6.3
Random error in atmospheric flux measurements
Peter L. Finkelstein, NOAA and U.S. EPA, Research Triangle Park, NC
Sampling errors in eddy correlation flux measurements arise from the small number of large eddies that dominate the flux during a short sampling period. Several methods to estimate sampling, or random error in flux measurements have been published. These methods are compared to a more statistically rigorous method which calculates the variance of a covariance when the two variables in the covariance are auto and cross correlated. Comparisons are offered between the various methods. Compared to previously published methods, estimates from this technique were 20% to 25% higher because of the incorporation of additional terms in the estimate of the variance. This new approach is then applied to define the random error component of representative eddy correlation flux measurements of momentum, sensible and latent heat, carbon dioxide, and ozone from 5 field studies, three over agricultural crops (corn, soybean, and pasture) and two from tall towers over deciduous and mixed forests. The mean normalized error for each type of flux measurement over the 5 studies ranged from 12% for sensible heat flux to 31% for ozone flux. There were not large or significant differences between random errors for fluxes measured over crops versus those measured over forests. The effects of stability, flux magnitude, and wind speed on measurement error are discussed.
Session 6, Micrometeorological Instrumentation
Thursday, 17 August 2000, 11:15 AM-11:44 AM
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