Divergence theory of cyclones
Term · Meteorology and atmospheric science · MLC-T-MET-005087
A meteorological theory explaining the formation and intensification of extratropical cyclones through the concept of upper-level divergence. It posits that regions of upper-level divergence, often associated with troughs in the jet stream, lead to upward motion and a decrease in surface pressure, fostering cyclogenesis. This theory highlights the dynamic coupling between upper and lower atmospheric levels in storm development.
| Identifier | MLC-T-MET-005087 |
|---|---|
| Field | Meteorology and atmospheric science |
Record as JSON
{
"id": "MLC-T-MET-005087",
"term": "Divergence theory of cyclones",
"field": "Meteorology and atmospheric science",
"definition": "A meteorological theory explaining the formation and intensification of extratropical cyclones through the concept of upper-level divergence. It posits that regions of upper-level divergence, often associated with troughs in the jet stream, lead to upward motion and a decrease in surface pressure, fostering cyclogenesis. This theory highlights the dynamic coupling between upper and lower atmospheric levels in storm development.",
"url": "https://mlchart.com/terminology/meteorology/divergence-theory-of-cyclones/"
}
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