An acoustic radar is a device acting as the well known radars, with the
difference that the transmitted and the received signals have frequencies
in the acoustic region. An alternate name for this class of instruments is
'Sodar', due to the SOund Detection And Ranging'. A short acoustic pulse is transmitted in the atmosphere.
While it is travelling in there, it is scattered from the atmospheric
irregularities. Here, the irregularities don't mean a 'target' object, as in the
usual electromagnetic or microwave radars. A change in the wind velocity, a
turbulent layer, a temperature inversion e.t.c. cause scattering of the acoustic
waves. A part of the scattered signal returns to the receiver, where it is
collected and processed.
There are various configurations for a sodar device.
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- A monostatic system
These systems use the same antenna for
transmitting the acoustic pulse and receiving the backscattered acoustic waves.
- A bistatic system
These systems use two antennas, one for
trasmission of the acoustic pulses and one for the reception of the signals
scattered to the direction the receiving antenna points to.
- A tristatic system
Here we have three monostatic antennas
pointing to three no coplanar directions. These systems permit the measurement
of atmospheric parameters having a 'vector' nature (i.e. winds' velocity).
An example of an old monostatic system is presented in Figure 3. The antenna is
constructed from an electrodynamic transducer in the focal point of a
parabolic dish reflector. It is clear that the system is heavy and it is
difficult to move it in hard to reach places.
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An important point in the evolution of the sodars was the usage of array antennas. An antenna constructed from Celestions acoustic transducers, in a square planar topology, is presented in the figure left. You can also see in this figure the screening of the antenna using sound absorbing material. The screening is used to supress the sidelobes of the antenna (i.e. to reduce the undesired signal received from the sidelobes).
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Example of the antenna of a modern tristatic sodar (METEK's MODOS Model).
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Example of a modern antenna of a phased array sodar (REMTECH's PA2 Model). Due to the number of elements used and electronic 'apodization' (sidelobe suppression through the usage of different amplitudes for the signals feeding the elements) of the beam, the resulting main lobe's directivity and sidelobe levels are excellent and there is no need for shielding the antenna.
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Examples of facsimile recordings of the signal received from a sodar system (in
Black&White or Color Mode). The intensity of the received signal is used to show the existense of layers in the atmospheric boundary layer and their evolution with time.
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