동중국해에서 태풍 나리 통과후 관측된 관성진동

Abstract

To understand temporal variation of the sea water characteristic, ADOS drifters with temperature and pressure sensors are deployed in the East. Thermal structure of upper layer in the East China Sea was affected by the typhoon Nari passing at 15th to 16th of September in 2007. After immediately the typhoon passing, we found the characteristic of inertial oscillation. While the typhoon passing, inertial wave with about 24 hours period strongly shown and the clockwise rotation component is predominant. The phase between upper and lower layer show the difference more than 90°.