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Qing Yang, Larry K. Berg, Mikhail Pekour, Jerome D. Fast, Rob K. Newsom, Mark Stoelinga, and Catherine Finley

. Clough , 1997 : Radiative transfer for inhomogeneous atmosphere: RRTM, a validated correlated- k model for the longwave . J. Geophys. Res. , 102 , 16 663 – 16 682 . Pleim , J. E. , and A. Xiu , 1995 : Development and testing of a surface flux and planetary boundary layer model for application in mesoscale models . J. Appl. Meteor. , 34 , 16 – 32 . Shin , H. H. , and S.-Y. Hong , 2011 : Intercomparison of planetary boundary-layer parametrizations in the WRF model for a single day

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S.-E. Gryning, E. Batchvarova, and R. Floors

160 m is measured with wind vanes on booms directed to the south. A pulsed wind Doppler lidar (Leosphere WLS70) was operated during the campaign and was located about 20 m west of the meteorological mast. The wind Doppler lidar is equipped with a rotating silicon prism that provides an optical scanning cone of 15° to zenith. The lidar scans the atmosphere at four azimuth angles separated by 90°. One 360° full scan (rotation) is performed approximately every 30 s. The Doppler shift

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