Weather Prediction by Numerical Process¶
Richardson, L. F. (1922). Weather Prediction by Numerical Process. Cambridge University Press.
Cited by¶
1 citation across 1 artifact.
Each citation links to the sentence it supports in the citing article.
Primes¶
- Turbulence
- . Multi-scale structure. Eddies exist at a broad range of sizes, from the integral scale (set by the geometry or forcing) down to the dissipation scale (set by viscosity and energy-dissipation rate). Energy cascade. Kinetic energy is injected at the large scales, transferred down through the inertial range via nonlinear eddy interactions, and dissipated as heat at the smallest scales.
This sourceProposes the energy-cascade concept in turbulence: "Big whorls have little whorls that feed on their velocity, and little whorls have lesser whorls and so on to viscosity in the molecular viscosity range"; founds the Richardson cascade cascade of eddy sizes.
Supported in partVerified against the work's full text
Richardson's book treats eddying kinetic energy across eddy scales and its molecular dissipation as heat, backing the cascade frame but not the 'inertial range' clause.
“Let the kinetic energy of eddies be @ per mass of atmosphere, then from considera- tions of energy it has been deduced (L. F. Richardson (33), p. 354)* that where the integrals are taken over an atmospheric block so large that we may neglect the eddying energy traversing its boundaries. In the first member I is the linear dimension of a " typical " eddy, K is the molecular viscosity.”
- . Multi-scale structure. Eddies exist at a broad range of sizes, from the integral scale (set by the geometry or forcing) down to the dissipation scale (set by viscosity and energy-dissipation rate). Energy cascade. Kinetic energy is injected at the large scales, transferred down through the inertial range via nonlinear eddy interactions, and dissipated as heat at the smallest scales.
Verification¶
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Registry ID ref:aab24285c6d9 · see in the full table