Speed of Sound


I'm sorry to have to be so vague, but the answer to your question is "it depends!" The reason we can't be more specific is that it all depends on what the speed of sound is through a substance under certain conditions. Now if you had asked how fast is Mach 2 in the standard atmosphere at sea level, the answer could be found by simply looking up the speed of sound at sea level in a standard atmospheric table and multiplying it by two. Since the speed of sound through the standard atmosphere is 761 mph (1,223 km/h) at sea level, Mach 2 then follows as 1,522 mph (2,447 km/h). If you were to ask how fast is Mach 2 at an altitude of 30,000 ft (9,150 m), we would use the same methodology to find out that it is only 1,356 mph (2,180 km/h) because the speed of sound generally decreases as altitude increases.

So your next logical question is why does the speed of sound change? To understand this concept, we must understand the physical mechanism of how sound travels. In a solid material, sound waves propogate through vibration. The molecules of a solid are very closely packed together and physically connected to each other. A passing sound wave vibrates one molecule, and that molecule induces a vibration in its neighbors, and those molecules induce further vibrations in their neighbors, and so on until the sound wave runs out of energy. A similar process occurs is a gas, like air. The only difference is that the molecules of air are not physically connected to each other, but they do still vibrate under the influence of a sound wave. As a molecule vibrates, it collides with other molecules thereby transmitting some of its kinetic energy to those particles. These energetic gas molecules also continue moving about randomly colliding with new particles and transferring some of their excess kinetic energy.

In relation to our discussion, the speed of sound is directly related to the frequency at which these molecular collisions occur, and that frequency is directly related to the density of how those molecules are packed. Sound travels fastest through a solid and slowest through a gas. In the days of train travel, people used to hold their ears against the railroad tracks because they could hear the rumble of an oncoming train through the densely-packed molecules of the steel tracks long before the sound waves arrived through the air. Similarly, sound travels faster through a liquid, like water, than it does through the air due to the liquid's increased density. Sound also travels faster through harder solids, like metals, than through softer materials, like wood, because of the density of the molecules that make up the substance. The same principle holds true of the atmosphere. As discussed in a previous question on air density, the density of the atmosphere decreases as altitude increases, so we would expect the speed of sound through the air to decrease as well.

While this is indeed the case up to about 36,000 ft (11,000 m), the speed of sound eventually reaches a constant, then starts rising again, reaches a new constant, starts decreasing again, reaches a new constant, then starts rising yet again! The reason for this odd behavior is that the speed of sound depends on more than just density, but also on atmospheric pressure and (by extension) temperature. While I could easily bore you further with a detailed mathematical derivation to explain this, the simple explanation is that the atmosphere is made up of zones where atmospheric properties vary wildly. You may have heard of terms like the Troposphere, Stratosphere, and Tropopause. Based on experimental data, scientists have measured the atmospheric properties in each of these regions and defined how these properties vary, as illustrated below.

Variation of temperature through the layers of the atmosphere
Variation of temperature through the layers of the atmosphere

These defined relationships constitute the "standard atmosphere" we have already spoken of. The key variable in this standard atmosphere is temperature as all other basic properties can be computed from it. Since the speed of sound is a function of density and pressure and both density and pressure are functions of temperature, we end up with a simple relationship for speed of sound as a funtion of temperature:

where

By merely looking up the temperature at a specified altitude in a standard atmosphere chart (in degrees Rankine), one can then easily compute the speed of sound. We can make the process even easier for you since this method is also used in our Atmospheric Properties Calculator when a user enters nothing more than the altitude. Furthermore, a speed at that altitude can also be input to compute the associated Mach number, or a Mach number can be entered to calculate the associated true airspeed.
- answer by Jeff Scott, 30 December 2001

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