Abstract. A direct-detection Rayleigh–Mie Doppler lidar for measuring horizontal
wind speed in the middle atmosphere (10 to 50 km altitude) has
been deployed at Observatoire de Haute-Provence (OHP) in southern
France starting from 1993. After a recent upgrade, the instrument gained the
capacity of wind profiling between 5 and 75 km altitude with
vertical resolution up to 115 m and temporal resolution up to
5 min. The lidar comprises a monomode Nd:Yag laser emitting at
532 nm, three telescope assemblies and a double-edge
Fabry–Pérot interferometer for detection of the Doppler shift in the
backscattered light. In this article, we describe the instrument
design, recap retrieval methodology and provide an updated error
estimate for horizontal wind. The evaluation of the wind lidar
performance is done using a series of 12 time-coordinated
radiosoundings conducted at OHP. A point-by-point intercomparison
shows a remarkably small average bias of 0.1 m s−1 between
the lidar and the radiosonde wind profiles with a standard deviation
of 2.3 m s−1. We report examples of a weekly and an hourly
observation series, reflecting various dynamical events in the middle
atmosphere, such as a sudden stratospheric warming event in January
2019 and an occurrence of a stationary gravity wave, generated by the
flow over the Alps. A qualitative comparison between the wind profiles
from the lidar and the European Centre for Medium-Range Weather Forecasts (ECMWF) Integrated Forecast System is also
discussed. Finally, we present an example of early validation of the
European Space Agency (ESA) Aeolus space-borne wind lidar using its ground-based predecessor.