Dual-FOV Raman and Doppler lidar studies of aerosol-cloud interactions: Simultaneous profiling of aerosols, warm-cloud properties, and vertical wind

被引:26
作者
Schmidt, Joerg [1 ]
Ansmann, Albert [1 ]
Buehl, Johannes [1 ]
Baars, Holger [1 ]
Wandinger, Ulla [1 ]
Mueller, Detlef [2 ]
Malinka, Aleksey V. [3 ]
机构
[1] Leibniz Inst Tropospher Res, Leipzig, Germany
[2] Univ Hertfordshire, Sch Phys Astron & Math, Hatfield AL10 9AB, Herts, England
[3] Natl Acad Sci Belarus, BI Stepanov Inst Phys, Minsk, BELARUS
关键词
LIQUID WATER PATH; EFFECTIVE RADIUS; MICROWAVE RADIOMETERS; RADIATIVE PROPERTIES; BACKSCATTER LIDAR; ICE FORMATION; ART; RETRIEVAL; EXTINCTION; DISTRIBUTIONS;
D O I
10.1002/2013JD020424
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
For the first time, colocated dual-field of view (dual-FOV) Raman lidar and Doppler lidar observations (case studies) of aerosol and cloud optical and microphysical properties below and within thin layered liquid water clouds are presented together with an updraft and downdraft characterization at cloud base. The goal of this work is to investigate the relationship between aerosol load close to cloud base and cloud characteristics of warm (purely liquid) clouds and the study of the influence of vertical motions and turbulent mixing on this relationship. We further use this opportunity to illustrate the applicability of the novel dual-FOV Raman lidar in this field of research. The dual-FOV lidar combines the well-established multiwavelength Raman lidar technique for aerosol retrievals and the multiple-scattering Raman lidar technique for profiling of the single-scattering extinction coefficient, effective radius, number concentration of the cloud droplets, and liquid water content. Key findings of our 3 year observations are presented in several case studies of optically thin altocumulus layers occurring in the lower free troposphere between 2.5 and 4 km height over Leipzig, Germany, during clean and polluted situations. For the clouds that we observed, the most direct link between aerosol proxy (particle extinction coefficient) and cloud proxy (cloud droplet number concentration) was found at cloud base during updraft periods. Above cloud base, additional processes resulting from turbulent mixing and entrainment of dry air make it difficult to determine the direct impact of aerosols on cloud processes.
引用
收藏
页码:5512 / 5527
页数:16
相关论文
共 68 条
[1]   Ice formation in Saharan dust over central Europe observed with temperature/humidity//aerosol Raman lidar -: art. no. D18S12 [J].
Ansmann, A ;
Mattis, I ;
Müller, D ;
Wandinger, U ;
Radlach, M ;
Althausen, D ;
Damoah, R .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2005, 110 (D18) :1-12
[2]   COMBINED RAMAN ELASTIC-BACKSCATTER LIDAR FOR VERTICAL PROFILING OF MOISTURE, AEROSOL EXTINCTION, BACKSCATTER, AND LIDAR RATIO [J].
ANSMANN, A ;
RIEBESELL, M ;
WANDINGER, U ;
WEITKAMP, C ;
VOSS, E ;
LAHMANN, W ;
MICHAELIS, W .
APPLIED PHYSICS B-PHOTOPHYSICS AND LASER CHEMISTRY, 1992, 55 (01) :18-28
[3]   MEASUREMENT OF ATMOSPHERIC AEROSOL EXTINCTION PROFILES WITH A RAMAN LIDAR [J].
ANSMANN, A ;
RIEBESELL, M ;
WEITKAMP, C .
OPTICS LETTERS, 1990, 15 (13) :746-748
[4]   Evolution of the ice phase in tropical altocumulus: SAMUM lidar observations over Cape Verde [J].
Ansmann, A. ;
Tesche, M. ;
Seifert, P. ;
Althausen, D. ;
Engelmann, R. ;
Fruntke, J. ;
Wandinger, U. ;
Mattis, I. ;
Mueller, D. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2009, 114
[5]  
Ansmann A., 2005, Lidar. Range-Resolved Optical Remote Sensing of the Atmosphere, P105, DOI [10.1007/0-387-25101-4_4, DOI 10.1007/0-387-25101-4_4]
[6]  
Bissonnette L.R., 2005, LIDAR RANGE RESOLVED, P43, DOI DOI 10.1007/0-387-25101-4_3
[7]   Multiple-scattering lidar retrieval method:: tests on Monte Carlo simulations and comparisons with in situ measurements [J].
Bissonnette, LR ;
Roy, G ;
Poutier, L ;
Cober, SG ;
Isaac, GA .
APPLIED OPTICS, 2002, 41 (30) :6307-6324
[8]   MULTIPLY SCATTERED AEROSOL LIDAR RETURNS - INVERSION METHOD AND COMPARISON WITH IN-SITU MEASUREMENTS [J].
BISSONNETTE, LR ;
HUTT, DL .
APPLIED OPTICS, 1995, 34 (30) :6959-6975
[9]  
Brenguier JL, 2000, J ATMOS SCI, V57, P803, DOI 10.1175/1520-0469(2000)057<0803:RPOBLC>2.0.CO
[10]  
2