MLchartDataset catalogue

Thermal internal boundary layer

Term · Meteorology and atmospheric science · MLC-T-MET-009585

A layer of air that forms downwind from a coastline or other sharp change in surface temperature, where the air mass transitions from one thermal regime to another. It develops as cooler air moves over a warmer surface, or vice versa, leading to changes in atmospheric stability and mixing. The height of this boundary layer typically increases with distance downwind from the thermal discontinuity.

Table 1. Record
IdentifierMLC-T-MET-009585
FieldMeteorology and atmospheric science
Record as JSON
{
  "id": "MLC-T-MET-009585",
  "term": "Thermal internal boundary layer",
  "field": "Meteorology and atmospheric science",
  "definition": "A layer of air that forms downwind from a coastline or other sharp change in surface temperature, where the air mass transitions from one thermal regime to another. It develops as cooler air moves over a warmer surface, or vice versa, leading to changes in atmospheric stability and mixing. The height of this boundary layer typically increases with distance downwind from the thermal discontinuity.",
  "url": "https://mlchart.com/terminology/meteorology/thermal-internal-boundary-layer/"
}

Record 9,637 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.