Cold high
Term · Meteorology and atmospheric science · MLC-T-MET-004497
A high-pressure system characterized by a cold air mass extending through a deep layer of the troposphere. The high pressure at the surface is primarily due to the density of the cold air. These systems are common over continental interiors during winter, bringing clear skies and very low temperatures.
| Identifier | MLC-T-MET-004497 |
|---|---|
| Field | Meteorology and atmospheric science |
| Synonyms | cold anticyclone; cold-core high; cold-core anticyclone |
| See also | Thermal high |
Record as JSON
{
"id": "MLC-T-MET-004497",
"term": "Cold high",
"field": "Meteorology and atmospheric science",
"definition": "A high-pressure system characterized by a cold air mass extending through a deep layer of the troposphere. The high pressure at the surface is primarily due to the density of the cold air. These systems are common over continental interiors during winter, bringing clear skies and very low temperatures.",
"synonyms": [
"cold anticyclone",
"cold-core high",
"cold-core anticyclone"
],
"see_also": [
"thermal high"
],
"url": "https://mlchart.com/terminology/meteorology/cold-high/"
}
Record 1,950 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.