1) significant slope
有效波陡
2) effective steepness
有效陡度
3) wave steepness
波陡
1.
As a remedy,based upon the concepts of existence of wave steepness and limitation of wave energy density,two modification methods are proposed.
线性兴波理论用于计算实际船型阻力时偏差较大，本文基于有限波陡和波能密度限制，探讨对该理论的解释，提出两种修正方法对Ｗｉｇｌｅｙ船型和系列６０的三个船型的兴波阻力系数进行计算，结果与船模试验剩余阻力相符较好
2.
It reduces the excess phase speed overprediction of both Hedges modified relation and Kirby and Dalrymple s modified relation in the region of 1<kh<15 for small wave steepness and maintains the monotonicity in phase speed variation for large wave steepness.
针对Hedges及Kirby等对Kirby和Dalrymple的非线性弥散关系的修正关系,在小波陡时中等水深范围存在较大偏差的问题,给出了一个新的非线性弥散关系。
4) Steep Wave
陡波
1.
Numerical Simulation of Steep Waves Based on New Wave Theory;
基于新波理论的陡波数值模拟
5) filtering gradient
滤波陡波
6) effective wave
有效波
1.
The theory of optimized array filtering is advanced to cope with the multi-channel seismic data which include effective wave and coherent noise.
最优化列阵滤波理论是针对一级包含有效波和相干干扰波的多道记录信号而提出的。
补充资料：立陡陡
1.直立貌。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条