Period = (1) divided by (frequency) = (wavelength) divided by (speed)Frequency = (1) divided by (period) = (speed) divided by (period)Speed = (wavelength) times (frequency) = (wavelength) divided by (period)Wavelength = (speed) divided by (frequency) = (speed) times (period)
A series of regular timed disturbances in a medium.
u can differentiate seismic waves by 1- their movement , 2 - velocity , 3 - amplitude , period and frequency .
If a radio wave has a period of one then the period wave or two would be 2. This is math.
when there are more waves passing through the reference point in a period of time, which wave characteristic also increase
T=1/f T=1/1000 T=1*10-3
because your frequency has changed. The distance between waves is shorter at 1000hz than at 100hz.
0 dBrnc=-90dBm (1000Hz Toned)
You can use the formula v=fλ where v is velocity (speed), f is frequency, and λ is the wavelength. Thus, you get v=(1000Hz)(1.5m) --> v=1500m/s
no , 1hz is 1 oscillation , 1000hz ( 1khz ) is 1000 oscillations !
T, seconds
period
Period = (1) divided by (frequency) = (wavelength) divided by (speed)Frequency = (1) divided by (period) = (speed) divided by (period)Speed = (wavelength) times (frequency) = (wavelength) divided by (period)Wavelength = (speed) divided by (frequency) = (speed) times (period)
after a period of time yes
A series of regular timed disturbances in a medium.
u can differentiate seismic waves by 1- their movement , 2 - velocity , 3 - amplitude , period and frequency .
If a radio wave has a period of one then the period wave or two would be 2. This is math.