1) barotropic tide
正压潮
1.
Based on a 1/30° resolution,three dimensional POM (Princeton Ocean Model) with boundary conditions of four main constituents M2,S2 K1 and O1,barotropic tide in the northwestern South China Sea is simulated and the distribution characteristics of its energy flux in Qiongzhou Strait (QS) and its adjacent region is analyzed.
5-115°E,16-23°N)海域正压潮,分析琼州海峡及其附近区域正压潮能通量分布特征。
2) barotropic tidal current
正压潮流
1.
The impact of barotropic tidal current on internal wave mode st
分析正压潮流对内波模态结构函数? ( z),GK-dV方程非线性系数α、频散系数β、长内波相速度c,内孤立波振幅和波形的影响。
2.
The impact of barotropic tidal current on internal wave mode structure function φ(z),the nonlinearity coefficient α and the dispersion coefficient β of GK-dV equation,the phase speed c of long internal waves, as well as the amplitude and shape of internal solitary waves are considered.
分析正压潮流对内波模态结构函数φ(z),GK-dV方程非线性系数α、频散系数β、长内波相速度c、内孤立波振幅和波形的影响。
3) ATMDISP
大气压负荷非潮汐改正
6) tide rectification
潮位改正
补充资料：大气压
又称“大气压强”，简称“气压”。与大气接触的面上所受到的气体分子的压强。单位用百帕表示。随高度升高而降低，如高山顶上的大气压比山脚下要低。在同一高度的大气压，气温低，密度大，大气压就高；反之，大气压就低。
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