A typhoon (hurricane) is a very strong local disturbance that can affect ocean water as deep as 1000 m. According to observations and numerical simulations, the decrease in ocean temperature is believed to be caused by inertial pumping, entrainment, upwelling, and a pressure-gradient force; however, these assumptions are mostly based on modeling and do not have a clear dynamic mechanism. Therefore, in this study, the dynamic mechanism of ocean water in a highly-idealized ocean and wind field was calculated. Within the maximum wind range, upwelling in the ocean surface is caused as per the classical Ekman layer theory. Then, a pressure-gradient force drives a cyclo-geostrophic current. Because it provides centripetal force, the pressure-gradient force decreases with increasing depth. These different currents generate friction that is similar to bottom Ekman pumping, leading to upwelling. In the actual ocean, the pressure-gradient force is not only balanced by centripetal force but also baroclinic force. When these forces are balanced, the pressure-gradient force disappears, and the dynamic motion of the ocean water stops. Thus, upwelling no longer occurs. The depth at which this balance occurs is considered to be the maximum depth that a typhoon can impact. Therefore, the pressure-gradient force, caused by typhoons and then offset by centripetal and baroclinic forces, is the original dynamic of upwelling in deep ocean water.