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Airborne Wind Lidar Measurements of Vertical and Horizontal Winds for the Investigation of Orographically Induced Gravity Wavesflown along the same mountain transect, giving both the wind vector and the vertical wind speed with a slight temporal difference of about 1 h. However, as the data coverage of both measurements can be different, not every LOS wind measurement may correspond to a wind vector measurement that can be used for correction. Thus, to be able to correct all LOS measurements, the horizontal wind from European Centre for Medium-Range Weather Forecasts (ECMWF; T1279 L137, cycle 40r1) operational analyses on
flown along the same mountain transect, giving both the wind vector and the vertical wind speed with a slight temporal difference of about 1 h. However, as the data coverage of both measurements can be different, not every LOS wind measurement may correspond to a wind vector measurement that can be used for correction. Thus, to be able to correct all LOS measurements, the horizontal wind from European Centre for Medium-Range Weather Forecasts (ECMWF; T1279 L137, cycle 40r1) operational analyses on
