Abstract

The southern Yellow Sea Cold Water Mass (YSCWM) and the Yellow Sea Warm Current (YSWC) are prominent features in the southern Yellow Sea. The traditional viewpoint is that the southern YSCWM exists in the warm half of the year and the YSWC exists in the cold half of the year; the most existing studies have regarded these features as independent ocean phenomenon. Through marine investigations conducted in the recent years in the southern Yellow Sea, the southern YSCWM was found to exist in the early winter in 2010, and the YSWC was observed in the early summer in 2013, 2014. For approximately half the year, the southern YSCWM and YSWC existed simultaneously, and the YSWC was located in a slightly high-temperature region in the middle of the southern YSCWM. A sandwich-shaped temperature structure formed in the middle of the southern Yellow Sea from spring to autumn. This article studies the seasonal variation characteristics of the three-dimensional southern YSCWM and YSWC structures using ocean survey data collected in the recent years. The new perspective of the seasonal variations in the southern YSCWM and YSWC obtained herein will promote the recognition of southern Yellow Sea water exchanges and support biogeochemical cycle research in the Yellow Sea.

Highlights

  • The Yellow Sea is a semiclosed and shallow marginal sea located between the Chinese mainland and the Korean Peninsula

  • The thermocline descended to a depth of approximately 50 m, the 2 cold cores of the Yellow Sea Cold Water Mass (YSCWM) were clearly located at similar positions to those identified in summer, when the YSCWM is the strongest within the year

  • The relatively high temperature measured at approximately 123◦E between the 2 cold cores in the YSCWM implied the appearance of the Yellow Sea Warm Current (YSWC) in the same time period

Read more

Summary

Introduction

The Yellow Sea is a semiclosed and shallow marginal sea located between the Chinese mainland and the Korean Peninsula. The Yellow Sea borders the Bohai Sea to the north and is open to the East China Sea to the south. A deep trough with a maximum depth of more than 80 m is located in the central Yellow Sea. The most important physical features of the Yellow Sea are the existence of the Yellow Sea Cold Water Mass (YSCWM) in the summer season and the Yellow Sea Warm. Sandwich Structure YSCWM YSWC Mooring name Position.

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call