Collaborative research: Air-Sea CO2 Fluxes and Surface Physical Processes in the Labrador Sea

将在拉布拉多海春季水华期间对二氧化碳的海气通量和控制它的表面物理过程进行研究。拉布拉多海是北大西洋深水形成的重要区域之一。 在晚春的几个月里，拉布拉多海经历了一次强烈的浮游生物水华，是一个强烈的二氧化碳汇。在随后的冬季，深层对流混合了整个水柱中富含二氧化碳的沃茨。 新形成的NADW通过一个深海流系统向南输送到南极。考虑到1000年量级的环流时间尺度，NADW内的大气气体基本上被隔离。虽然全球海洋的中纬度地区同样是二氧化碳的强汇，但在这些纬度被海洋吸收的气体仍留在近地表沃茨，并在十年时间尺度上返回大气。因此，拉布拉多海的气体交换特性特别令人感兴趣，因为它是全球海洋中为数不多的长期二氧化碳汇的地区之一。 预测和预报大面积海气二氧化碳通量的能力对于量化邻近陆地的碳收支也是必要的，这项工作的更广泛影响涉及到提高我们预测大气二氧化碳水平的能力，以及评估它如何在各种情景下改变气候。大气和海洋之间的二氧化碳通量存在很大的不确定性，这阻碍了我们确定人为二氧化碳汇的分配 海洋和陆地生物圈之间的联系 这种不确定性也限制了我们准确模拟未来大气二氧化碳水平的能力。 我们提出的过程研究将提高全球海洋二氧化碳通量估计的准确性，并增加我们对其可变性原因的了解。 该项目将涉及作为本科生和研究生研究助理的学生。迈阿密大学是一所西班牙裔服务机构，从而促进了科学和工程领域代表性不足的群体的参与。 这些数据将通过万维网通过若干数据库提供。 该项目将促进通过迈阿密大学教务处协调的积极外联活动。

A study of the air-sea flux of carbon dioxide and the surface physical processes controlling it will be conducted during the Labrador Sea spring bloom. The Labrador Sea is highly significant as one of the areas of North Atlantic Deep Water (NADW) formation. During the late spring months, the Labrador Sea experiences a strong plankton bloom, and is an intense sink for carbon dioxide. Deep convection during the subsequent winter mixes the carbon dioxide rich waters throughout the water column. The newly formed NADW is transported southward towards the Antarctic, via a system of deep currents. Given the circulation time scale of order 1000 years, atmospheric gases within the NADW are essentially sequestered. While mid-latitude areas of the global ocean are equally strong sinks of carbon dioxide, gases absorbed into the ocean at these latitudes remain in the near surface waters, and are returned to the atmosphere on the decadal time scale. Hence the gas exchange characteristics in the Labrador Sea are of particular interest because it is one of the few areas of the global ocean that is a long term carbon dioxide sink. The ability to predict and forecast air-sea carbon dioxide fluxes over large areas is also necessary to quantify the adjacent terrestrial carbon budget.The broader impacts of this work relate to improvement of our ability to predict atmospheric carbon dioxide levels, and to assess how it might change climate under various scenarios. The large uncertainty surrounding the flux of carbon dioxide between the atmosphere and ocean prevent us from determining the partitioning of the sink of anthropogenic carbon dioxide between the ocean and the terrestrial biosphere. This uncertainty also limits our ability to accurately model future atmospheric carbon dioxide levels. The process study we have proposed will improve the accuracy of the global ocean carbon dioxide flux estimates and increase our understanding of the causes of its variability. The project will involve students as undergraduate and post-graduate research assistants. The University of Miami is a Hispanic Serving Institution and thereby fosters the participation of under-represented groups in science and engineering. The data will be made available through several data bases via the World Wide Web. The project will contribute to the active outreach activities coordinated through the Dean's Office at the University of Miami.