Sound spectrum, from low frequency to high frequency, is a continuous spectrum.
Over the entire span of the frequency spectrum there is gradual change of properties.
Propagating sound is propagating (longitudinal) waves of compression and rarefaction of air. As we know, when air is compressed it heats up. So the temperature of the air is non-uniform, in accordance with the oscillation pattern. The temperature difference is minute, but there is an audible effect that arises from it.
The shorter the wavelength of the sound, the more opportunity is for the heat to spread. The effect of this spreading is that the energy of the pressure oscillation dissipates to evenly distributed heat. What that means is that high frequency sound has a noticably faster rate of dissipation of sound energy to heat.
For instance, when a lightning strike is relatively close by then the explosive sound that is produced sounds like a harsh crack. It sounds as if a giant whip is cracked. The harshness of the sound arises from high frequency components in the sound.
When a lightning strike occurs many kilometers away the sound that reaches you, eventually, sounds like low pitched rumbling. Over the length of the kilometers of travel all the high frequency components have dissipated to heat. The lower the frequency, the further it can travel. So, over a distance of many kilometers only the lowest frequencies make it to your ears.
This trend of higher sound frequencies dissipating to heat faster continues with Ultrasonic sound.
In that sense 'Ultrasonic sound' is in fact different, but the difference correlates with the frequency of the sound produced; not with whether the sound is audible to humans or not