Abstract
The dynamics of tropical cyclone motion are investigated by solving for instantaneous motion tendencies using the divergent barotropic vorticity equation on a beta plane. Two methods of solution are presented: a direct analytic solution for a constant basic current, and simple numerical solution for more general conditions.-from Author
| Original language | English |
|---|---|
| Pages (from-to) | 328-342 |
| Number of pages | 15 |
| Journal | Journal of the Atmospheric Sciences |
| Volume | 40 |
| Issue number | 2 |
| DOIs | |
| State | Published - 1983 |
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