African dust source regions for observed dust outbreaks over the Subtropical Eastern North Atlantic region, above 25°N

被引:29
作者
Alonso-Perez, S. [1 ,2 ]
Cuevas, E. [1 ]
Querol, X. [2 ]
Guerra, J. C. [3 ]
Perez, C. [4 ,5 ]
机构
[1] Izana Atmospher Res Ctr AEMET, Santa Cruz De Tenerife 38071, Spain
[2] Inst Environm Assessment & Water Res CSIC, Barcelona 08028, Spain
[3] Univ La Laguna, Atmospher Phys Lab, Tenerife 38200, Spain
[4] Columbia Univ, Earth Inst, NASA Goddard Inst Space Studies, New York, NY 10025 USA
[5] Int Res Inst Climate & Soc, New York, NY 10025 USA
关键词
Aerosols; African dust; Marine Boundary Layer; Dust sources; Residence time; HYSPLIT; LONG-RANGE TRANSPORT; SAHARAN DUST; MINERAL-DUST; CANARY-ISLANDS; ATMOSPHERIC TRANSPORT; ELEMENTAL COMPOSITION; CHEMICAL-COMPOSITION; SUSPENDED PARTICLES; OPTICAL-THICKNESS; AEROSOL;
D O I
10.1016/j.jaridenv.2011.11.013
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
High mineral dust-laden air mass potential source regions affecting the Marine Boundary Layer (MBL) of the Subtropical Eastern North Atlantic Region above 25 degrees N (SENAR), directly or by means of gravitational settlement, were objectively identified. We introduced a new hybrid Lagrangian-Eulerian receptor model, in which air mass residence time probability maps in the geographical domain latitude = [5 degrees N, 60 degrees N], longitude = [70 degrees W, 30 degrees E] were combined with TOMS-AI data (TAPI Index), and with simulated Total Suspended Particles (TSP) with the BSC/DREAM model (SDPI Index). Both approaches show a good agreement. For dust gravitational settlement episodes within the MBL, the dust sources are located in southernmost latitudes compared to those associated with lower air mass transport. A seasonal variability in potential dust sources is found with both approaches, TAPI and SDPI. In winter, most dust sources are located within the Sahara in an area bounded by latitude = [18 degrees N, 35 degrees N], longitude = [15 degrees W, 15 degrees E]. In summer, a high dust-laden air mass reservoir above the Atlantic Ocean has been found during episodes for low altitudes, and dust source regions in the Sahara have been identified for middle and upper altitudes. The Bodele depression was found to have a minor impact on dust outbreaks affecting the SENAR. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:100 / 109
页数:10
相关论文
共 91 条
[1]   Characterisation of TSP and PM2.5 at Izana and Sta. Cruz de Tenerife (Canary Islands, Spain) during a Saharan Dust Episode (July 2002) [J].
Alastuey, A ;
Querol, X ;
Castillo, S ;
Escudero, M ;
Avila, A ;
Cuevas, E ;
Torres, C ;
Romero, PM ;
Exposito, F ;
García, O ;
Diaz, JP ;
Van Dingenen, R ;
Putaud, JP .
ATMOSPHERIC ENVIRONMENT, 2005, 39 (26) :4715-4728
[2]   Impact of the Saharan dust outbreaks on the ambient levels of total suspended particles (TSP) in the marine boundary layer (MBL) of the Subtropical Eastern North Atlantic Ocean [J].
Alonso-Perez, S. ;
Cuevas, E. ;
Querol, X. ;
Viana, M. ;
Guerra, J. C. .
ATMOSPHERIC ENVIRONMENT, 2007, 41 (40) :9468-9480
[3]  
Alonso-Perez S., 2008, CARACTERIZACION INTR
[4]   Vertical distribution of Saharan dust based on 2.5-year model predictions [J].
Alpert, P ;
Kishcha, P ;
Shtivelman, A ;
Krichak, SO ;
Joseph, JH .
ATMOSPHERIC RESEARCH, 2004, 70 (02) :109-130
[5]   A STATISTICAL TRAJECTORY TECHNIQUE FOR DETERMINING AIR-POLLUTION SOURCE REGIONS [J].
ASHBAUGH, LL .
JOURNAL OF THE AIR POLLUTION CONTROL ASSOCIATION, 1983, 33 (11) :1096-1098
[6]   AFRICAN DUST OBSERVED OVER CANARY ISLANDS - SOURCE-REGIONS IDENTIFICATION AND TRANSPORT PATTERN FOR SOME SUMMER SITUATIONS [J].
BERGAMETTI, G ;
GOMES, L ;
COUDEGAUSSEN, G ;
ROGNON, P ;
LECOUSTUMER, MN .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1989, 94 (D12) :14855-14864
[7]   Seasonal variability of the elemental composition of atmospheric aerosol particles over the northwestern Mediterranean [J].
Bergametti, Gilles ;
Dutot, Alain-Louis ;
Buat-Menard, Patrick ;
Losno, Remi ;
Remoudaki, Emmanouela .
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 1989, 41 (03) :353-361
[8]  
Blanco A., 2003, Atmos. Chem. Phys. Discuss, V3, P1
[9]  
Bonelli P, 1996, ENVIR SCI TECH LIB, V11, P275
[10]   Saharan dust episodes in Hungarian aerosol:: elemental signatures and transport trajectories [J].
Borbély-Kiss, I ;
Kiss, AZ ;
Koltay, E ;
Szabó, G ;
Bozó, L .
JOURNAL OF AEROSOL SCIENCE, 2004, 35 (10) :1205-1224