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一、引言近年来,国内外在利用气象卫星观测资料监测和研究台风的生命史、移动路径、影响范围和外观结构等方面获得了极大成功。卫星的连续观测,为我们进一步揭示现象的物理机制提供了可靠的资料和证据。尤其在实测资料稀少的大洋区和灾害性天气系统到来之即,卫星资料就显得更为可贵。在台风外观结构的研究中,Hadbook和Hess、张捷迁和魏鼎文用不同媒介物在实验室内进行了各种不同条件下的模拟实验,得到了详尽的各层(上、中、下层)温度
I. INTRODUCTION In recent years, great success has been achieved at home and abroad in using meteorological satellite observations to monitor and study the life history, movement paths, influence ranges and appearance structures of typhoons. The continuous observation of satellites provides reliable data and evidences for us to further reveal the physical mechanism of the phenomenon. In particular, satellite data become even more valuable as the real-world, disastrous oceanic data and disastrous weather systems arrive. In the study of the appearance structure of the typhoon, Hadbook and Hess, Zhang Jieqian, and Wei Dingwen performed various experiments under different conditions in the laboratory with different media, and exhaustive temperature (upper, middle and lower layers)