浅水波是指当水深与波长的比值较小时,水底边界影响水质点运动的波浪。它在传播过程中,波高 、波长 、波速等随水深的变化而变化;当波峰线与等深线不平行时,将发生波浪折射现象,波向也随之改变。浅水前进波和浅水立波都属于它的范畴。
潮流场计算是基于浅水波理论。
The shallow water wave theory is employed in the description of tidal flows.
利用浅水波正压模式研究了环境流场切应变率对台风移动的影响。
The role of shear strain rate of an environmental flow in typhoon propagation is investigated using a shallow water model.
分别从连续的、离散的非线性二维浅水波模式,建立其伴随模式。
The adjoint models are derived from continuous and discrete two dimension shallow-water models.
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