论文部分内容阅读
In the context of a model of tropical cyclone intensity based on an improved meso-scaleatmospheric model, numerical simulation is performed of the track and intensity variation oftropical cyclones (TC) arising from sea surface temperature (SST) variation over a specified searegion. Evidence suggests that the model is capable of modeling quite welt the track and intensityof TC: SST variation leads to an abrupt change in the cyclone intensity: the response of thecyclone to the abrupt SST change lasts 8—12 h.
In the context of a model of tropical cyclone intensity based on an improved meso-scaleatmospheric model, numerical simulation is performed on the track and intensity variation oftropical cyclones (TC) variation from a specified searegion. Evidence suggests that the model is capable of modeling quite welt the track and intensity of TC: SST variation leads to an abrupt change in the cyclone intensity: the response of thecyclone to the abrupt SST change lasts 8-12 h.