Transport of dust particles from the Bodele region to the monsoon layer - AMMA case study of the 9-14 June 2006 period

被引:22
作者
Crumeyrolle, S. [1 ,2 ]
Tulet, P. [2 ,3 ]
Gomes, L. [2 ]
Garcia-Carreras, L. [4 ]
Flamant, C. [5 ]
Parker, D. J. [4 ]
Matsuki, A. [1 ,6 ]
Formenti, P. [7 ,8 ]
Schwarzenboeck, A. [1 ]
机构
[1] Univ Blaise Pascal, Lab Meteorol Phys, UMR 6016, Clermont Ferrand, France
[2] Meteo France, GAME, Ctr Natl Rech Meteorol, Toulouse, France
[3] Univ La Reunion, LACy, St Denis, France
[4] Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England
[5] CNRS UPMC UVSQ, LATMOS IPSL, Paris, France
[6] Kanazawa Univ, Frontier Sci Org, Kanazawa, Ishikawa 9201192, Japan
[7] Univ Paris 12, LISA IPSL, CNRS, UMR 6240, Creteil, France
[8] Univ Paris 07, LISA IPSL, CNRS, UMR 6240, Creteil, France
关键词
MESOSCALE CONVECTIVE SYSTEM; LAND-SURFACE PARAMETERS; SAHARAN DUST; INTERTROPICAL DISCONTINUITY; AEROSOL CHARACTERIZATION; BOUNDARY-LAYER; DIURNAL CYCLE; MINERAL DUST; MODEL; SCHEME;
D O I
10.5194/acp-11-479-2011
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Aerosol properties were measured during an airborne campaign experiment that took place in June 2006 in West Africa within the framework of the African Monsoon Multidisciplinary Analyses (AMMA). The goal of the present study was to investigate a dynamical mechanism able to facilitate the sedimentation of dust particles from the Saharan Air Layer (SAL) into the boundary layer. A significant change in the dust particle concentration measured along the meridian between Niamey (Niger) and Cotonou (Benin) was found in the boundary layer (similar to 700 m), where the dust particle concentration increased in a zone where local emission is not possible. Moreover, the boundary layer top observed with the dropsondes launched with the F-F20 shows a strong relationship with the surface cover anomalies, with higher Boundary Layer (BL) tops over the warmer surfaces, such as croplands, as opposed to adjacent forest. A mesoscale atmospheric model with a new on-line dust parameterization, resulting from the Alfaro and Gomes (2001) parametrisation and AMMA observations, was used to interpret the impact of vegetation anomalies on dust particle sedimentation. The results of the simulation are consistent with the observations, with higher dust concentration over the warm surface cover anomalies.
引用
收藏
页码:479 / 494
页数:16
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