Abstract

Responses of Kaijo Denki TR-61A, TR-61B, and TR-61C; Solent Research/Gill; and METEK USA-1 sonic anemometer systems have been examined in a wind tunnel investigation. To determine their characteristics the anemometers were turned for 360° and tilted for up to ±8°. With a small Pitot tube the modification of the wind field by a Kaijo Denki TR-61B sensor is examined within its measuring volume. Extra measurements were executed to analyze the influence of turbulent wakes behind sensor parts windward of the measuring volume. Measurements from the Echival Field Experiment in Desertification Threatened Areas of 1994 are used to compare the measurements of Kaijo Denki TR-61C, Solent Research/Gill, and METEK USA-1 sonic anemometers in the atmospheric boundary layer. Struts and transducers are leading to decreased mean wind velocity, deviation, and higher variances depending on the probe geometry and dimension. Best results can be achieved with the Solent Research and Kaijo Denki TR-61B sensors. The Solent Research/Gill calibration procedure improves the mean horizontal wind velocity and direction significantly, but it should be used with caution because it increases variances especially at incoming flow directions where sensor-induced turbulence is at its highest. The TR-61C is still a usable instrument for the measurement of turbulent fluxes as long as the vertical sound path is not placed in the turbulent wake of the sensor foot. The direction characteristic of the TR-61A reduces its operational range but supplies most precise vertical wind velocity measurements. The METEK USA-1 has an interesting sensor geometry and user interface but needs further improvements in its electronics.

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