Saharan dust absorption and refractive index from aircraft-based observations during SAMUM 2006

被引:134
作者
Petzold, Andreas [1 ]
Rasp, Katharina [1 ]
Weinzierl, Bernadett [1 ]
Esselborn, Michael [1 ]
Hamburger, Thomas [1 ]
Doernbrack, Andreas [1 ]
Kandler, Konrad [2 ]
Schuetz, Lothar [3 ]
Knippertz, Peter [3 ]
Fiebig, Markus [4 ]
Virkkula, Aki [5 ]
机构
[1] Deutsch Zentrum Luft & Raumfahrt, Inst Phys Atmosphare, Oberpfaffenhofen, Wessling, Germany
[2] Tech Univ Darmstadt, Appl Geosci Dept, D-64287 Darmstadt, Germany
[3] Johannes Gutenberg Univ Mainz, Inst Atmospher Phys, D-55099 Mainz, Germany
[4] Norwegian Inst Air Res, Dept Atmospher & Climate Res, Kjeller, Norway
[5] Finnish Meteorol Inst, FIN-00101 Helsinki, Finland
关键词
PARTICLE-SIZE DISTRIBUTION; AIRBORNE MINERAL AEROSOLS; RADIATIVE PROPERTIES; OPTICAL-PROPERTIES; LIGHT-ABSORPTION; SENSITIVITY; WAVELENGTHS; CALIBRATION; SCATTERING; SHADE;
D O I
10.1111/j.1600-0889.2008.00383.x
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
During the Saharan Mineral Dust Experiment (SAMUM) conducted in summer 2006 in southeast Morocco, the complex refractive index of desert dust was determined from airborne measurements of particle size distributions and aerosol absorption coefficients at three different wavelengths in the blue (467 nm), green (530 nm) and red (660 nm) spectral regions. The vertical structure of the dust layers was analysed by an airborne high spectral resolution lidar (HSRL). The origin of the investigated dust layers was estimated from trajectory analyses, combined with Meteosat 2nd Generation (MSG) scenes and wind field data analyses. The real part n of the dust refractive index was found almost constant with values between 1.55 and 1.56, independent of the wavelength. The values of the imaginary part k varied between the blue and red spectral regions by a factor of three to ten depending on the dust source region. Absolute values of k ranged from 3.1 x 10(-3) to 5.2 x 10(-3) at 450 nm and from 0.3 x 10(-3) to 2.5 x 10(-3) at 700 nm. Groupings of k values could be attributed to different source regions.
引用
收藏
页码:118 / 130
页数:13
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