Tide-Induced Variability and Mechanisms of Surface Suspended Sediment in the Zhoushan Archipelago along the Southeastern Coast of China Based on GOCI Data

Yunfei Du,Jicai Zhang,Huiyi Lin,Shuangyan He,Daosheng Wang,Ya Ping Wang

doi:10.3390/rs13050929

Abstract

The variations and dynamics of suspended sediment in the coastal waters around the Zhoushan Archipelago are complex due to strong tidal dynamics. This study aims to delineate the tide-induced variability of surface suspended sediment and reveal its mechanisms in the Zhoushan Archipelago based on Geostationary Ocean Color Imager (GOCI) data. Suspended sediment concentration (SSC) estimations through the ultraviolet wavelength atmospheric correction (UV-AC) algorithm and a tuned empirical inversion algorithm using extensive in situ measurements are presented. GOCI-processed remote sensing reflectance (Rrs) is validated using field data and is cross-validated with Landsat 8 Operational Land Imager (L8/OLI) measurements, respectively. The estimated SSC is validated with independent datasets. The validations reveal that GOCI-processed Rrs is reasonable and that the GOCI-retrieved SSC is accurate and can be used to quantify SSC distributions and variations in the Zhoushan Archipelago. The variations of the SSC in the study area are closely related to the temporal variations of the tidal level. High SSCs often occur in the middle of ebb or flood tides due to large tidal discharge and high tidal velocity. Significant hourly variations of the SSC are mainly controlled by tidal forces. Dynamic mechanism analysis indicates that during neap and middle tides, the local high SSC is mainly attributed to the sediment resuspension process driven by tidal currents; in addition, during the spring tide, the variations of the SSC are simultaneously modulated by sediment resuspension and horizontal advection processes.

Highlights

Estuaries and coastal waters are the key areas for interactions between land and sea and have various physical and ecological processes, which are often characterized by high suspended sediment concentrations (SSCs) due to tides, waves, river runoff, eddies, seasonal winds, coastal currents, and human activities [1,2,3]
It is of great practical significance to fully understand the variations of suspended sediment transport and its dynamic mechanisms, which are key to understanding sedimentary processes in estuarine and coastal waters
The transport mechanisms of suspended sediments were investigated in the Zhoushan Archipelago and the results showed that advection transport and gravitational circulation transport were the primary dynamic factors in suspended sediment transport [9]

Summary

Introduction

Estuaries and coastal waters are the key areas for interactions between land and sea and have various physical and ecological processes, which are often characterized by high suspended sediment concentrations (SSCs) due to tides, waves, river runoff, eddies, seasonal winds, coastal currents, and human activities [1,2,3]. It is of great practical significance to fully understand the variations of suspended sediment transport and its dynamic mechanisms, which are key to understanding sedimentary processes in estuarine and coastal waters. Numerous islands, narrow channels, and rugged undersea terrain, the Zhoushan Archipelago is one of the most complex geographical environments in the East China Sea/Pacific

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Conclusion