Diagnostic study of spring dusty days over the southwest region of the Kingdom of Saudi Arabia

被引:18
作者
Awad, Adel M. [1 ]
Mashat, Abdul-Wahab S. [1 ]
Salem, Faisal F. Abo [1 ]
机构
[1] King Abdulaziz Univ, Dept Meteorol, Jeddah 21413, Saudi Arabia
关键词
TOMS Aerosol Index; Spring dust; Dust classes; Saudi Arabia; SYNOPTIC ANALYSIS; NORTH-AFRICA; MIDDLE-EAST; MODEL; REANALYSIS; AEROSOLS; STORMS; PENINSULA; TRANSPORT; EVENT;
D O I
10.1007/s12517-014-1318-x
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Three classes of dust over the southwest region of the Kingdom of Saudi Arabia were classified based on both the values and distribution of the TOMS Aerosol Index. These classes include a narrow spread class (i.e., a weak class), a moderate spread class, and a wide spread class (i.e., a strong class). A diagnostic study of these classes indicated that there are common atmospheric features for dust cases, and the intensity of these features increases with the characteristic strength of the dust cases. These features are the horizontal circulation of anticyclonic wind flow associated with lower layer upward motion through the zonal stripe between 17A degrees N and 25A degrees N through the meridional cross-section in addition to a vertical circulation, especially for the layers above 850 hPa. These two circulation patterns merge to form an unstable atmosphere and a deep cyclone. Furthermore, there are areas of convergence and divergence at the points of deepening upward motion and shallow upward motion, respectively. Finally, all these features collectively force the dust from the Arabian Desert to move into the southwest region of the Kingdom of Saudi Arabia.
引用
收藏
页码:2265 / 2282
页数:18
相关论文
共 41 条
[21]  
Kim D., 2011, ATMOS CHEM PHYS DISC, V11, P20181
[22]   Characteristics of Asian dust transport based on synoptic meteorological analysis over Korea [J].
Kim, YK ;
Song, SK ;
Lee, HW ;
Kim, CH ;
Oh, IB ;
Moon, YS ;
Shon, ZH .
JOURNAL OF THE AIR & WASTE MANAGEMENT ASSOCIATION, 2006, 56 (03) :306-316
[23]   Atmospheric response to Saharan dust deduced from ECMWF reanalysis (ERA) temperature increments [J].
Kishcha, P ;
Alpert, P ;
Barkan, J ;
Kirchner, I ;
Machenhauer, B .
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2003, 55 (04) :901-913
[24]  
Kistler R, 2001, B AM METEOROL SOC, V82, P247, DOI 10.1175/1520-0477(2001)082<0247:TNNYRM>2.3.CO
[25]  
2
[26]   Dust storms in the Middle East: Sources of origin and their temporal characteristics [J].
Kutiel, H ;
Furman, H .
INDOOR AND BUILT ENVIRONMENT, 2003, 12 (06) :419-426
[27]   Impact of the March 2009 dust event in Saudi Arabia on aerosol optical properties, meteorological parameters, sky temperature and emissivity [J].
Maghrabi, A. ;
Alharbi, B. ;
Tapper, N. .
ATMOSPHERIC ENVIRONMENT, 2011, 45 (13) :2164-2173
[28]   Interannual variability in atmospheric mineral aerosols from a 22-year model simulation and observational data [J].
Mahowald, N ;
Luo, C ;
del Corral, J ;
Zender, CS .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D12)
[29]  
Mashat A., 2010, B FS CAIRO U, V78, P1
[30]   DUST STORMS IN THE MIDDLE-EAST [J].
MIDDLETON, NJ .
JOURNAL OF ARID ENVIRONMENTS, 1986, 10 (02) :83-96