Abstract
A combination of lateral coherence measurements of wind speed at five locations suggests that the ‘decay constant’ is a monotonically increasing function of the ratio of separation to height, under neutral conditions.
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Kristensen, L., Panofsky, H.A. & Smith, S.D. Lateral coherence of longitudinal wind components in strong winds. Boundary-Layer Meteorol 21, 199–205 (1981). https://doi.org/10.1007/BF02033937
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DOI: https://doi.org/10.1007/BF02033937