LP Storm
Term · Meteorology and atmospheric science · MLC-T-MET-001590
Low-Precipitation storm (or Low-Precipitation supercell). A
supercell thunderstorm characterized by a relative lack of visible precipitation. Visually similar to a
classic supercell, except without the heavy precipitation core. LP storms often exhibit a
striking visual appearance; the main tower often is bell-shaped, with a corkscrew appearance
suggesting rotation. They are capable of producing tornadoes and very large hail. Radar
identification often is difficult relative to other types of supercells, so visual reports are very
important. LP storms almost always occur on or near the dry line, and thus are sometimes referred
to as dry line storms.
| Identifier | MLC-T-MET-001590 |
|---|---|
| Field | Meteorology and atmospheric science |
| References | NWS Glossary |
Record as JSON
{
"id": "MLC-T-MET-001590",
"term": "LP Storm",
"field": "Meteorology and atmospheric science",
"definition": "Low-Precipitation storm (or Low-Precipitation supercell). A\nsupercell thunderstorm characterized by a relative lack of visible precipitation. Visually similar to a\nclassic supercell, except without the heavy precipitation core. LP storms often exhibit a\nstriking visual appearance; the main tower often is bell-shaped, with a corkscrew appearance\nsuggesting rotation. They are capable of producing tornadoes and very large hail. Radar\nidentification often is difficult relative to other types of supercells, so visual reports are very\nimportant. LP storms almost always occur on or near the dry line, and thus are sometimes referred\nto as dry line storms.",
"references": [
"NWS Glossary"
],
"url": "https://mlchart.com/terminology/meteorology/lp-storm/"
}
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