The speed. Also, the wavelength, since the speed is equal to wavelength x frequency, and the frequency will normally NOT change.
If the wave slows down but its frequency remains the same, the wavelength of the wave will also decrease. This is because the speed of a wave is directly proportional to its wavelength when frequency is constant. Therefore, when the wave slows down, its wavelength decreases proportionally to maintain the same frequency.
If the wave slows down but its frequency remains the same, the wavelength of the wave will also decrease. This is because the speed of a wave is inversely proportional to its wavelength, so if the speed decreases, the wavelength must also decrease.
If the wave slows down but its frequency remains the same, the wavelength will shorten. This is because the speed of a wave is directly proportional to its wavelength - if the speed decreases and frequency stays constant, the wavelength must also decrease to maintain the relationship.
When a wave approaches land, it slows down because of the shallower water depth. This causes the wavelength to decrease and the wave height to increase, eventually leading to the wave breaking near the shore.
The bending of a light wave as it slows down after hitting a medium is called refraction. This occurs because light travels at different speeds in different mediums, causing the change in direction as it moves from one medium to another.
If the wave slows down but its frequency remains the same, the wavelength of the wave will also decrease. This is because the speed of a wave is directly proportional to its wavelength when frequency is constant. Therefore, when the wave slows down, its wavelength decreases proportionally to maintain the same frequency.
If the wave slows down but its frequency remains the same, the wavelength of the wave will also decrease. This is because the speed of a wave is inversely proportional to its wavelength, so if the speed decreases, the wavelength must also decrease.
If the wave slows down but its frequency remains the same, the wavelength will shorten. This is because the speed of a wave is directly proportional to its wavelength - if the speed decreases and frequency stays constant, the wavelength must also decrease to maintain the relationship.
the frequancy of a wave is always equal to the rate of vibration of the source that creates it.
Diffraction, with light it splits the colors most notably in a prism.
When a wave approaches land, it slows down because of the shallower water depth. This causes the wavelength to decrease and the wave height to increase, eventually leading to the wave breaking near the shore.
i need help please!!!!!!!!!
The bending of a light wave as it slows down after hitting a medium is called refraction. This occurs because light travels at different speeds in different mediums, causing the change in direction as it moves from one medium to another.
The process is called wave refraction. As deep water waves enter shallow water, the portion of the wave closest to the shore slows down due to the shallower depth, causing the wave to bend and align more parallel to the shoreline. This phenomenon helps reduce the wave energy hitting the shore more directly.
The wavelength of the wave decreases as it enters Perspex due to the change in the speed of the wave, according to Snell's Law. The wave slows down in Perspex, causing the wavelength to shorten.
Wavelength and frequency are locked together in an inverse proportionality. If the frequency of a wave is constant, the wavelength of the wave will be constant. Increase one and the other decreases. Decrease one and the other increases. That said, let's look at the dynamics of a tsunami, which may be the general direction in which this was heading. In a tsunami, the wave moves very quickly in the open ocean, and it has a long wavelength. As it closes on shore, the leading edge of the wave slows down as the sea bottom "rises up" to meet the wave. As the leading edge of the wave continues to slow down, the "rest of the wave" begins to "catch up" with the wave front. This causes the wave to build; its height will increase. The actual wavelength is decreasing (and its frequency will be increasing), and the wave continues to slow down. Higher and higher it will build, and then it will break on the shore and carry inland.
Wavelength and frequency are locked together in an inverse proportionality. If the frequency of a wave is constant, the wavelength of the wave will be constant. Increase one and the other decreases. Decrease one and the other increases. That said, let's look at the dynamics of a tsunami, which may be the general direction in which this was heading. In a tsunami, the wave moves very quickly in the open ocean, and it has a long wavelength. As it closes on shore, the leading edge of the wave slows down as the sea bottom "rises up" to meet the wave. As the leading edge of the wave continues to slow down, the "rest of the wave" begins to "catch up" with the wave front. This causes the wave to build; its height will increase. The actual wavelength is decreasing (and its frequency will be increasing), and the wave continues to slow down. Higher and higher it will build, and then it will break on the shore and carry inland.