Articles | Volume 8, issue 8
Atmos. Meas. Tech., 8, 3527–3536, 2015
https://doi.org/10.5194/amt-8-3527-2015

Special issue: BACCHUS – Impact of Biogenic versus Anthropogenic emissions...

Atmos. Meas. Tech., 8, 3527–3536, 2015
https://doi.org/10.5194/amt-8-3527-2015

Research article 31 Aug 2015

Research article | 31 Aug 2015

Combined vertical-velocity observations with Doppler lidar, cloud radar and wind profiler

J. Bühl et al.

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Cited articles

Angevine, W. M.: Errors in Mean Vertical Velocities Measured by Boundary Layer Wind Profilers, J. Atmos. Ocean. Tech., 14, 565–569, https://doi.org/10.1175/1520-0426(1997)014<0565:EIMVVM>2.0.CO;2, 1997.
Böhme, T., Hauf, T., and Lehmann, V.: Investigation of short-period gravity waves with the Lindenberg 482 MHz tropospheric wind profiler, Q. J. Roy. Meteor. Soc., 130, 2933–2952, https://doi.org/10.1256/qj.03.179, 2004.
Bühl, J.: Combined lidar and radar observations of vertical motions and heterogeneous ice formation in mixed-phase layered clouds, Univ. Leipzig, available at: http://nbn-resolving.de/urn:nbn:de:bsz:15-qucosa-171998, 2015.
Bühl, J., Engelmann, R., and Ansmann, A.: Removing the laser-chirp influence from coherent doppler lidar datasets by two-dimensional deconvolution, J. Atmos. Ocean. Tech., 29, 1042–1051, https://doi.org/10.1175/JTECH-D-11-00144.1, 2012.
Bühl, J., Ansmann, A., Seifert, P., Baars, H., and Engelmann, R.: Towards a quantitative characterization of heterogeneous ice formation with lidar/radar: comparison of CALIPSO/CloudSat with ground-based observations, Geophys. Res. Lett., 40, 4404–4408, https://doi.org/10.1002/grl.50792, 2013.
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Short summary
Case studies of combined vertical-velocity measurements of Doppler lidar, cloud radar and wind profiler are presented. The measurements were taken at the Meteorological Observatory, Lindenberg, Germany. Synergistic products are presented that are derived from the vertical-velocity measurements of the three instruments: a comprehensive classification mask of vertically moving atmospheric targets and the terminal fall velocity of water droplets and ice crystals corrected for vertical air motion.