Hydraulics of a two-layer rotating flow; Application to the Korea Strait

  • Cho, Yang-Ki (Department of Oceanography, Seoul National University) ;
  • Kim, Kuh (Department of Oceanography, Seoul National University)
  • Published : 1995.10.01

Abstract

The Korea Strait becomes deeper than 200 m from south to north in general except coastal area, whereas its southern part is shallower than 125 m except for a deep trough (Fig.1). The flow in the Korea Strait could be simplified as two layers (Isobe, 1995); the Tsushima Warm Water in the upper layer and the Korea Strait Bottom Cold Water (KSBCW) in the lower layer (Fig.2). (omitted)

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