M. V. Iersel, J. Rzasa, Daniel A. Paulson, Nathaniel A. Ferlic, C. Davis, Jonathan Spychalsky, Joseph T. Coffaro, Franklin Titus, R. Crabbs
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Comparing measurements of RTD probe systems and sonic anemometers
Ground to air temperature gradients are the drivers of optical turbulence. Different systems can measure temperature fluctuations. C T 2 and C n 2 are derived from RTD probe systems and sonic anemometers mounted at several heights and compared.