Physics · waves

Speed of Sound & Mach Cone

How fast sound travels up there, the cone a supersonic body drags behind it, and when — or whether — the boom reaches the ground.
sin μ = 1/M
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Flight

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The air

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Offset from the standard atmosphere at every height, as pilots quote it: ISA+15 is a hot day.

The wavefronts, and the cone they make

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sound on · heard from 300 m
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Where the boom lands — and where it turns back

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Sound is faster in warm air, and the air is warmest near the ground. A body only a little faster than the sound around it at altitude can be slower than the sound near the ground — and then its shock bends back upward before it lands. The shaded band is where the body outruns the sound.

Every gas has its own speed of sound

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The geometry

Why the cone has exactly the angle it has

A moving body sends out sound in every direction, all the time, and each burst spreads as a circle at the speed of sound from wherever the body was. Slower than sound, the body stays inside its own circles: they crowd together ahead of it and spread out behind — the Doppler effect, and the reason a passing car's note drops. At exactly the speed of sound every circle touches the same point, the nose, and the pressure piles up into a wall. Faster than that, the body leaves its circles behind, and all of them are tangent to one cone.

The angle falls out in one line

In a time t the body travels vt and its first circle grows to a radius of at. The cone's edge is the tangent from the body to that circle, so sin μ = at/vt = 1/M. At Mach 2 the half-angle is 30°; at Mach 1.1 it is 65°, nearly flat; a rifle bullet at Mach 2.7 drags a cone 22° either side of its path.

A sonic boom is not an event that happens when something "breaks the barrier". It is that cone sweeping over you, and it sweeps over everyone along the whole route for as long as the flight stays supersonic. What you hear is two cracks a fraction of a second apart — one from the bow shock, one from the tail — because the pressure jumps up, falls through ambient, and jumps back: an N-wave.

The part people get wrong

Sound speed follows temperature, not pressure

It is tempting to think sound is slower in thin air. It is slower up there, but not because the air is thin. In an ideal gas the speed of sound is √(γRT/M): temperature, and what the gas is made of. Pressure cancels out entirely, because thinner air is also lighter air, and the two effects are exactly equal. The stratosphere is slow because it is −56.5 °C, and above 20 km, where it warms again, sound speeds up again.

What that does to "Mach 2"

Mach number is a ratio, not a speed. Mach 2 at sea level on a standard day is 681 m/s; at 11 km it is 590 m/s, thirteen per cent slower through the air for the same number. Aircraft limits are quoted in Mach high up precisely because it is the ratio, not the speed, that decides how the air behaves around the wing.

Why do some supersonic flights make no boom on the ground at all?

Because sound bends towards the slower air, and the air near the ground is warmer and faster. Follow the shock downward: its angle to the horizon shrinks as the sound around it speeds up, and if it reaches a height where the local speed of sound matches the body's speed, it is travelling horizontally — and then it bends back up. That is Mach cutoff. At 11 km on a standard day it happens below about Mach 1.15, which is the whole idea behind quiet supersonic flight over land: go fast, but not so fast that the ground can hear.

Is the boom only when the plane breaks the sound barrier?

No. The cone exists the whole time the body is supersonic, so a boom is heard along the entire route, by everyone the cone sweeps across. The barrier crossing itself is not special on the ground; what is special is that the cone first exists then.

Why does the pitch drop as a car goes past?

Ahead of a moving source the wavefronts are squeezed together and behind it they are stretched out, so you hear the note raised as it approaches, by a factor of 1/(1−M), and lowered as it leaves, by 1/(1+M). The drop between the two is what you hear. A car at 100 km/h is Mach 0.08, and the note falls by nearly three semitones — enough to hear clearly, as everyone has.

What this page assumes

An ideal gas for the speed of sound, √(γRT/M), with a constant ratio of specific heats. Real air departs from it by well under a tenth of a per cent in the range here; humidity raises the speed slightly (about half a per cent in warm, saturated air), and that is not modelled.

The International Standard Atmosphere for temperature with height: 15 °C at sea level falling 6.5 °C per kilometre to −56.5 °C at 11 km, constant to 20 km, then warming 1 °C per kilometre — shifted up or down by the day-temperature offset. Real days have inversions and weather this does not.

Still air. Wind shifts where a boom lands and can cause or prevent cutoff on its own; it is not modelled. The boom's path to the ground is the acoustic ray through the layered temperature profile, and only straight down the flight path — the width of the boom carpet either side is not computed.

Choosing another gas fills the whole atmosphere with it at the same temperatures, which no atmosphere does; it is there to show what γ and molar mass do. The flyby sound is a synthesis of the Doppler shift and the N-wave, not a recording.

Field notes

Things that follow from the cone

Exact for an ideal gas in a standard, still atmosphere. Real days have wind, humidity and temperature inversions, and each moves where a boom lands — or whether it lands at all. See Sources.
Version history · unchanged

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