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Ji Chengzhen,Ge Yong,Li Jian, et al. Study of the Yellow Sea responses to peripheral processes of Typhoon Chan-hom[J]. Haiyang Xuebao,2020, 42(1):46–53,doi:10.3969/j.issn.0253−4193.2020.01.006
Citation: Ji Chengzhen,Ge Yong,Li Jian, et al. Study of the Yellow Sea responses to peripheral processes of Typhoon Chan-hom[J]. Haiyang Xuebao,2020, 42(1):46–53,doi:10.3969/j.issn.0253−4193.2020.01.006

Study of the Yellow Sea responses to peripheral processes of Typhoon Chan-hom

doi: 10.3969/j.issn.0253-4193.2020.01.006
  • Received Date: 2018-12-10
  • Rev Recd Date: 2019-02-28
  • Available Online: 2021-04-21
  • Publish Date: 2020-01-25
  • In September 2015, Typhoon Chan-hom passed over the buoy named QF111 that can record the ocean temperature and current in the Yellow Sea. Affected by the typhoon, the drop of the sea surface temperatures is obvious, the cooling rate is in 2−4℃, and there formed low temperature patches below 20℃ at the right side of the typhoon path. The current increased during the transit of the typhoon, the velocity is up to 1.2−1.5 m/s, presenting the characteristics of reinforcement from the surface to the bottom. The result that wind did the work to the ocean indicates that wind always input the energy to the ocean, it reached the largest during typhoon transited, and the rotate power spectrum analysis results show that the energy from the wind spread to the ocean interior. The inertial oscillation inspired by the typhoon damp faster in the Yellow Sea, according to the evolution of the inertia horizontal kinetic energy, the e-folding time of the inertial oscillation is about two days.
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