MLchartDataset catalogue

Inertial subrange

Term · Meteorology and atmospheric science · MLC-T-MET-006527

A specific portion of the inertial range in turbulent flows where the energy cascade from large to small scales is dominant, and viscous dissipation is negligible. In this subrange, the kinetic energy spectrum typically follows the Kolmogorov -5/3 power law. It is characterized by a balance between inertial forces and the transfer of energy across different eddy sizes.

Table 1. Record
IdentifierMLC-T-MET-006527
FieldMeteorology and atmospheric science
See alsoSpectral gap; Kolmogorov's similarity hypotheses
Record as JSON
{
  "id": "MLC-T-MET-006527",
  "term": "Inertial subrange",
  "field": "Meteorology and atmospheric science",
  "definition": "A specific portion of the inertial range in turbulent flows where the energy cascade from large to small scales is dominant, and viscous dissipation is negligible. In this subrange, the kinetic energy spectrum typically follows the Kolmogorov -5/3 power law. It is characterized by a balance between inertial forces and the transfer of energy across different eddy sizes.",
  "see_also": [
    "spectral gap",
    "Kolmogorov's similarity hypotheses"
  ],
  "url": "https://mlchart.com/terminology/meteorology/inertial-subrange/"
}

Record 4,948 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.