A Numerical Study on the Circulation in Deukryang Bay -I. Tidal Circulation forced by $M_2$-tide-

득량만의 해수유동에 관한 수치실험 -1. $M_2$ 조에 의한 해수유동-

  • JUNG Eun-Jin (Department of Oceanography, National Fisheries University of Pusan) ;
  • HONG Chol-Hoon (Research Center for Ocean Industrial Development, National Fisheries University of Pusan) ;
  • LEE Byung-Gul (Research Center for Ocean Industrial Development, National Fisheries University of Pusan) ;
  • CHO Kyu-Dae (Department of Oceanography, National Fisheries University of Pusan)
  • 정은진 (부산수산대학교 해양학과) ;
  • 홍철훈 (부산수산대학교 해양산업개발연구소) ;
  • 이병걸 (부산수산대학교 해양산업개발연구소) ;
  • 조규대 (부산수산대학교 해양학과)
  • Published : 1994.07.01

Abstract

Circulations in Deukryang Bay are investigated using a numerical shallow water model. In the flow fields observed at four stations, north-south velocity components are dominant. In the model, the circulation forced by $M_2$-tide basically corresponded well to the observations. The model shows the strong currents in the mouth and the eastern part in the bay with about 60 cm/s and 50 cm/s, respectively. The model also shows the eddies in the tidal residual currents. To investigate the mechanism of eddy formation some numerical experiments are carried out. The results show that inertial and topographic effects play an important role in the eddy formation.

Keywords