MLchartDataset catalogue

Ekman pumping

Term · Meteorology and atmospheric science · MLC-T-MET-005299

The vertical motion of water or air induced by the divergence or convergence of Ekman transport within the boundary layer. When Ekman transport diverges, water or air is drawn up from below (upwelling), and when it converges, fluid is pushed downwards (downwelling). This process is a key mechanism for nutrient upwelling in coastal ocean regions and for driving vertical motion in atmospheric boundary layers.

Table 1. Record
IdentifierMLC-T-MET-005299
FieldMeteorology and atmospheric science
Record as JSON
{
  "id": "MLC-T-MET-005299",
  "term": "Ekman pumping",
  "field": "Meteorology and atmospheric science",
  "definition": "The vertical motion of water or air induced by the divergence or convergence of Ekman transport within the boundary layer. When Ekman transport diverges, water or air is drawn up from below (upwelling), and when it converges, fluid is pushed downwards (downwelling). This process is a key mechanism for nutrient upwelling in coastal ocean regions and for driving vertical motion in atmospheric boundary layers.",
  "url": "https://mlchart.com/terminology/meteorology/ekman-pumping/"
}

Record 3,071 of 10,702 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.