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首页> 外文期刊>Ocean Dynamics >Vertical mixing and elements of mesoscale dynamics over North Carolina shelf and contiguous Gulf Stream waters
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Vertical mixing and elements of mesoscale dynamics over North Carolina shelf and contiguous Gulf Stream waters

机译:北卡罗来纳州陆架和连续的墨西哥湾流水域的垂直混合和中尺度动力学要素

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摘要

Results of microstructure measurements conducted in October-November of 2015 as a part of the Coupled Air Sea Processes and Electromagnetic Ducting Research (CASPER) project are discussed. The measurements were taken on the North Carolina shelf and across the Gulf Stream front. On the shelf, the oceanic stratification was influenced by highly variable surface salinity and along-bottom advection. Vertical mixing was mostly governed by variable winds. The vertical eddy diffusivity was estimated using the VMP-based dissipation measurements, and the diffusivity values obtained during calm periods and stormy winds were compared. Parameterization of the diffusivity for various mesoscale dynamical conditions is discussed in terms of shear instabilities and internal wave-generated turbulence based on data obtained in deep waters of the Gulf Stream and on the continental slope.
机译:讨论了2015年10月至11月进行的微结构测量结果,这是气海过程和电磁风管研究耦合项目(CASPER)的一部分。测量是在北卡罗来纳州的架子上和墨西哥湾流的整个前沿进行的。在架子上,海洋分层受到高度变化的表面盐度和沿底部平流的影响。垂直混合主要受风的影响。使用基于VMP的耗散测量值估算垂直涡流扩散率,并比较在平静期和暴风中获得的扩散率值。基于在湾流深水区和大陆坡上获得的数据,根据剪切不稳定性和内部波产生的湍流,讨论了各种中尺度动力条件下扩散系数的参数化。

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