Temporal and spatial variations of oceanic fronts and their impact on transportation and deposition of fine-grained sediments in the East China Shelf Seas

YUAN Ping; WANG Houjie; BI Naishuang; WU Xiao; ZHANG Yong

doi:10.16562/j.cnki.0256-1492.2019050602

2020 Vol. 40, No. 3

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Article navigation > Marine Geology & Quaternary Geology > 2020 > 40(3): 25-42

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YUAN Ping, WANG Houjie, BI Naishuang, WU Xiao, ZHANG Yong. Temporal and spatial variations of oceanic fronts and their impact on transportation and deposition of fine-grained sediments in the East China Shelf Seas[J]. Marine Geology & Quaternary Geology, 2020, 40(3): 25-42. doi: 10.16562/j.cnki.0256-1492.2019050602

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YUAN Ping, WANG Houjie, BI Naishuang, WU Xiao, ZHANG Yong. Temporal and spatial variations of oceanic fronts and their impact on transportation and deposition of fine-grained sediments in the East China Shelf Seas[J]. Marine Geology & Quaternary Geology, 2020, 40(3): 25-42. doi: 10.16562/j.cnki.0256-1492.2019050602

Temporal and spatial variations of oceanic fronts and their impact on transportation and deposition of fine-grained sediments in the East China Shelf Seas

1.
College of Marine Geosciences, Ocean University of China, Key Laboratory of Submarine Geosciences and Prospecting Technique, Ministry of Education, Qingdao 266100,China
2.
Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266071,China

More Information

Corresponding author: WANG Houjie, hjwang@ouc.edu.cn

Received Date: 06 May 2019

Revised Date: 21 May 2019

Publish Date: 25 June 2020

Abstract

Abstract

Observed hydrologic datasets and HYCOM modelling data were used in this paper to evaluate the applicability and stability of the HYCOM temperature and salinity data to the temporal-spatial distribution of oceanic fronts and its impact on transportation and deposition of fine-grained sediments in the East China Shelf Seas. The results show that the distribution of thermal fronts or salinity fronts are similar on the surface and bottom in the Bohai, Yellow and East China Seas excluding the east of Okinawa Trough. However, the strength and coverage of the fronts on the bottom are larger than those on the surface. The location of thermal fronts depends on the basic structure of currents. Both the surface and bottom thermal fronts develop along the boundaries of water masses, suggesting that thermal current fronts are closely related to the current and water masses of the study area. However, the distribution of the salinity fronts is greatly influenced by water discharge, coastal currents and warm currents. In addition, the distribution of mud patches in the Eastern China Shelf Sea are closely related to the patterns of oceanic fronts, which means that the thermal and salinity fronts do play a critical role in the formation of mud deposits.
- East China Shelf Seas /
- oceanic fronts /
- temporal and spatial variation /
- fine-grained sediment /
- sediment transportation /
- mud patches

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References

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