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Aerosol optical properties over Ebinur region in spring |
ZHANG Zhe1,2, DING Jian-li1,2, WANG Jin-jie1,2,3 |
1. College of Resources and Environment Science, Xinjiang University, Urumqi 830046, China; 2. China Key Laboratory of Oasis Ecosystem of Education Ministry, Xinjiang University, Urumqi 830046, China; 3. Xingjiang Vocational and Technical College of Communication, Urumqi 831401, China |
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Abstract Microtops II sun photometers were used to retrieve data on the aerosol optical depth (AOD550) and Angström wavelength exponent (α) over Ebinur Lake region in spring. The results showed that high frequency value of AOD mainly concentrated in 0.1~0.4Affected by diffusion and sedimentation of salt dust, there were some differences in the aerosol optical properties between Jinghe and Wusu region. The mean values of AOD in Jinghe and Wusu were 0.290 and 0.242 with coefficients of variation were 62.966%, 47.444%, the mean values of α were 0.609 and 0.894 with coefficients of variation were 33.368% and 56.946%, it showed that atmospheric aerosol particle size was relatively large in Jinghe and the particle size of aerosol particles changed significantly in Wusu region; It had a complex relationship between AOD and α; the local dominant wind was the leading factor of dust aerosols. Temperature not played a critical role in the local changes of AOD. When α <0.5, AOD and RH showed a negative correlation in Wusu, while Jinghe area showed a hygroscopic due to the impact of soluble ions in salt dust. When α>1.0, the hygroscopic growth of fine particles lead to AOD and RH showed a positive correlation trend, When 0.5 < α < 1.0, aerosol showed a certain hygroscopic, while when RH>50%, it was not surprising that rainfall lead to reduced aerosol concentration. The results showed that the high AOD in Jinghe mainly caused by the dust aerosols and the high AOD in Wusu both clustering in the fine mode growth wing and the coarse mode.
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Received: 23 June 2016
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[1] |
Kristjánsson J E, Iversen T, Kirkevåg A, et al. Response of the climate system to aerosol direct and indirect forcing:Role of cloud feedbacks[J]. Journal of Geophysical Research, 2005, 110(D24):D24206.
|
[2] |
王静,牛生杰,许丹,等.南京一次典型雾霾天气气溶胶光学特性[J]. 中国环境科学, 2013,33(2):201-208.
|
[3] |
刘唯佳,韩永翔,王静,等.北京2010年10月一次典型灰霾过程光学特性分析[J]. 中国环境科学, 2015,35(7):1931-1937.
|
[4] |
Smirnov A, Holben B N, Kaufman Y J, et al. Optical properties of atmospheric aerosol in maritime environments[J]. Journal of the Atmospheric Sciences, 2002,59(3):501-523.
|
[5] |
赵胡笳,马雁军,王扬锋,等.沈阳一次雾霾天气颗粒物浓度及光学特征变化[J]. 中国环境科学, 2015,35(5):1288-1296.
|
[6] |
刘东伟,吉力力·阿不都外力,雷加强,等.盐尘暴及其生态效应[J]. 中国沙漠, 2011,31(1):168-173.
|
[7] |
Blank R R, Young J A, Allen F L. Aeolian dust in a saline playa environment, Nevada, USA[J]. Journal of Arid Environments, 1999,41(4):365-381.
|
[8] |
Argaman E, Singer T H. Erodibility of some crust-forming soil sediments from the southern Aral sea basin as determined in a wind tunnel[J]. Earth Surface Processes and Landforms, 2006, 31:47-63.
|
[9] |
Mees F, Singer A. Surface crusts on soil sediment of southern Aral Sea Basin, Uzbekistan[J]. Geoderma, 2006,136:152-159.
|
[10] |
葛拥晓,吉力力·阿不都外力,刘东伟,等.艾比湖干涸湖底6种景观类型不同深度富盐沉积物粒径的分形特征[J]. 中国沙漠, 2013,33(3):804-812.
|
[11] |
Abuduwaili J, Mu G J. Eolian factor in the process of salt accumulation in the west Dzungaria, China[J]. Eurasian Soil Science, 2006,39(4):367-376.
|
[12] |
张勇,银燕,刘藴芳,等.北京秋季大气气溶胶光学厚度与Angstrom指数观测研究[J]. 中国环境科学, 2014,34(6):1380-1389.
|
[13] |
齐冰,杜荣光,于之锋,等.杭州市大气气溶胶光学厚度研究[J]. 中国环境科学, 2014,34(3):588-595.
|
[14] |
吕睿,于兴娜,沈丽,等.北京春季大气气溶胶光学特性研究[J]. 中国环境科学, 2016,36(6):1660-1668.
|
[15] |
于兴娜,李新妹,登增然登,等.北京雾霾天气期间气溶胶光学特性[J]. 环境科学, 2012,33(4):1057-1062.
|
[16] |
王跃思,辛金元,李占清,等.中国地区大气气溶胶光学厚度与Angstrom参数联网观测(2004-08-2004-12)[J]. 环境科学, 2006,27(9):1703-1711.
|
[17] |
饶加旺,马荣华,段洪涛,等.太湖上空大气气溶胶光学厚度及其特征分析[J]. 环境科学, 2012,33(7):2158-2164.
|
[18] |
吉力力·阿不都外力,徐俊荣,穆桂金,等.艾比湖盐尘对周边地区土壤盐分及景观变化的影响[J]. 冰川冻土, 2007,29(6):928-939.
|
[19] |
鄢雪英.基于空间信息技术的盐碱尘暴信息提取-以艾比湖地区为例[D]. 乌鲁木齐:新疆大学, 2014.
|
[20] |
毕雪岩,吴兑,谭浩波,等.MicrotopsⅡ型太阳光度计的使用、计算及定标[J]. 气象科技, 2007,35(4):583-588.
|
[21] |
Dubovik O, Holben B N, Eck T F, et al. Variability of absorption and optical properties of key aerosol types observed in worldwide locations[J]. Journal of the Atmospheric Sciences, 2002,59(3):590-608.
|
[22] |
Kim D H, Sohn B J, Nakajima T, et al. Aerosol optical propertiesover east Asia determined from ground-based sky radiation measurements[J]. Journal of Geophysical Research, 2004,109:D02209.
|
[23] |
Tanré D, Kaufman Y J, Holben B N, et al. Climatology of dust aerosol size distribution and optical properties derived from remotely sensed data in the solar spectrum[J]. Journal of Geophysical Research, 2001,106(D16):18205-18217.
|
[24] |
鲁如坤.土壤农业化学分析方法[M]. 北京:中国农业科技出版社, 2000.
|
[25] |
Gobbi G P, Kaufman Y J, Koren I, et al. Classification of aerosol properties derived from AERONET direct sun data[J]. Atmospheric Chemistry and Physics, 2007,7(2):453-458.
|
|
|
|