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Pressure, velocity, and temperature do change across a shock front. I think a
shock is, by definition, a discontinuity. The changes are described by a set of
"jump conditions" called the Rankine-Hugoniot equations. Each equation can be
expressed in terms of the adiabatic gas constant (gamma) and M1, the Mach number
for the gas behind the shock front.
Pressure: P2 / P1 = 1 + [2*gamma*(M1^2 - 1) / (gamma + 1)]
Density: rho2 / rho1 = [1 + ((gamma + 1)/(gamma - 1))*P2/P1] / [((gamma + 1) /
(gamma - 1)) + P2/P1]
Temperature: T2 / T1 = (P2 / P1)[((gamma + 1)/(gamma - 1)) + (P2/P1)] / [1 +
((gamma + 1) / (gamma - 1))*P2/P1]