Simulated Tropical Cyclone Climatology in the Tropical Channel Experiments

摘要: As described in Chap. 1, coarse resolution GCMs are capable of producing hurricane-like vortices. However, they cannot resolve the hurricane core or intensity hurricane. In addition, mesoscale processes that contribute to genesis. Coarse-resolution also have high tropical biases generally underestimate precipitation, and poorly simulate modes such as monsoons convectively coupled waves. Capturing these is important simulating TC genesis development. Since current computing capacity not sufficient run global models at very over decadal time scales, an alternative nest a high-resolution model within GCM region interest. This approach has been shown improve simulation frequency structure compared those it general adopted here. The Advanced Research WRF version 3 (ARW), adapted nested either reanalysis regional climate Nested Regional Climate Model (NRCM). Such modeling still its infancy there remains much understand about resolution. work attempt understanding projection.