Abstract
The Tropical Cyclone Reports states that the development of nearly half of the Atlantic tropical cyclones from 2000 to 2003 depended on an extratropical precursors. A fundamental dynamic and thermodynamic transformation of such disturbance is required to create a warm-core tropical cyclone. The process is referred to as tropical transition (TT), to be contrasted with extratropical transition (ET), which results in an extratropical disturbance given a tropical cyclone. Focusing on the Atlantic basin, this paper reviews briefly what is known about TT and how it can be anticipated. While TT storms typically do not exceed Category 2 intensity, their tendency to form close to North America can create significant forecast and evacuation problems.
| Original language | English |
|---|---|
| Pages (from-to) | 1657-1662 |
| Number of pages | 6 |
| Journal | Bulletin of the American Meteorological Society |
| Volume | 85 |
| Issue number | 11 |
| DOIs | |
| State | Published - Nov 2004 |
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