The upper-ocean responses to Typhoon Megi(2010)are investigated using data from ARGO floats and the satellite TMI.The experiments are conducted using a three-dimensional Princeton Ocean Model(POM)to assess the storm,which affected the Northwest Pacific Ocean(NWP)and the South China Sea(SCS).Results show that the upwelling and entrainment experiment together account for 93% of the SST anomalies,where typhoon-induced upwelling may cause strong ocean cooling.In addition,the anomalous SST cooling is stronger in the SCS than in the NWP.The most striking feature of the ocean response is the presence of a two-layer inertial wave in the SCS—a feature that is absent in the NWP.The near-inertial oscillations can be generated as typhoon wakes,which have maximum flow velocity in the surface mixed layer and may last for a few days,after the typhoon’s passage.Along the typhoon tracks,the horizontal currents in the upper ocean show a series of alternating negative and positive anomalies emanating from the typhoon. The upper-ocean responses to Typhoon Megi (2010) are investigated using data from ARGO floats and the satellite TMI. The experiments are conducted using a three-dimensional Princeton Ocean Model (POM) to assess the storm, which affected the Northwest Pacific Ocean ( NWP) and the South China Sea (SCS). Results show that the upwelling and entrainment experiment together accounts for 93% of the SST anomalies, where typhoon-induced upwelling may cause strong ocean cooling. In addition, the anomalous SST cooling is stronger in the SCS than in the NWP. The most striking feature of the ocean response is the presence of a two-layer inertial wave in the SCS-a feature that is absent in the NWP. near-inertial oscillations can be generated as typhoon wakes, which have maximum flow velocity in the surface mixed layer and may last for a few days, after the typhoon’s passage. Along the typhoon tracks, the horizontal currents in the upper ocean show a series of alternating negative and positive anomalies emanating f rom the typhoon.