Gradient transport theory

{
  "id": "MLC-T-MET-006019",
  "term": "Gradient transport theory",
  "field": "Meteorology and atmospheric science",
  "definition": "A conceptual framework that describes the transport of atmospheric properties, such as heat, momentum, and moisture, as being proportional to their respective gradients. This theory assumes that fluxes occur down the gradient, from regions of higher concentration to lower concentration. It is a simplification often used in atmospheric models, particularly in the planetary boundary layer.",
  "see_also": [
    "higher-order closure",
    "nonlocal closure",
    "transilient turbulence theory"
  ],
  "url": "https://mlchart.com/terminology/meteorology/gradient-transport-theory/"
}