'Du dt' diaporamas de présentation

Ch. 11: Introduction to Compressible Flow

Ch. 11: Introduction to Compressible Flow. Focus on 1-dimensional, compressible, inviscid flows. Liquids, ? = constant for us (1% increase in ? for every 1.6 km deep). Air, 1% change for every 26 m deep. M = 0.3 ~ 5% = ??/?; M = 0.3 ~ 100 m/s or 230 mph.

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Secondary effects on output side of VSD and mitigation methods

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Criteria for Spontaneity

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Field energy in a dispersive medium

Field energy in a dispersive medium. Section 80. Review energy in non-dispersive dielectrics. U = internal energy difference for body with and without fields, holding entropy and density constant. Dispersive media dissipate energy. Mean evolved heat density per unit time Q = <- div S > t

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Day 4 Differential Equations (option chapter)

Day 4 Differential Equations (option chapter). Recall from AP Calculus. The number of rabbits in a population increases at a rate that is proportional to the number of rabbits present (at least for awhile.).

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What Is a Numerical Weather Prediction Model?

What Is a Numerical Weather Prediction Model?. Seek relationships (equations) between variables you want to know (e.g. - v, T, p, z, q) and the forcing mechanisms that cause changes in these variables. Example:. Presented by Fred Carr COMAP Symposium 00-1. In meteorology, we solve for Du/Dt

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