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 tunne
l investigation. To determine their characteristics the anemometers were tu
rned for 360 degrees and tilted for up to +/-8 degrees. With a small Pitot
tube the modification of the wind field by a Kaijo Denki TR-61B sensor is e
xamined within its measuring volume. Extra measurements were executed to an
alyze the influence of turbulent wakes behind sensor parts windward of the
measuring volume. Measurements from the Echival Field Experiment in Deserti
fication Threatened Areas of 1994 are used to compare the measurements of K
aijo Denki TR-61C, Solent Research/Gill, and METEK USA-1 sonic anemometers
in the atmospheric boundary layer. Struts and transducers are leading to de
creased mean wind velocity, deviation, and higher variances depending on th
e probe geometry and dimension. Best results can be achieved with the Solen
t Research and Kaijo Denki TR-61B sensors. The Solent Research/Gill calibra
tion procedure improves the mean horizontal wind velocity and direction sig
nificantly, but it should be used with caution because it increases varianc
es especially at incoming flow directions where sensor-induced turbulence i
s at its highest. The TR-61C is still a usable instrument for the measureme
nt 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 win
d velocity measurements. The METEK USA-1 has an interesting sensor geometry
and user interface but needs further improvements in its electronics.