Rain Induced Fog
Term · Meteorology and atmospheric science · MLC-T-MET-002247
When warm rain falls through cooler air, water evaporates from the warm rain. It subsequently condenses in the cool air forming fog. Such fog can be quite dense. It generally will persist as long as the rain continues. Since temperature rises little during the day, there is little diurnal variation in rain induced fog. Improvement in visibility cannot be expected until the rain stops or moves out of the affected area.
| Identifier | MLC-T-MET-002247 |
|---|---|
| Field | Meteorology and atmospheric science |
| References | NWS Glossary |
Record as JSON
{
"id": "MLC-T-MET-002247",
"term": "Rain Induced Fog",
"field": "Meteorology and atmospheric science",
"definition": "When warm rain falls through cooler air, water evaporates from the warm rain. It subsequently condenses in the cool air forming fog. Such fog can be quite dense. It generally will persist as long as the rain continues. Since temperature rises little during the day, there is little diurnal variation in rain induced fog. Improvement in visibility cannot be expected until the rain stops or moves out of the affected area.",
"references": [
"NWS Glossary"
],
"url": "https://mlchart.com/terminology/meteorology/rain-induced-fog/"
}
Record 2,246 of 3,164 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.