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al to the square root of

absolute temperature. Sound pulses are transmitted into the air with a vertical trajectory, and their motion monitored using acoustic backscattering in the SODAR system and radar in the RASS system. Instruments intended for extended range into the atmosphere rely more on the radarEMRTC and less on the acoustic responses. As the sound pulse travels upward, its velocity will change as it travels t

hrough layers having differing temperatures in the atmosphere