非线性海洋内波的理论、模型与计算1)
王展*†2)(
),朱玉可**
),朱玉可**
THEORY, MODELLING AND COMPUTATION OF NONLINEAR OCEAN INTERNAL WAVES1)
Wang Zhan*†2)(),Zhu Yuke**
),Zhu Yuke**
图3. 中国南海观测到的大振幅内孤立波. 水平坐标表示时间, 每隔1 min采样一次; 垂直坐标表示海洋深度(总深度约为340 m)
Fig.3. A large-amplitude internal solitary wave observed in the South China Sea. The horizontal coordinate represents the time, sampling every 1 min, and the vertical coordinate indicates the depth of the ocean (the total depth is about 340 m)
