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for generating an RMA number. If additional help is needed, please contact Campbell Scientific.
When preparing the CSAT3BH for shipment, be sure to package it in the same foam in which it
was sent. If the foam cannot be found, new foam should be ordered from Campbell Scientific
before returning the unit.
9. References
Burns, S.P., T.W. Horst, L. Jacobsen, P.D. Blanken, and R.K. Monson. 2012. “Using sonic
anemometer temperature to measure sensible heat flux in strong winds.”
Atmos Meas Tech
5: 2095–2111.
Horst, T.W., S.R. Semmer, and G. Maclean. 2015. “Correction of a Non-orthogonal, Three-
Component Sonic Anemometer for Flow Distortion by Transducer Shadowing.”
Boundary-
Layer Meteorology
155: 371–395. https://doi.org/. 10.1007/s10546-015-0010-3.
Kaimal, J.C. 1979. “Sonic anemometer measurement of atmospheric turbulence.” Proceeding of
the Dynamic Flow Conference of DISA Electronic A/S, Skovlunde 551–565.
Kaimal, J.C. and J.J. Finnigan. 1994.
Atmospheric Boundary Layer Flows
. Oxford: Oxford University
Press.
Liu, H., G. Peter, and T. Foken. 2001. "New equations for sonic temperature variance and
buoyancy heat flux with an omnidirectional sonic anemometer."
Boundary-Layer
Meteorology
100: 459–468.
Schotanus, P., F.T.M. Nieuwstadt, and H.A.R. de Bruin. 1983. "Temperature measurement with a
sonic anemometer and its application to heat and moisture fluxes."
Boundary-Layer
Meteorology
26: 81–93.
CSAT3BH Three-Dimensional Heated Sonic Anemometer
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