of the work will include an integration of available data with a model of the Okhotsk Sea that will also take into account the important physical oceanographic processes in the region. An analysis of the heat and fresh water budgets of the region will also be made, focusing on both the seasonal cycle and inter-annual variability. The dense water formation in the model will be quantified, and the sensitivity of the model to the influence of tides will be tested. In addition to the regional modeling, the researcher will also analyze the influence of the Okhotsk Sea on a larger scale using the Community Climate System Model (CCSM, a global climate model). The regional ocean-ice model will be used to estimate the importance of processes that are absent from the CCSM. Broader Impacts:The results from this work will not only lead to an improved understanding of polynyas but also to the potential global importance of the Okhotsk Sea. In addition to training a graduate student, the work will also develop a partnership with the Community Climate System Model project at NCAR. The use of the CCSM sea-ice model in a regional context will help with future development of the CCSM as the new generation of super-computers allow for higher resolution climate simulations.