热带气旋“玲玲”期间海-气界面热通量的估算与分析

Based on the remote sensing data combined with reanalysis data, and the COARE3.0 algorithm, the air-sea interface heat fluxes were estimated and analyzed during the 2001 tropical cyclone "Lingling". The results show that: the air-sea interface heat flux is mainly in latent heat flux during tropical cyclones; the heat flux is more influenced by the sea surface temperature in the warm eddy and cold eddy regions. The existence of the warm eddy, resulting in the increase of heat flux for providing a large number of heat energy to tropical cyclone, will be conducive to the development and maintenance of tropical cyclones. The existence of the cold eddy, reducing the heat flux, so the sensible heat flux significantly decreases in particular. In the near ocean surface, the ocean releases latent heat, while the atmosphere mainly absorbs latent heat. In the upper troposphere, the atmosphere mainly releases latent heat.