Abstract
The analytic predictions of tropical cyclone motion by Holland are shown to be in very good agreement with observations in the Australian/southwest Pacific region. These results indicate that a combined linear asymmetric advection and divergence of earth and cyclone vorticity provides the main mechanism for tropical cyclone motion. It is also shown that an accurate prediction requires a consideration of horizontal and vertical asymmetries in the wind field. -from Author
| Original language | English |
|---|---|
| Pages (from-to) | 68-75 |
| Number of pages | 8 |
| Journal | Journal of the Atmospheric Sciences |
| Volume | 41 |
| Issue number | 1 |
| DOIs | |
| State | Published - 1984 |