Abstract
A potential vorticity mechanism for sub-tropical cyclogenesis (STCG) and tropical transition was discussed. The first stage of STCG is identified with the intensification of pre-existing lower and upper PV anomalies by baroclinic instability. In the second stage, the amplified upper trough PV anomaly becomes cut off from the mean flow, via Rossby wave-breaking. In the third stage these cut-off features become embedded in a region of much greatly reduced of negligible vertical shear.
| Original language | English (US) |
|---|---|
| Pages | 411-412 |
| Number of pages | 2 |
| State | Published - 2004 |
| Event | 26th Conference on Hurricanes and Tropical Meteorolgy - Miami, FL., United States Duration: May 3 2004 → May 7 2004 |
Other
| Other | 26th Conference on Hurricanes and Tropical Meteorolgy |
|---|---|
| Country/Territory | United States |
| City | Miami, FL. |
| Period | 5/3/04 → 5/7/04 |
All Science Journal Classification (ASJC) codes
- General Engineering
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