whether you are talking about waves on the beach or waves of light or sound waves. the time it takes for one wave to oscillate completely is the period of the wave. if, however you would like to know how many oscillations each wave completes per second, then you would be looking for frequencys
The length of time between breaking waves is called the wave period. It is typically measured in seconds and is an important characteristic in understanding wave behavior and forecasting ocean conditions.
whether you are talking about waves on the beach or waves of light or sound waves. the time it takes for one wave to oscillate completely is the period of the wave. if, however you would like to know how many oscillations each wave completes per second, then you would be looking for frequencys
Frequency is inversely proportional to the wave length, thus saying the shorter the wave length the higher the frequency and vice versa.The frequency is the number of waves within a time period. As the frequency within that time period increases, the number of waves increases, therefore the width of each wave (wavelength) within that time period has to decrease. Therefore:As the wave length increases, the frequency decreasesAs the wave length decreases, the frequency increases
To determine the phase difference between two waves, you can compare the starting points of the waves and measure the time it takes for each wave to reach a specific point. The phase difference is then calculated based on the difference in time or angle between the two waves.
The distance a wave travels in a given length of time depends on its speed. The speed of a wave is determined by the medium through which it travels. In general, faster waves will travel greater distances in the same amount of time compared to slower waves.
The length of time between breaking waves is called the wave period. It is typically measured in seconds and is an important characteristic in understanding wave behavior and forecasting ocean conditions.
whether you are talking about waves on the beach or waves of light or sound waves. the time it takes for one wave to oscillate completely is the period of the wave. if, however you would like to know how many oscillations each wave completes per second, then you would be looking for frequencys
The length of time between pulses is the "pulse repetition rate". The length of time between consecutive waves is the "period". It's the reciprocal of the frequency.
It is a range between a certain time and another time. Ex. length of time between 2000 and 2009 is 9 years.
(The power of the radio transmitter) times (the length of time it continues to transmit)
False. The closer an earthquake is, the shorter the time difference between the arrival of P waves and S waves. P waves travel faster than S waves, so the time interval decreases as the distance to the earthquake epicenter decreases.
Yes, that is correct. The time difference between the arrival of P-waves and S-waves increases as the earthquake epicenter gets closer to the seismograph. P-waves are faster, so they arrive first, followed by the slower S-waves.
Starfish spend most of their time in deep water. This means they're well out of the reach of the effects of waves breaking on the shore. If they ARE 'caught' by waves - their only option is to 'go with the flow' !
Frequency is inversely proportional to the wave length, thus saying the shorter the wave length the higher the frequency and vice versa.The frequency is the number of waves within a time period. As the frequency within that time period increases, the number of waves increases, therefore the width of each wave (wavelength) within that time period has to decrease. Therefore:As the wave length increases, the frequency decreasesAs the wave length decreases, the frequency increases
The lag time between the arrival of P-waves and S-waves generally gets longer the further you are from the earthquake's epicenter. P-waves travel faster than S-waves, so the time difference between their arrivals increases with distance.
As P-waves travel at a higher velocity than S-waves they arrive at a seismometer station before the S-waves. The difference between their arrival time can be used to calculate the distance from the seismometer station to the epicentre.
To determine the phase difference between two waves, you can compare the starting points of the waves and measure the time it takes for each wave to reach a specific point. The phase difference is then calculated based on the difference in time or angle between the two waves.