Development and evaluation of the BSC-DREAM8b dust regional model over Northern Africa, the Mediterranean and the Middle East

被引:167
作者
Basart, Sara [1 ]
Perez, Carlos [2 ,3 ]
Nickovic, Slodoban [4 ]
Cuevas, Emilio [5 ]
Maria Baldasano, Jose [1 ,6 ]
机构
[1] Barcelona Supercomp Ctr, Ctr Nacl Supercomp, Dept Earth Sci, Barcelona, Spain
[2] NASA, Goddard Inst Space Studies, New York, NY 10025 USA
[3] Columbia Univ, Dept Appl Phys & Appl Math, New York, NY USA
[4] World Meteorol Org, Geneva, Switzerland
[5] Meteorol State Agcy Spain AEMET, Izana Atmospher Res Ctr, Santa Cruz De Tenerife, Spain
[6] Tech Univ Catalonia, Environm Modelling Lab, Barcelona, Spain
来源
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY | 2012年 / 64卷
关键词
mineral dust; model simulation; model comparison; aerosol optical depth; seasonal variability; AEROSOL OPTICAL-PROPERTIES; STEP-MOUNTAIN COORDINATE; DESERT DUST; SAHARAN DUST; CHEMICAL-COMPOSITION; TRANSPORT; VARIABILITY; AERONET; CYCLE; DEPOSITION;
D O I
10.3402/tellusb.v64i0.18539
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The BSC-DREAM8b model and its predecessor are analysed in terms of aerosol optical depth (AOD) for 2004 over Northern Africa, the Mediterranean and the Middle East. We discuss the model performance and we test and analyse its behaviour with new components. The results are evaluated using hourly data from 44 AERONET stations and seasonally averaged satellite observations. The operational versions strongly underestimate the winter AOD over the Sahel and overestimate the AOD over the Middle East and the Mediterranean achieving a low average annual correlation (similar to 0.35). The use of a more detailed size distribution and a corrected wash-out ratio, together with a new dry deposition scheme, improves the transport over the Mediterranean, although underestimations remain over the Sahel and overestimations over the Middle East. The inclusion of a 'preferential source' mask improves the localisation of the main North African sources and consequently the dust transport towards Europe and the Atlantic. The use of a more physically based dust emission scheme and a new soil texture database leads to significant improvements in the representation of emissions and the transport over the Sahel, achieving an average annual correlation of 0.53. In this case, the use of a preferential source mask does not introduce significant improvements.
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页数:23
相关论文
共 107 条
[51]  
Liu M, 2000, MON WEATHER REV, V128, P1309, DOI 10.1175/1520-0493(2000)128<1309:NSOALL>2.0.CO
[52]  
2
[53]   Observed 20th century desert dust variability: impact on climate and biogeochemistry [J].
Mahowald, N. M. ;
Kloster, S. ;
Engelstaedter, S. ;
Moore, J. K. ;
Mukhopadhyay, S. ;
McConnell, J. R. ;
Albani, S. ;
Doney, S. C. ;
Bhattacharya, A. ;
Curran, M. A. J. ;
Flanner, M. G. ;
Hoffman, F. M. ;
Lawrence, D. M. ;
Lindsay, K. ;
Mayewski, P. A. ;
Neff, J. ;
Rothenberg, D. ;
Thomas, E. ;
Thornton, P. E. ;
Zender, C. S. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2010, 10 (22) :10875-10893
[54]   Aerosol modelling in MOCAGE and operational dust forecasting at Meteo-France [J].
Martet, M. ;
Peuch, V-H .
WMO/GEO EXPERT MEETING ON AN INTERNATIONAL SAND AND DUST STORM WARNING SYSTEM, 2009, 7
[55]   MODELING THE ATMOSPHERIC DUST CYCLE .1. DESIGN OF A SOIL-DERIVED DUST EMISSION SCHEME [J].
MARTICORENA, B ;
BERGAMETTI, G .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1995, 100 (D8) :16415-16430
[56]   Comparison of MISR and AERONET aerosol optical depths over desert sites [J].
Martonchik, JV ;
Diner, DJ ;
Kahn, R ;
Gaitley, B ;
Holben, BN .
GEOPHYSICAL RESEARCH LETTERS, 2004, 31 (16) :L161021-4
[57]   Sensitivity of hourly Saharan dust emissions to NCEP and ECMWF modeled wind speed [J].
Menut, Laurent .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2008, 113 (D16)
[58]  
MESINGER F, 1988, MON WEATHER REV, V116, P1493, DOI 10.1175/1520-0493(1988)116<1493:TSMCMD>2.0.CO
[59]  
2
[60]   Saharan dust: sources and trajectories [J].
Middleton, NJ ;
Goudie, AS .
TRANSACTIONS OF THE INSTITUTE OF BRITISH GEOGRAPHERS, 2001, 26 (02) :165-181