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If the source and listener are moving closer to each other, the listener will
          perceive  a  higher  frequency  -  the  faster  the  source  or  receiver  is
          approaching the higher the Doppler shift.
          If  the  source  and  listener  are  getting  farther  apart,  the  listener  will
          perceive a lower frequency - the faster the source or receiver is moving
          away the lower the frequency.

          The Doppler shift is directly proportional to speed between source and
          listener, frequency of the source, and the speed the wave travels.
          In above figure ‘v’ is the velocity of sound, and the propagation speed is ‘
          c’, every wave is shortened due to the movement of the source by ‘d’



















          The Doppler log is based on measurement of the Doppler effect.

          It is seen that an observer, moving with a source of sound towards a
          reflecting plane, receives a frequency:

          Where fv  is the  received frequency, f  the  transmitted frequency, c the
          speed of sound and v the speed of the source of sound.

          Principle

          A transmitting transducer below the ship continuously emits a beam of
          sound vibrations in the water at an angle  (usually 60˚ to the keel) in the
          forward direction.

          A  second  transducer  aboard  receives  the  echo  caused  by  diffuse
          reflection from the seabed.

          A Doppler log uses a higher frequency than an echo sounder.





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