Airborne measurements of dust layer properties, particle size distribution and mixing state of Saharan dust during SAMUM 2006

被引:149
作者
Weinzierl, Bernadett [1 ]
Petzold, Andreas [1 ]
Esselborn, Michael [1 ]
Wirth, Martin [1 ]
Rasp, Katharina [1 ]
Kandler, Konrad [2 ]
Schuetz, Lothar [3 ]
Koepke, Peter [4 ]
Fiebig, Markus [5 ]
机构
[1] Deutsch Zentrum Luft & Raumfahrt, Inst Phys Atmosphare, D-82234 Oberpfaffenhofen, Wessling, Germany
[2] Tech Univ Darmstadt, Inst Angew Geowissensch, D-64287 Darmstadt, Germany
[3] Johannes Gutenberg Univ Mainz, Inst Phys Atmosphare, D-55099 Mainz, Germany
[4] Univ Munich, Inst Meteorol, D-80333 Munich, Germany
[5] Norwegian Inst Air Res NILU, Dept Atmospher & Climate Res, N-2027 Kjeller, Norway
来源
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY | 2009年 / 61卷 / 01期
关键词
OPTICAL-PROPERTIES; DESERT DUST; MINERAL AEROSOL; C-130; AIRCRAFT; PUERTO-RICO; SCATTERING; LIGHT; ABSORPTION; FSSP-300; NUMBER;
D O I
10.1111/j.1600-0889.2008.00392.x
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The Saharan Mineral Dust Experiment (SAMUM) was conducted in May/June 2006 in southern Morocco. As part of SAMUM, airborne in situ measurements of the particle size distribution in the diameter range 4 nm < D-p < 100 mu m were conducted. The aerosol mixing state was determined below D-p < 2.5 mu m. Furthermore, the vertical structure of the dust layers was investigated with a nadir-looking high spectral resolution lidar (HSRL). The desert dust aerosol exhibited two size regimes of different mixing states: below 0.5 mu m, the particles had a non-volatile core and a volatile coating; larger particles above 0.5 mu m consisted of non-volatile components and contained light absorbing material. In all cases, particles larger than 10 mu m were present, and in 80% of the measurements no particles larger than 40 mu m were present. The abundance of large particles showed almost no height dependence. The effective diameter D-eff in the dust plumes investigated showed two main ranges: the first range of D-eff peaked around 5 mu m and the second range of D-eff around 8 mu m. The two ranges of D-eff suggest that it may be inadequate to use one average effective diameter or one parametrization for a typical dust size distribution.
引用
收藏
页码:96 / 117
页数:22
相关论文
共 61 条
[41]  
PETZOLD A, 2008, TELLUS B, V61
[42]  
RASP K, 2007, THESIS LUDWIG MACIMI
[43]   Analysis of measurements of Saharan dust by airborne and ground-based remote sensing methods during the Puerto Rico Dust Experiment (PRIDE) -: art. no. 8586 [J].
Reid, JS ;
Kinney, JE ;
Westphal, DL ;
Holben, BN ;
Welton, EJ ;
Tsay, SC ;
Eleuterio, DP ;
Campbell, JR ;
Christopher, SA ;
Colarco, PR ;
Jonsson, HH ;
Livingston, JM ;
Maring, HB ;
Meier, ML ;
Pilewskie, P ;
Prospero, JM ;
Reid, EA ;
Remer, LA ;
Russell, PB ;
Savoie, DL ;
Smirnov, A ;
Tanré, D .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D19)
[44]   Comparison of size and morphological measurements of coarse mode dust particles from Africa [J].
Reid, JS ;
Jonsson, HH ;
Maring, HB ;
Smirnov, A ;
Savoie, DL ;
Cliff, SS ;
Reid, EA ;
Livingston, JM ;
Meier, MM ;
Dubovik, O ;
Tsay, SC .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D19)
[45]   Desert dust suppressing precipitation: A possible desertification feedback loop [J].
Rosenfeld, D ;
Rudich, Y ;
Lahav, R .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2001, 98 (11) :5975-5980
[46]   Aircraft measurements of sub micrometer aerosol particles (>7 nm) in the midlatitude free troposphere and tropopause region [J].
Schroder, F ;
Strom, J .
ATMOSPHERIC RESEARCH, 1997, 44 (3-4) :333-356
[47]  
SCHUTZ L, 1974, J APPL METEOROL, V13, P863, DOI 10.1175/1520-0450(1974)013<0863:PNAMDA>2.0.CO
[48]  
2
[49]   Modeling the radiative characteristics of airborne mineral aerosols at infrared wavelengths [J].
Sokolik, IN ;
Toon, OB ;
Bergstrom, RW .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1998, 103 (D8) :8813-8826
[50]   Introduction to special section: Outstanding problems in quantifying the radiative impacts of mineral dust [J].
Sokolik, IN ;
Winker, DM ;
Bergametti, G ;
Gillette, DA ;
Carmichael, G ;
Kaufman, YJ ;
Gomes, L ;
Schuetz, L ;
Penner, JE .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2001, 106 (D16) :18015-18027