MLchartDataset catalogue

Vorticity advection

Term · Meteorology and atmospheric science · MLC-T-MET-010069

The transport of vorticity by the horizontal wind field. This process is a primary mechanism for forcing vertical motion in the atmosphere, with positive vorticity advection (PVA) leading to upward motion and negative vorticity advection (NVA) causing subsidence. In the Northern Hemisphere, PVA is maximized downstream of a trough axis in the jet stream, contributing to surface cyclogenesis and precipitation.

Table 1. Record
IdentifierMLC-T-MET-010069
FieldMeteorology and atmospheric science
See alsoOmega equation
Record as JSON
{
  "id": "MLC-T-MET-010069",
  "term": "Vorticity advection",
  "field": "Meteorology and atmospheric science",
  "definition": "The transport of vorticity by the horizontal wind field. This process is a primary mechanism for forcing vertical motion in the atmosphere, with positive vorticity advection (PVA) leading to upward motion and negative vorticity advection (NVA) causing subsidence. In the Northern Hemisphere, PVA is maximized downstream of a trough axis in the jet stream, contributing to surface cyclogenesis and precipitation.",
  "see_also": [
    "omega equation"
  ],
  "url": "https://mlchart.com/terminology/meteorology/vorticity-advection/"
}

Record 10,368 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.