1) divergently excurrent layer
辐散流出层
1.
Combining the Lagrange description method in particle dynamics with the Euler description method used in fluid dynamics, this paper has set up the unique twodimension differential equation set which describes the Coriolis rotational flow of the divergently excurrent layer in the top of typhoon.
本文把质点动力学的Lagrange表述法和流体力学惯用的Euler表述法结合起来,建立了描述台风顶部辐散流出层Coriolis旋流的独特的二维微分方程组。
2) non-divergent level
无辐散层
3) Divergent circulation
辐散环流
1.
The present paper gives an analysis of the low frequency (LF) vortex and divergent circulation systems and their interactions in terms of the ECMWF/WMO data (summer of 1984).
利用1984年夏季ECMWF/WMO资料分析了低频涡度系统和低频辐散环流系统,讨论了两者之间的相互作用。
4) nondivergent flow
非辐散流
5) storm-top divergence
高层强辐散
6) divergence to the right of the exit region
出口处右侧辐散
补充资料：散逸层
| 散逸层 见外逸层。 |
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