Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science & Technology, Nanjing 210044, China.
J Environ Sci (China). 2019 Feb;76:154-166. doi: 10.1016/j.jes.2018.04.019. Epub 2018 Apr 27.
This study presents detailed analysis of spatiotemporal variations and trend of dust optical properties i.e., Aerosol Optical Depth (AOD) and Angstrom component over Asian desert regions using thirteen years of data (i.e., 2001-2013) retrieved from Aerosol Robotic Network (AERONET), Moderate Resolution Imaging Spectroradiometer (MODIS) and Multi-angle Imaging Spectroradiometer (MISR). These regions include Solar Village, Dunhuang and Dalangzadgad and are considered as origin of desert aerosols in Asia. Mann-Kendall trend test was used to show the trend of AOD. The relationship of AOD with weather parameters and general AOD trend over different wavelengths has also been shown. AOD's trend has been observed significant throughout the year in Solar Village, while in Dunhuang and Dalanzadgad the significant trend has been found only in peak period (March-June). Analysis show high values of AOD and low values of angstrom in Solar Village during peak period. In Chinese desert regions, high values of AOD have been found during peak period and low values in pre-peak period. Significant relationship has been observed between AOD and average temperature in Solar Village and Dalanzadgad whereas rainfall and wind speed showed no significant impact on AOD in all desert regions.
本研究利用十三年(2001-2013 年)的气溶胶机器人网络(AERONET)、中分辨率成像光谱仪(MODIS)和多角度成像光谱仪(MISR)数据,对亚洲沙漠地区的时空变化和尘埃光学特性(即气溶胶光学深度(AOD)和 Angstrom 分量)进行了详细分析。这些地区包括太阳村、敦煌和达兰扎德嘎德,被认为是亚洲沙漠气溶胶的发源地。Mann-Kendall 趋势检验用于显示 AOD 的趋势。还显示了 AOD 与天气参数的关系以及不同波长上的总体 AOD 趋势。在太阳村,AOD 的趋势全年都很显著,而在敦煌和达兰扎德嘎德,只有在高峰期(3 月至 6 月)才发现显著趋势。分析表明,在高峰期,太阳村的 AOD 值较高,Angstrom 值较低。在中国沙漠地区,高峰期的 AOD 值较高,高峰期前的 AOD 值较低。在太阳村和达兰扎德嘎德,AOD 与平均温度之间存在显著关系,而在所有沙漠地区,降雨和风速对 AOD 没有显著影响。