Observations of the Near-Field Yellow River Plume, Multiple Fronts and Their Biogeochemical Effects

IF 3.3 2区 地球科学 Q1 OCEANOGRAPHY
Zhixing Chen, Tao Wang, Dan Xu, Wensheng Jiang, Changwei Bian
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Abstract

River plumes transport fresh water into the ocean, and exhibit intense convergent and turbulent processes in the frontal regions, ultimately influencing coastal ecosystems. Satellite images show multiple fronts can be generated in river plumes. Although some efforts have been done to study the generation of multiple fronts inside river plumes by theoretical, numerical modeling and laboratory methods, their generation mechanisms and effects on biogeochemical processes remain to be clarified through in situ observational evidence. In the present study, the near-field Yellow River plume, multiple fronts and their biogeochemical effects are investigated through moored, shipboard, and remote sensing observations. Numerical model simulations are conducted to help study the tidal movement of the Yellow River plume. The results show that the near-field Yellow River plume is generally advected back and forth in the east‒west direction under the effects of tidal currents. Following the plume leading front, a turbulent bore is observed to be generated and mix near-surface water with low turbidity and high concentration of dissolved oxygen into the water column. Behind the turbulent bore, a series of subfronts with distances of O (∼100 m) are formed. The generation mechanisms of these subfronts are found to be associated with internal shear instabilities. Under the effects of cross-front shear currents and vertical mixing near the subfronts, a three-layer structure of turbidity and surface low-turbidity stripes form inside the plume. Multiple fronts also have significant effects on the accumulation of surface materials.

近场黄河羽流观测、多重锋面及其生物地球化学效应
河流羽流将淡水输送到海洋中,并在锋面区域表现出强烈的汇聚和湍流过程,最终影响沿岸生态系统。卫星图像显示,河流羽流中会产生多重锋面。虽然人们已经通过理论、数值模拟和实验室方法对河流羽流中多重锋面的产生进行了一些研究,但其产生机理及其对生物地球化学过程的影响仍有待于通过现场观测证据加以澄清。本研究通过系泊观测、船上观测和遥感观测,对黄河近场羽流、多锋及其生物地球化学效应进行了研究。同时还进行了数值模型模拟,以帮助研究黄河羽流的潮汐运动。结果表明,在潮汐流的作用下,近场黄河羽流一般沿东西方向来回平移。在羽流前沿之后,观察到产生了一个湍流孔,将浊度低、溶解氧浓度高的近表层水混合到水体中。在湍流孔后面,形成了一系列距离为 O(∼100 米)的子前沿。这些子前沿的产生机制与内部剪切不稳定性有关。在交叉锋面剪切流和子锋面附近垂直混合的作用下,羽流内部形成了浊度和表面低浊度条纹的三层结构。多重锋面对表面物质的堆积也有显著影响。
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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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