Interplay Between Wind-Driven Advection and Mixing of Salt and Dissolved Oxygen in a Microtidal Estuary

IF 3.3 2区 地球科学 Q1 OCEANOGRAPHY
Jianxing Wang, Johanna H. Rosman, James L. Hench, Nathan S. Hall, Anthony C. Whipple, Richard A. Luettich Jr.
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Abstract

Most work on how estuarine dynamics impact dissolved oxygen (DO) distributions has focused on tides, but in shallow estuaries with large fetch or small tides, wind can be the primary mixing agent and also drives advection. To investigate how these processes affect DO distributions, an observational study was conducted in the shallow, microtidal Neuse Estuary. Salinity, DO, and velocity profiles were measured at multiple positions along and across the estuary over a 6-month period. A one-dimensional model (General Ocean Turbulence Model) provided additional insight into the response of salinity and DO to wind. Salinity and oxygen conservation equation terms were calculated from observations and simulations. Cross-estuary wind drove lateral circulation and tilted the isohalines, reducing stratification; lateral advection and enhanced mixing reduced vertical gradients and increased the bottom DO. Down-estuary wind tended to increase the exchange flow and stratification, but concurrently the surface wind-mixed layer deepened over time. The balance of these processes determined if the water column became fully mixed or remained stratified, and the depth of the pycnocline and oxycline. An expression for steady state surface layer thickness was derived by considering the competition between the horizontal and vertical buoyancy flux, and the predictions agreed well with observations and simulations. Up-estuary wind inhibited the exchange flow and the combination of advection and mixing homogenized the water column. While these patterns generally held for purely across- or along-channel wind, the response was often more complex as the wind vector varied in orientation and with time.

微潮河口风力平流与盐溶解氧混合的相互作用
大多数关于河口动力学如何影响溶解氧(DO)分布的研究都集中在潮汐上,但在潮汐大或小的浅河口,风可以是主要的混合剂,也可以驱动平流。为了研究这些过程如何影响DO的分布,我们在浅水微潮的新河口进行了观测研究。盐度、DO和流速剖面在6个月的时间里沿着河口和河口的多个位置进行了测量。一维模型(一般海洋湍流模型)提供了盐度和DO对风的响应的额外见解。盐度和氧守恒方程项由观测和模拟计算得到。入海口风驱动横向环流,使等盐线倾斜,分层减少;横向平流和增强的混合降低了垂直梯度,增加了底部DO。河口下风有增加交换流和分层的趋势,但同时表层风混合层也随着时间的推移而加深。这些过程的平衡决定了水柱是否完全混合或保持分层,以及斜斜层和氧斜层的深度。考虑水平和垂直浮力通量之间的竞争,导出了稳态地表层厚度的表达式,预测结果与观测和模拟结果吻合较好。河口上风向抑制了交换流,平流和混合的结合使水柱均匀化。虽然这些模式通常适用于纯粹的跨通道或沿通道的风,但随着风矢量在方向和时间上的变化,响应往往更加复杂。
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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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