Measuring C T 2 , C Q 2 , and C TQ in the unstable surface layer, and relations to the vertical fluxes of heat and moisture
Author:
Publisher
Springer Science and Business Media LLC
Subject
Atmospheric Science
Link
http://link.springer.com/content/pdf/10.1007/BF00121802.pdf
Reference18 articles.
1. Coulter, R. L. and Wesely, M. L.: 1980, ?Estimates of Surface Heat Flux from Sodar and Laser Scintillation Measurements in the Unstable Boundary Layer?, J. Appl. Meteorol. 19, 1209?1222.
2. Davidson, K. L., Houlihan, T. M., Fairall, C. W., and Schacher, G. E.: 1978, ?Observation of the Temperature Structure Function Parameter, C T 2 , over the Ocean?, Boundary-Layer Meteorol. 15, 507?523.
3. Dyer, A. J. and Hicks, B. B.: 1970, ?Flux-Gradient Relationships in the Constant Flux Layer?, Quart. J. Roy. Meteorol. Soc. 96, 715?721.
4. Fairall, C. W., Schacher, G. E., and Davidson, K. L.: 1980, ?Measurements of the Humidity Structure Function Parameters, C q 2 and C Tq , over the Ocean?, Boundary-Layer Meteorol. 19, 81?92.
5. Fitzmaurice, M. W., Bufton, J. L., and Minott, P. O.: 1969, ?Wavelength Dependence of Laser-Beam Scintillation?, J. Opt. Soc. Amer. 59, 7?10.
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