1) baroclinic gravity wave
斜压重力波
1.
Therefore the baroclinic gravity wave phase speed C n and corresp.
根据南海 1°× 1°网格的标准层季节平均温、盐度资料 ,在未引入Boussinesq近似条件下 ,采用改进的Thompson Haskell算法求解线性化斜压海洋水平大尺度波的垂直结构方程 (重力内波方程 ) ,从而得到了南海各网格点的第一斜压重力波相速度和相应的罗斯贝变形半径 ,并探讨其地理分布和季节变化特征 ,以期有助于南海环流和中尺度涡旋以及有关海洋侧边界效应的研究。
2) baroclinic waves thermal structure
斜压波热力结构
3) baroclinic wave packets
斜压波包
1.
Using NCEP/NCAR reanalysis data and diagnosis of local kinetic energy and 3-dimensional quasi-geostrophic wave-activity fluxes,the author carried out a case study of baroclinic wave packets in the northern hemisphere summer season of 2002.
利用NCEP/NCAR再分析资料,使用局地能量诊断和三维准地转波动通量等工具分析了2002年北半球夏季的一次斜压波包过程。
2.
Using Hilbert transform and NCEP/NCAR reanalysis data, the authors analyze the structures and nature of the long life-cycle baroclinic wave packets in the Southern Hemisphere.
利用Hillbert变换和NCEP/NCAR再分析资料,研究南半球夏季长生命期的斜压波包的结构和传播特征。
3.
hPa meridional wind data from a GCM experiment run at GFDL of Princeton University was analyzed to document the characteristics of the baroclinic wave packets in GCM data.
斜压波包的波长为数千公里 ,相速为 10m s左右。
4) baroclinic waves
斜压波动
1.
Our results have demonstrated that the baroclinic waves in upper troposphere organize into the Rossby wave packets during the Meiyu period of 1998 and disperse to their downstream area distinctly.
结果表明,梅雨期间的高频斜压波动(周期≤7天)具有明显的下游频散效应,在其东传过程中常组织成局地波包向下游传播。
5) baroclinic solenoid
斜压力管
6) barodine force
斜张压力
补充资料：冲击波超压与动压