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Fig. 11. Relationship between lidar- and eddy-covariance-derived integral length scales and the Obukhov length (L) estimated from two field experiments. The similarity model based on a stability function (Eq. [13]) is shown as a dotted line and the ±10% uncertainty functions are shown as dashed lines; the equations used to compute the similarity based estimates based on z/L and friction velocity are also shown.

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