1) characteristic steepness
特征波陡
2) 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。
3) 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
4) steep ridge geography characteristic line
陡坎类地貌特征线
5) characteristic harmonic
特征谐波
1.
Improvement of characteristic harmonic method in rotational arc sensor
旋转电弧传感器特征谐波法的改进
2.
The method of identifying signals of the seam deviation by the characteristic harmonic detection method is expounded.
介绍了该传感器的结构与工作原理,阐述了采用特征谐波检测法识别焊缝偏差信号的方法。
6) characteristic wave
特征波
1.
The derivation of eigenvalue problem for characteristic wave number is carried out based on Maxwell equations.
由麦克斯韦方程导出关于特征波的本征值问题,令本征矩阵的行列式为零,得到含参量的四次方程。
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