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Atmospheric Measurement Techniques An interactive open-access journal of the European Geosciences Union
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Volume 7, issue 11
Atmos. Meas. Tech., 7, 3685–3704, 2014
https://doi.org/10.5194/amt-7-3685-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Meas. Tech., 7, 3685–3704, 2014
https://doi.org/10.5194/amt-7-3685-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 08 Nov 2014

Research article | 08 Nov 2014

Mixing-layer height retrieval with ceilometer and Doppler lidar: from case studies to long-term assessment

J. H. Schween et al.

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Cited articles

American Meteorological Society: Glossary of Meteorology, American Meteorological Society, http://glossary.ametsoc.org/, last access: 25 April 2014, 2013.
Augstein, E., Schmidt, H., and Wagner, V.: The vertical structure of the atmospheric planetary boundary layer in undisturbed Trade winds over the Atlantic Ocean, Bound-Lay. Meteorol., 6, 129–150, https://doi.org/10.1007/BF00232480, 1974.
Baars, H., Ansmann, A., Engelmann, R., and Althausen, D.: Continuous monitoring of the boundary-layer top with lidar, Atmos. Chem. Phys., 8, 7281–7296, https://doi.org/10.5194/acp-8-7281-2008, 2008.
Banta, R. M., Pichugina, Yelena, L., and Brewerm, W. A.: Turbulent Velocity-Variance Profiles in the Stable Boundary Layer Generated by a Nocturnal Low-Level Jet, J. Atmos. Sci., 63, 2700–2719, https://doi.org/10.1175/JAS3776.1, 2006.
Barlow, J., F., Dunbar, T. M., Nemitz, E. G., Wood, C. R., Gallagher, M., Davies, F., O'Connor, E., and Harrison, R. M.: Boundary layer dynamics over London, UK, as observed using Doppler lidar during REPARTEE-II, Atmos. Chem. Phys., 11, 2111–2125, https://doi.org/10.5194/acp-11-2111-2011, 2011.
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Two different methods for the determination of the mixing layer height (MLH) are investigated with a one-year data set from central Europe: (i) based on a significant gradient of backscatter and (ii) on the vertical velocity. The aerosol-based method shows significant over-estimation in the morning hours when the ML grows into the residual layer and late afternoon hours when turbulent mixing decays. This results in systematic over-estimation of average characteristcs as e.g. maximum MLH.
Two different methods for the determination of the mixing layer height (MLH) are investigated...
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