Absolute Velocity, Transport and Stability of the Polar Front Downstream of the Southeast Indian Ridge

IF 3.3 2区 地球科学 Q1 OCEANOGRAPHY
Annie Foppert, Stephen R. Rintoul, Helen E. Phillips
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Abstract

The fronts of the Antarctic Circumpolar Current (ACC) influence the growth and instability of eddies, eddy-mean flow interaction, and the development of submesoscale processes. We use in situ hydrography and directly measured velocity from a comprehensive shipboard survey of the Polar Front (PF) south of Tasmania to characterize the synoptic mean velocity and transport structure of the PF. A stream-coordinate system, based on dynamic height anomaly (ϕ), is constructed to create an along- and across-stream perspective of the PF that naturally follows the current. We find the surface-intensified along-stream flow carries a full-depth transport of 80.5 Sv over a width of 90 km, with roughly two-thirds carried by the baroclinic flow. The across-stream velocities are largely depth-independent; the mean depth-averaged flow across the PF core is 0.08 m s−1 in the quasi-northward direction, associated with along-isopyncal downwelling and cold water advection. We calculate potential vorticity (PV) to investigate the stability of the PF and find it is susceptible to both baroclinic and barotropic instability. Mean PV is dominated by the thickness PV term f N 2 g $\left(\frac{f{N}^{2}}{g}\right)$ , that is PV is controlled by changes in stratification. While strong upper-ocean PV gradients indicate a barrier to mixing, weaker PV gradients and relatively elevated mixing lengths at mid-depth (≈2,000–2,500 m depth) suggest a deep steering level where eddies can efficiently mix properties across the PF.

Abstract Image

东南印度洋脊下游极锋的绝对速度、输送和稳定性
南极环极流锋面影响着涡旋的生长和不稳定、涡旋-平均流相互作用以及亚中尺度过程的发展。我们利用对塔斯马尼亚南部极锋(PF)的现场水文测量和直接测量的速度来表征PF的天气平均速度和运输结构。基于动态高度异常(ϕ)的流坐标系统构建了一个沿流和跨流的PF视角,自然地跟随洋流。我们发现,地表增强的沿流流在90 km的宽度上携带80.5 Sv的全深度输送,其中大约三分之二由斜压流携带。跨流速度在很大程度上与深度无关;在准北方向上,通过PF核心的平均深度流为0.08 m s - 1,并伴有沿等锥向下流动和冷水平流。我们计算了位涡量(PV)来研究气流的稳定性,发现气流易受斜压和正压不稳定的影响。平均PV由厚度PV项f n2 g $\left(\frac{f{N}^{2}}{g}\right)$决定,即PV受分层变化的控制。虽然强的上层海洋PV梯度表明存在混合障碍,但在中深度(≈2,000-2,500 m深度)较弱的PV梯度和相对较高的混合长度表明存在深层转向水平,涡流可以有效地混合整个PF的特性。
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来源期刊
Journal of Geophysical Research-Oceans
Journal of Geophysical Research-Oceans Earth and Planetary Sciences-Oceanography
CiteScore
7.00
自引率
13.90%
发文量
429
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