MLchartDataset catalogue

Local isotropy

Term · Meteorology and atmospheric science · MLC-T-MET-007013

A concept in turbulence theory stating that at sufficiently small scales, turbulent eddies become statistically isotropic, meaning their properties are independent of direction. This implies that the smallest eddies are primarily responsible for dissipating kinetic energy into heat, regardless of the direction of the larger-scale flow. The Kolmogorov microscale defines the approximate size below which this isotropy holds.

Table 1. Record
IdentifierMLC-T-MET-007013
FieldMeteorology and atmospheric science
See alsoIsotropic turbulence
Record as JSON
{
  "id": "MLC-T-MET-007013",
  "term": "Local isotropy",
  "field": "Meteorology and atmospheric science",
  "definition": "A concept in turbulence theory stating that at sufficiently small scales, turbulent eddies become statistically isotropic, meaning their properties are independent of direction. This implies that the smallest eddies are primarily responsible for dissipating kinetic energy into heat, regardless of the direction of the larger-scale flow. The Kolmogorov microscale defines the approximate size below which this isotropy holds.",
  "see_also": [
    "isotropic turbulence"
  ],
  "url": "https://mlchart.com/terminology/meteorology/local-isotropy/"
}

Record 5,649 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.