Key Laboratory of Atmospheric Chemistry of CMA, Institute of Atmospheric Composition, Chinese Academy of Meteorological Sciences, Beijing 100081, China; College of Earth Science, University of Chinese Academy of Sciences, Beijing 100081, China; National Meteorological Center, CMA, Beijing 100081, China.
Key Laboratory of Atmospheric Chemistry of CMA, Institute of Atmospheric Composition, Chinese Academy of Meteorological Sciences, Beijing 100081, China.
Sci Total Environ. 2018 Aug 15;633:452-462. doi: 10.1016/j.scitotenv.2018.03.068. Epub 2018 Mar 28.
We analyzed the frequency and intensity of sand and dust storms (SDSs) in East Asia from 2007 to 2016 using observational data from ground stations, numerical modeling, and vegetation indices obtained from both satellite and reanalysis data. The relationships of SDSs with surface conditions and the synoptic circulation pattern were also analyzed. The statistical analyses demonstrated that the number and intensity of SDS events recorded in spring during 2007 to 2016 showed a decreasing trend. The total number of spring SDSs decreased from at least ten events per year before 2011 to less than ten events per year after 2011. The overall average annual variation of the surface dust concentration in the main dust source regions decreased 33.24μg/m (-1.75%) annually. The variation in the temperatures near and below the ground surface and the amount of precipitation and soil moisture all favored an improvement in vegetation coverage, which reduced the intensity and frequency of SDSs. The strong winds accompanying the influx of cold air from high latitudes showed a decreasing trend, leading to a decrease in the number of SDSs and playing a key role in the decadal decrease of SDSs. The decrease in the intensity of the polar vortex during study period was closely related to the decrease in the intensity and frequency of SDSs.
我们利用地面站观测数据、数值模拟以及卫星和再分析数据获取的植被指数,分析了 2007 年至 2016 年东亚地区沙尘暴(SDSs)的频率和强度。还分析了 SDSs 与地表状况和天气环流模式的关系。统计分析表明,2007 年至 2016 年春季记录的 SDS 事件数量和强度呈下降趋势。春季 SDS 事件的总数从 2011 年之前每年至少十次减少到 2011 年之后每年不到十次。主要尘源区地表灰尘浓度的年平均变化每年减少 33.24μg/m(-1.75%)。地面和地面以下附近温度的变化、降水和土壤湿度的变化都有利于植被覆盖的改善,从而降低了 SDS 的强度和频率。伴随高纬度冷空气流入的强风呈下降趋势,导致 SDS 数量减少,在 SDS 的年代际减少中起关键作用。研究期间极地涡旋强度的下降与 SDSs 强度和频率的下降密切相关。