MLchartDataset catalogue

Viscous-convective subrange

Term · Meteorology and atmospheric science · MLC-T-MET-010034

A range of spatial scales in a turbulent fluid where the dissipation of temperature variance is caused by both molecular viscosity and thermal diffusivity. This subrange lies at the small-scale end of the inertial-convective subrange, just before the scales where viscous effects completely dominate thermal effects. The Batchelor scale, which characterizes the smallest eddies of a scalar field before it is smoothed out by molecular diffusion, marks the lower boundary of this subrange.

Table 1. Record
IdentifierMLC-T-MET-010034
FieldMeteorology and atmospheric science
Record as JSON
{
  "id": "MLC-T-MET-010034",
  "term": "Viscous-convective subrange",
  "field": "Meteorology and atmospheric science",
  "definition": "A range of spatial scales in a turbulent fluid where the dissipation of temperature variance is caused by both molecular viscosity and thermal diffusivity. This subrange lies at the small-scale end of the inertial-convective subrange, just before the scales where viscous effects completely dominate thermal effects. The Batchelor scale, which characterizes the smallest eddies of a scalar field before it is smoothed out by molecular diffusion, marks the lower boundary of this subrange.",
  "url": "https://mlchart.com/terminology/meteorology/viscous-convective-subrange/"
}

Record 10,317 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.