Théorie analytique de la chaleur¶
Boussinesq, J. (1903). Théorie analytique de la chaleur.
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Primes¶
- Convection
- Fluid medium. A fluid (liquid, gas, partially molten rock, plasma) capable of flowing coherently over the scales of interest. Density gradient. A spatial density contrast exists, typically arising from temperature gradients (thermal convection) or compositional gradients (double-diffusive or compositional convection). Buoyancy force exceeds stabilizing resistance. The
This sourceIntroduces the Boussinesq approximation: density variations are neglected throughout the equations of motion except where they are multiplied by gravity in the buoyancy term, yielding a quasi-incompressible system in which buoyancy is the driving force.
- Fluid medium. A fluid (liquid, gas, partially molten rock, plasma) capable of flowing coherently over the scales of interest. Density gradient. A spatial density contrast exists, typically arising from temperature gradients (thermal convection) or compositional gradients (double-diffusive or compositional convection). Buoyancy force exceeds stabilizing resistance. The
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