MLchartDataset catalogue

Holmboe instability

Term · Meteorology and atmospheric science · MLC-T-MET-006262

A type of hydrodynamic instability that occurs in a continuously stratified fluid with a shear flow, characterized by the presence of two critical levels where the fluid velocity matches the phase speed of a wave. This instability can lead to the growth of internal gravity waves and turbulence. It is relevant to atmospheric and oceanic flows where density stratification and velocity shear coexist.

Table 1. Record
IdentifierMLC-T-MET-006262
FieldMeteorology and atmospheric science
Record as JSON
{
  "id": "MLC-T-MET-006262",
  "term": "Holmboe instability",
  "field": "Meteorology and atmospheric science",
  "definition": "A type of hydrodynamic instability that occurs in a continuously stratified fluid with a shear flow, characterized by the presence of two critical levels where the fluid velocity matches the phase speed of a wave. This instability can lead to the growth of internal gravity waves and turbulence. It is relevant to atmospheric and oceanic flows where density stratification and velocity shear coexist.",
  "url": "https://mlchart.com/terminology/meteorology/holmboe-instability/"
}

Record 4,553 of 10,756 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.