1) storm-top divergence
高层强辐散
2) divergence intensity
辐散强度
3) Upper-level mesoscale divergence area
高层中尺度辐散区
4) non-divergent level
无辐散层
6) 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。
补充资料:椐椐强强
1.相随貌。
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