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Observations and transport modeling of dust storm event over Northeast Asia using HYSPLIT: case study

机译:基于HYSPLIT的东北亚沙尘暴事件观测和传输模型:案例研究

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This study analyzes a regional dust storm event that occurred in spring 2016 using data from observation sites, Lidar measurements, and satellite imageries. PM_(10)concentrations at surface observation stations are considered as a primary indicator of the dust events. The dust events occurred on 3-12 March with PM_(10)reaching a maximum beyond 1682, 1498, 706, and 165 μg m~(?3)at observation sites in Mongolia, China, Korea and Japan, respectively. The dust event in Northeast Asia is captured by time series of PM_(10)concentrations at observation sites. On 3-4 March, the dust storm event originated from Mongolia move toward China, Korea and Japan. Vertical distributions of dust observed by Lidar measurements from stations in AD-Net capture a thick layer of nearly 2.2 km of high concentrations above surface in the area of origin. The maximum PM_(10)concentration drops with downwind transport. Dust source identification and dust-loaded air parcel trajectories are calculated using the HYSPLIT model. According to the HYSPLIT model, the dust storm started on 3-4 March from Mongolia and reached northern Japan in about 4 days passing over northern China and Korea.
机译:这项研究使用观测站,激光雷达测量和卫星图像数据分析了2016年春季发生的区域沙尘暴事件。表面观测站的PM_(10)浓度被认为是粉尘事件的主要指标。粉尘事件发生在3月3日至12日,在蒙古,中国,韩国和日本的观测地点,PM_(10)分别达到最大,分别超过1682、1498、706和165μgm〜(?3)。东北亚的尘埃事件是通过观测地点的PM_(10)浓度的时间序列捕获的。 3月3-4日,源自蒙古的沙尘暴事件向中国,韩国和日本转移。在AD-Net站点中,通过激光雷达测量所观测到的垂直尘埃分布,在原始区域的地面上方捕获了近2.2 km的高浓度厚层。最大PM_(10)浓度随顺风运输而下降。使用HYSPLIT模型可以计算出粉尘源识别和装满粉尘的空气轨迹。根据HYSPLIT模型,沙尘暴始于3月3-4日,从蒙古开始,经过约4天到达中国北部和韩国,到达日本北部。

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