Tempo-Spatial Distributions and Transport Characteristics of Two Dust Events over Northern China in March 2021

• Published in: Remote sensing (Basel, Switzerland) Vol. 14; no. 23; p. 5967
• Main Authors: Sun, Xiaoguang, Fan, Xuehua, Zhang, Tianle, Wang, Yinan, Wang, Yuntao, Lyu, Daren, Zheng, Mei
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01.12.2022
• Subjects: Accuracy; aerosol optical properties; Aerosols; Air masses; Atmosphere; Coastal zone; Datasets; Deserts; Dust; dust transport; Eastern Asia dust; Experiments; Ground-based observation; Meteorological satellites; Mongolian cyclone; Optical properties; Polar orbiting satellites; Pollutants; Radiation; Regions; Remote sensing; Satellite observation; Satellites; Spatial distribution; Trajectories; Transport properties; East Asia; Mongolia; Pacific Ocean; China
• ISSN: 2072-4292; 2072-4292
• DOI: 10.3390/rs14235967

The Taklamakan Desert and the Gobi Desert in East Asia constitute the second-largest sources of dust in the world. In particular, dust originating from the Gobi Desert is more susceptible to long-range transport, with consequent impacts in downwind Asian countries and the Northwest Pacific region. Two intensive dust events (the 3·15 dust event and the 3·28 dust event) were experienced in North China in March 2021. The 3·15 dust process was rated as the most intensive dust process in China in the past 10 years. In this study, by using a combination of spaceborne remote sensing datasets from geostationary and polar-orbiting satellites, ground-based columnar observations of aerosol optical parameters, meteorological reanalysis data, and backward trajectory simulations of air masses, the transport pathways and the three-dimensional structure characteristics of dust aerosols during the transport of the two dust events in March 2021 were cross-validated. The results of the study indicated that the two dust events were induced by the Mongolian cyclone. Due to the different configurations of the ground meteorological system conditions, a backflow process occurred during the 3·15 dust event transmission process. After passing over North China and the Bohai Sea, the direction of transport of the dust plume was reversed. The wind deflected from northwest to northeast, and the dust reached the eastern coastal areas of China and was finally deposited on land. The 3·28 dust event exhibited aerosol stratification in the transport path, the higher pure dust layer reached up to 9 km height, and the lower layer underwent aerosol mixing and became a polluted dust aerosol. This study implies that the investigation of dust aerosol transport and the deposition processes, the impact on the ocean, and the impact of marine aerosols on land also needs to be taken into consideration; the integration of advanced satellites and ground-based remote sensing data, the meteorological reanalysis data and the backward trajectories simulation, which complemented and verified each other, can enhance the ability to delineate the transport pathways and the three-dimensional structural characteristics of dust events.