MLchartDataset catalogue

Slope flow

Term · Meteorology and atmospheric science · MLC-T-MET-008939

A localized wind system driven by differential heating or cooling of a sloping terrain, causing air to move up or down the incline. During the day, solar heating of the slope can create an upslope flow (anabatic wind), while nighttime cooling leads to a downslope flow (katabatic wind). These flows are common in mountainous regions and can influence local weather patterns.

Table 1. Record
IdentifierMLC-T-MET-008939
FieldMeteorology and atmospheric science
Record as JSON
{
  "id": "MLC-T-MET-008939",
  "term": "Slope flow",
  "field": "Meteorology and atmospheric science",
  "definition": "A localized wind system driven by differential heating or cooling of a sloping terrain, causing air to move up or down the incline. During the day, solar heating of the slope can create an upslope flow (anabatic wind), while nighttime cooling leads to a downslope flow (katabatic wind). These flows are common in mountainous regions and can influence local weather patterns.",
  "url": "https://mlchart.com/terminology/meteorology/slope-flow/"
}

Record 8,671 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.