Nonlinear acoustics and shock dynamics in isentropic atmospheres

TL;DR

This paper develops exact simple-wave solutions for nonlinear acoustic waves in stratified atmospheres, enabling analytical discrimination of shock formation and reflection, validated by hydrodynamic simulations.

Contribution

It introduces a novel analytical framework using simple-wave solutions to describe nonlinear wave and shock evolution in stratified atmospheres, bridging the gap between low amplitude and strong shock regimes.

Findings

Analytical solutions accurately predict shock formation up to Mach 15.

Wave reflection and shock evolution are described explicitly for specific adiabatic indices.

Subsonic pulses cannot unbind atmospheric mass without entropy increase.

Abstract

Nonlinear acoustic evolution is often discussed in the context of wave-steepening that leads to shock formation, and is of special interest in applications where the shock continues to strengthen due to a narrowing of its channel or the stratification of the medium. Accurate scalings govern low amplitude waves and strong shocks, but connecting these phases, or describing waves that are nonlinear from the outset, generally requires simulation. We address this problem using the fact that waves within a plane-parallel, isentropic and gravitationally stratified atmosphere are described by exact simple-wave solutions, thanks to the conservation of Riemann invariants in a freely falling reference frame. Our solutions enable us to discriminate waves that reflect from those that form shocks, and to capture wave and shock evolution using an ordinary differential equation. For several relevant values of the adiabatic index $\gamma$ the solutions are explicit; furthermore, nonlinear wave reflection from a free surface can be described analytically for $\gamma=3$. Comparison to hydrodynamic simulations shows that our analytic shock approximation is accurate up to moderate ($\sim$ few--15) Mach numbers, where the accuracy increases with the adiabatic index. Our solutions also imply that an initially subsonic pulse is unable to unbind mass from the atmosphere without significantly increasing its entropy.