Key Laboratory of Land Surface Process and Climate Change in Cold and Arid Regions, Cold & Arid Regions Environmental & Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China.
Key Laboratory of Land Surface Process and Climate Change in Cold and Arid Regions, Cold & Arid Regions Environmental & Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China.
Environ Pollut. 2015 Dec;207:107-22. doi: 10.1016/j.envpol.2015.08.052. Epub 2015 Sep 11.
The dust origins of the two events were identified using HYSPLIT trajectory model and MODIS and CALIPSO satellite data to understand the particle size distribution during two contrasting dust events originated from Taklimakan and Gobi deserts. The supermicron particles significantly increased during the dust events. The dust event from Gobi desert affected significantly on the particles larger than 2.5 μm, while that from Taklimakan desert impacted obviously on the particles in 1.0-2.5 μm. It is found that the particle size distributions and their modal parameters such as VMD (volume median diameter) have significant difference for varying dust origins. The dust from Taklimakan desert was finer than that from Gobi desert also probably due to other influencing factors such as mixing between dust and urban emissions. Our findings illustrated the capacity of combining in situ, satellite data and trajectory model to characterize large-scale dust plumes with a variety of aerosol parameters.
利用 HYSPLIT 轨迹模型和 MODIS 以及 CALIPSO 卫星数据,确定了这两起事件的尘埃来源,以了解源自塔克拉玛干沙漠和戈壁沙漠的两起对比鲜明的尘埃事件期间的颗粒尺寸分布。在尘埃事件期间,超微米颗粒显著增加。来自戈壁沙漠的尘埃事件对大于 2.5μm 的颗粒有显著影响,而来自塔克拉玛干沙漠的尘埃事件对 1.0-2.5μm 的颗粒有明显影响。结果发现,颗粒尺寸分布及其模态参数(如 VMD(体积中值直径))因尘埃来源的不同而有显著差异。来自塔克拉玛干沙漠的尘埃比来自戈壁沙漠的尘埃更细,这可能也归因于尘埃与城市排放物混合等其他影响因素。我们的研究结果表明,结合现场、卫星数据和轨迹模型来描述具有多种气溶胶参数的大规模尘埃羽流的能力。