End of storm oscillation
Term · Meteorology and atmospheric science · MLC-T-MET-005365
A distinct, final fluctuation in atmospheric pressure that occurs as a thunderstorm moves away from an observation point. This feature appears on a barograph trace as a sharp pressure drop followed by a rapid recovery, creating a V-shaped signature. The oscillation is associated with the wake low that forms to the rear of the storm's main precipitation area, marking the passage of the complete storm system.
| Identifier | MLC-T-MET-005365 |
|---|---|
| Field | Meteorology and atmospheric science |
| Abbreviation | EOSO |
Record as JSON
{
"id": "MLC-T-MET-005365",
"term": "End of storm oscillation",
"field": "Meteorology and atmospheric science",
"definition": "A distinct, final fluctuation in atmospheric pressure that occurs as a thunderstorm moves away from an observation point. This feature appears on a barograph trace as a sharp pressure drop followed by a rapid recovery, creating a V-shaped signature. The oscillation is associated with the wake low that forms to the rear of the storm's main precipitation area, marking the passage of the complete storm system.",
"abbreviation": "EOSO",
"url": "https://mlchart.com/terminology/meteorology/end-of-storm-oscillation/"
}
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