Sound waves travel faster in warmer air. If the temperature of the air near the ground is colder than air higher up, then sound waves traveling slightly upward will bend downward. This tends to "focus" the sound waves back toward the ground and can help amplify the sounds when you are far away.
The sound made by wind is commonly called "whistling" or "whistling sound."
Earthquake?
Whistling can create a tone that resonates with the natural frequency of the wind, causing the wind to vibrate and amplify the sound. This phenomenon is known as the "Möbius resonance effect." The interaction between the whistling sound and the wind can create a feedback loop that enhances the sound and seems to call for the wind.
Sound energy is carried through vibrations in a medium, such as air, water, or solid objects. When an object vibrates, it causes the particles in the medium to move in a wave-like pattern, transmitting the sound energy from the source to our ears.
Sound travels faster downwind. The speed at which sound travels is relative to the medium it is moving through. When sound is traveling upwind, you subtract the wind speed from the speed of sound. When it is traveling down wind you add the wind speed.
Aloha: The sound of the wind. (not the sound that the wind makes, but it means "the sound of the wind")
When the wind stops blowing.
wind
Wind pollination is when pollen is carried in the wind
by the wind
Eroded materials carried by wind or water are called sediment.
The onomatopoeia for the sound of wind is "whooosh" or "whistling."
Wind-carried sediment falls to the ground when the wind speed decreases or when the particles become too heavy to be carried by the wind. Additionally, obstacles like vegetation or changes in topography can also cause sediment to settle out of the air.
wind
The sound made by wind is commonly called "whistling" or "whistling sound."
No Sound But the Wind was created on 2010-07-26.
dust