The vertical distribution of aerosol over Europe -: synthesis of one year of EARLINET aerosol lidar measurements and aerosol transport modeling with LMDzT-INCA

被引:41
作者
Guibert, S [1 ]
Matthias, V
Schulz, M
Bösenberge, J
Eixmann, R
Mattis, I
Pappalardo, G
Perroneg, MR
Spinelli, N
Vaughan, G
机构
[1] CEA, CNRS, IPSL, LSCE, F-91191 Gif Sur Yvette, France
[2] GKSS Forschungszentrum Geesthacht GmbH, Inst Coastal Res, Geesthacht, Germany
[3] Max Planck Inst Meteorol, Hamburg, Germany
[4] Leibniz Inst ATmospharenphys, Kuhlungsborn, Germany
[5] Leibniz Inst Tropospharenforsch, Leipzig, Germany
[6] CNR, Ist Metodol Anal Ambientale, Potenza, Italy
[7] Univ Lecce, Dipartimento Fis, I-73100 Lecce, Italy
[8] Univ Naples Federico II, Ist Nazl Fis Mat, Naples, Italy
[9] Univ Naples Federico II, Dipartimento Sci Fisiche, Naples, Italy
[10] Univ Wales, Dept Phys, Aberystwyth, Dyfed, Wales
关键词
aerosol extinction; vertical profiles; aerosol composition; Saharan dust; GCM;
D O I
10.1016/j.atmosenv.2004.12.046
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Aerosol extinction vertical profiles measured with Raman lidar in the framework of EARLINET in 2000 are compared to profiles modeled by a general circulation model, LMDzT-INCA, at seven stations in Europe. Comparisons based on individual profiles show moderate correlation between model and data. Averaging aerosol extinction values on larger temporal or spatial scales improves the comparison. Furthermore, we show that the model succeeds to reproduce the mean annual aerosol distribution over Europe. Comparisons of the aerosol vertical distribution in two distinct regions of Europe are presented. For the northern stations, the observed yearly average aerosol extinction coefficient vertical profile and the modeled one show an average bias of 22%. For the southern stations the mean bias is slightly higher (29%). Both model and lidar show different extinction profiles in different parts of Europe, with higher values in upper heights in the South. According to modeled profiles of each aerosol component, this is caused by the presence of dust at altitudes between 2 and 6 km. In addition vertical mixing in the South seems to be more effective for the other aerosol components. (c) 2005 Elsevier Ltd. All rights reserved.
引用
收藏
页码:2933 / 2943
页数:11
相关论文
共 31 条
  • [1] MEASUREMENT OF ATMOSPHERIC AEROSOL EXTINCTION PROFILES WITH A RAMAN LIDAR
    ANSMANN, A
    RIEBESELL, M
    WEITKAMP, C
    [J]. OPTICS LETTERS, 1990, 15 (13) : 746 - 748
  • [2] Balkanski Y., 2003, EMISSION ATMOSPHERIC, P253
  • [3] Global modeling of heterogeneous chemistry on mineral aerosol surfaces: Influence on tropospheric ozone chemistry and comparison to observations
    Bauer, SE
    Balkanski, Y
    Schulz, M
    Hauglustaine, DA
    Dentener, F
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2004, 109 (D2)
  • [4] Bosenberg J., 2003, 348 MAX PLANCK I MET
  • [5] Bosenberg J., 2001, 317 MAX PLANCK I MET
  • [6] Boucher O., 2002, Simulation of the atmospheric sulfur cycle in the Laboratoire de Meteorologie Dynamique General Circulation Model: Model description, model evaluation, and global and European budgets
  • [7] CLIMATE FORCING BY ANTHROPOGENIC AEROSOLS
    CHARLSON, RJ
    SCHWARTZ, SE
    HALES, JM
    CESS, RD
    COAKLEY, JA
    HANSEN, JE
    HOFMANN, DJ
    [J]. SCIENCE, 1992, 255 (5043) : 423 - 430
  • [8] SENSITIVITY OF THE BACKSCATTER EXTINCTION RATIO TO CHANGES IN AEROSOL PROPERTIES - IMPLICATIONS FOR LIDAR
    EVANS, BTN
    [J]. APPLIED OPTICS, 1988, 27 (15): : 3299 - 3305
  • [9] ANALYSIS OF ATMOSPHERIC LIDAR OBSERVATIONS - SOME COMMENTS
    FERNALD, FG
    [J]. APPLIED OPTICS, 1984, 23 (05): : 652 - 653
  • [10] Improving the seasonal cycle and interannual variations of biomass burning aerosol sources
    Generoso, S
    Bréon, FM
    Balkanski, Y
    Boucher, O
    Schulz, M
    [J]. ATMOSPHERIC CHEMISTRY AND PHYSICS, 2003, 3 : 1211 - 1222