上层海洋对台风的响应和调制机理
陈大可1, 雷小途2, 王伟3, 王桂华1, 韩桂军4, 周磊1

Upper Ocean Response and Feedback Mechanisms to Typhoon
Chen Dake1, Lei Xiaotu2, Wang Wei3, Wang Guihua1, Han Guijun4, Zhou Lei1
图2 2003年“鸣蝉”台风经过西太平洋暖涡时从一级到超级台风的强化过程 黑色直线为高度计轨道；等值线为海表高度异常（单位：cm）；左下角图标表示台风等级, 从TD到H5逐渐增强
Fig.2 Process through which the Typhoon Maemi intensified from grade 1 to a super typhoon Black lines mark the altimeter tracks; Contours show the sea surface height anomalies unit:cm； The legend at the lower left corner shows the strength of typhoon, increasing from TD to H5