Campbell Scientific CSAT3B CSAT3B Three-Dimensional Sonic Anemometer - Page 79
B.2 References
View all Campbell Scientific CSAT3B manuals
Add to My Manuals
Save this manual to your list of manuals |
Page 79 highlights
Appendix B. CSAT3B Measurement Theory Substitute Eq. (B-7a) and (B-7b) into (B-6) and ignore the higher order terms. This yields c2 = γ dRdTs = γ dRdT(1+ 0.51q) (B-8) where: Ts = sonic virtual temperature γd = ratio of specific heat of dry air at constant pressure to that at constant volume (Fleagle and Businger, 1980; Kaimal and Gaynor, 1991; Kaimal and Businger, 1963; Schotanus et al., 1983) With Eq. (B-8), the effect of humidity, on the speed of sound, is included in the sonic virtual temperature. The sonic virtual temperature, in degrees Celsius, is given by Eq. (B-9), where γd = 1.4 and Rd = 287.04 JK-1 kg-1. c2 Ts = γ dRd − 273.15 (B-9) B.2 References Kaimal, J. C. and Businger, J. A.: 1963, "A Continuous Wave Sonic Anemometer-Thermometer", J. Applied Meteorol., 2, 156-164. Kaimal, J. C. and Gaynor, J. E.: 1991, "Another Look at Sonic Thermometry", Boundary-Layer Meteorol., 56, 401-410. Fleagle, R. G. and Businger, J. A.: 1980, An Introduction to Atmospheric Physics, Academic Press, Inc., New York. Liu, H., Peters, G. and Foken, T.: 2001, "New Equations for Sonic Temperature Variance and Buoyancy Heat Flux with an Omnidirectional Sonic Anemometer", Boundary-Layer Meteorol., 100, 459-468. Schotanus, P., Nieuwstadt, F. T. M. and de Bruin, H. A. R.: 1983, "Temperature Measurement with a Sonic Anemometer and its Application to Heat and Moisture Fluxes", Boundary-Layer Meteorol., 26, 81-93. Wallace, J. M. and Hobbs, P. V.: 1977, Atmospheric Science an Introductory Survey, Academic Press, Inc., New York. B-3