Atmos. Chem. Phys. Discuss., 11, 30949-30987, 2011
www.atmos-chem-phys-discuss.net/11/30949/2011/
doi:10.5194/acpd-11-30949-2011
© Author(s) 2011. This work is distributed
under the Creative Commons Attribution 3.0 License.
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This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Lidar and radar measurements of the melting layer in the frame of the Convective and Orographically-induced Precipitation Study: observations of dark and bright band phenomena
P. Di Girolamo1, D. Summa1, R. Bhawar1, T. Di Iorio2, E. G. Norton3, G. Peters4, and Y. Dufournet5
1Dipartimento di Ingegneria e Fisica dell'Ambiente, Università degli Studi della Basilicata, Potenza, Italy
2Dipartimento di Fisica, Università degli Studi di Roma "La Sapienza", Roma, Italy
3School of Earth, Atmospheric & Environmental Sciences, University of Manchester, Manchester, UK
4Meteorologisches Institut, Universität Hamburg, Hamburg, Germany
5Delft University of Technology, Delft, The Netherlands

Abstract. During the Convective and Orographically-induced Precipitation Study (COPS), lidar dark and bright bands were observed by the University of BASILicata Raman lidar system (BASIL) during several intensive (IOPs) and special (SOPs) observation periods (among others, 23 July, 15 August, and 17 August 2007). Lidar data were supported by measurements from the University of Hamburg cloud radar MIRA 36 (36 GHz), the University of Hamburg dual-polarization micro rain radars (24.1 GHz) and the University of Manchester UHF wind profiler (1.29 GHz). Results from BASIL and the radars for 23 July 2007 are illustrated and discussed to support the comprehension of the microphysical and scattering processes responsible for the appearance of the lidar and radar dark and bright bands. Simulations of the lidar dark and bright band based on the application of concentric/eccentric sphere Lorentz-Mie codes and a melting layer model are also provided. Lidar and radar measurements and model results are also compared with measurements from a disdrometer on ground and a two-dimensional cloud (2DC) probe on-board the ATR42 SAFIRE.

Citation: Di Girolamo, P., Summa, D., Bhawar, R., Di Iorio, T., Norton, E. G., Peters, G., and Dufournet, Y.: Lidar and radar measurements of the melting layer in the frame of the Convective and Orographically-induced Precipitation Study: observations of dark and bright band phenomena, Atmos. Chem. Phys. Discuss., 11, 30949-30987, doi:10.5194/acpd-11-30949-2011, 2011.
 
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