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

discrepancies between measurements and model counterparts that are due to local terrain effects ( Hahmann et al. 2010 ; Boilley and Mahfouf 2012 ). Observed wind speeds at greater heights can show large differences when using different reanalysis data to reinitialize the Weather Research and Forecasting (WRF) model ( Floors et al. 2013 ). Verification of data assimilation techniques is now possible with the advent of new types of instruments, such as wind Doppler lidars, that observe winds with high

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