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南大洋生物地球化学浮标部署策略,以格林威治子午线(GO-SHIP A12)为例。

Southern Ocean Biogeochemical Float Deployment Strategy, With Example From the Greenwich Meridian Line (GO-SHIP A12).

作者信息

Talley L D, Rosso I, Kamenkovich I, Mazloff M R, Wang J, Boss E, Gray A R, Johnson K S, Key R M, Riser S C, Williams N L, Sarmiento J L

机构信息

Scripps Institution of Oceanography University of California, San Diego La Jolla CA USA.

Rosenstiel School of Marine and Atmospheric Sciences University of Miami Miami FL USA.

出版信息

J Geophys Res Oceans. 2019 Jan;124(1):403-431. doi: 10.1029/2018JC014059. Epub 2019 Jan 21.

Abstract

Biogeochemical Argo floats, profiling to 2,000-m depth, are being deployed throughout the Southern Ocean by the Southern Ocean Carbon and Climate Observations and Modeling program (SOCCOM). The goal is 200 floats by 2020, to provide the first full set of annual cycles of carbon, oxygen, nitrate, and optical properties across multiple oceanographic regimes. Building from no prior coverage to a sparse array, deployments are based on prior knowledge of water mass properties, mean frontal locations, mean circulation and eddy variability, winds, air-sea heat/freshwater/carbon exchange, prior Argo trajectories, and float simulations in the Southern Ocean State Estimate and Hybrid Coordinate Ocean Model (HYCOM). Twelve floats deployed from the 2014-2015 Polarstern cruise from South Africa to Antarctica are used as a test case to evaluate the deployment strategy adopted for SOCCOM's 20 deployment cruises and 126 floats to date. After several years, these floats continue to represent the deployment zones targeted in advance: (1) Weddell Gyre sea ice zone, observing the Antarctic Slope Front, and a decadally-rare polynya over Maud Rise; (2) Antarctic Circumpolar Current (ACC) including the topographically steered Southern Zone where upwelling carbon/nutrient-rich deep waters produce surprisingly large carbon dioxide outgassing; (3) Subantarctic and Subtropical zones between the ACC and Africa; and (4) Cape Basin. Argo floats and eddy-resolving HYCOM simulations were the best predictors of individual SOCCOM float pathways, with uncertainty after 2 years of order 1,000 km in the sea ice zone and more than double that in and north of the ACC.

摘要

由南大洋碳与气候观测及建模项目(SOCCOM)在南大洋各处部署的生物地球化学Argo浮标,可探测至2000米深度。目标是到2020年部署200个浮标,以提供跨多个海洋学区域的首套完整的碳、氧、硝酸盐和光学特性年度循环数据。从之前没有覆盖到形成一个稀疏阵列,部署是基于对水体属性、平均锋面位置、平均环流和涡旋变率、风、海气热/淡水/碳交换、先前的Argo轨迹以及南大洋状态估计和混合坐标海洋模型(HYCOM)中的浮标模拟的先验知识。从2014年至2015年从南非到南极洲的“极地星”号巡航中部署的12个浮标被用作测试案例,以评估SOCCOM迄今为止的20次部署巡航和126个浮标所采用的部署策略。几年后,这些浮标仍继续代表预先设定的部署区域:(1)威德尔环流海冰区,观测南极陆坡锋以及莫德海隆上一个数十年一遇的冰间湖;(2)南极绕极流(ACC),包括地形引导的南区,那里富含碳/营养物质的上升深层水产生了惊人的大量二氧化碳排放;(3)ACC与非洲之间的亚南极和亚热带区域;以及(4)好望角海盆。Argo浮标和能解析涡旋的HYCOM模拟是单个SOCCOM浮标路径的最佳预测指标,在海冰区,2年后的不确定性约为1000千米,而在ACC及其以北地区则超过这个数值的两倍。

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