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Real-time observational evidence of changing Asian dust morphology with the mixing of heavy anthropogenic pollution

机译:实时观测证据表明由于严重的人为污染亚洲尘埃形态发生了变化

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摘要

Natural mineral dust and heavy anthropogenic pollution and its complex interactions cause significant environmental problems in East Asia. Due to restrictions of observing technique, real-time morphological change in Asian dust particles owing to coating process of anthropogenic pollutants is still statistically unclear. Here, we first used a newly developed, single-particle polarization detector and quantitatively investigate the evolution of the polarization property of backscattering light reflected from dust particle as they were mixing with anthropogenic pollutants in North China. The decrease in observed depolarization ratio is mainly attributed to the decrease of aspect ratio of the dust particles as a result of continuous coating processes. Hygroscopic growth of Calcium nitrate (Ca(NO3)2) on the surface of the dust particles played a vital role, particularly when they are stagnant in the polluted region with high RH conditions. Reliable statistics highlight the significant importance of internally mixed, ‘quasi-spherical’ Asian dust particles, which markedly act as cloud condensation nuclei and exert regional climate change.
机译:天然矿物粉尘和严重的人为污染及其复杂的相互作用在东亚引起了严重的环境问题。由于观测技术的限制,由于人为污染物的包被过程,亚洲尘埃颗粒的实时形态变化在统计上仍不清楚。在这里,我们首先使用了一种新开发的单粒子偏振探测器,并定量研究了华北尘埃粒子与人为污染物混合后向后散射光的偏振特性的演变。观察到的去极化比的降低主要归因于连续涂覆过程导致的灰尘颗粒长径比的降低。灰尘颗粒表面的硝酸钙(Ca(NO3)2)的吸湿性起着至关重要的作用,尤其是当它们在高RH条件的污染区域停滞时。可靠的统计数据突显出内部混合的“准球形”亚洲尘埃颗粒的重要性,这些尘埃颗粒显着充当云凝结核并施加区域气候变化。

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