Abstract
During integration both vortices develop to become TCs with the structure closely resembling that of actual TCs. The development and motion of two TCs with and without incorporation of the ocean model are shown to differ greatly. Studied are the fields of pressure, relative vorticity, vertical motions, and ocean surface temperatures in different experiments. -from Journal summary
| Original language | English |
|---|---|
| Pages (from-to) | 33-40 |
| Number of pages | 8 |
| Journal | Russian Meteorology and Hydrology |
| Volume | 7 |
| State | Published - 1993 |
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