A Morphodynamic Modeling Study on the Formation of the Large‐Scale Radial Sand Ridges in the Southern Yellow Sea. Issue 7 (5th July 2019)

• Record Type: Journal Article
• Authors: Tao, Jianfeng; Wang, Zheng Bing; Zhou, Zeng; Xu, Fan; Zhang, Changkuan; Stive, Marcel J.F.
• Is Part Of: Journal of geophysical research. Volume 124:Issue 7(2019)
• Page Start: 1742
• Page End: 1761
• Publication Date: 2019-07-05
• Subjects: radial sand ridges -- morphodynamic modeling -- tidal wave systems -- Jiangsu Coast -- Southern Yellow Sea; Geomorphology -- Periodicals; 551.3
• DOI: 10.1029/2018JF004866
• Languages: English
• ISSNs: 2169-9003

Abstract

Abstract: The radial sand ridges (denoted as "RSRs" hereafter) in the Southern Yellow Sea, China, are morphologically striking because of the remarkable size and radial planar orientation, standing out as a unique coastal geomorphology among the worldwide sand ridge systems. The formation of this giant fan‐shaped geomorphic feature requires delicate conditions and awaits in‐depth investigation. Using an idealized morphodynamic model, this study unravels the governing factors for the formation of the unique large‐scale RSRs, in comparison with other types of sand ridge systems over the world. The effects of the M2 tidal constituent, the Coriolis forcing, the bed resistance, and the initial water depths on the morphodynamic behavior of the RSRs are explored. Numerical results indicate that the tidal regime, characterized by rotational and progressive current action associated with the tidal bulge, is dependent on the eastern coastline of China as well as latitudinal effects. Through the comparison between the simulated and the measured morphology, this tidal regime is demonstrated to be the key driver in forming and maintaining the present‐day RSRs. The runs with different parameters further suggest that the asymmetric pattern of the RSRs, which shows larger northern sand ridges than the southern ones, results from both the asymmetric distribution of current activity caused by the tidal bulge and unequal sediment supply. Overall, this study highlights the delicate condition, predominantly represented by the particular currents set up by the tidal wave system and the sediment supply, required to shape the striking large‐scale RSRs in the Southern Yellow Sea. Key Points: The unique giant fan‐shaped morphology of the radial sand ridges (RSRs) is numerically simulated The formation of the RSRs requires delicate conditions governed by currents originating from the rotational, progressive tidal wave system The mechanism underlying the asymmetric spatial pattern of the RSRs is revealed