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Source, transport and impacts of a heavy dust event in the Yangtze River Delta, China, in 2011

机译:2011年中国长江三角洲一场重尘事件的来源,运输和影响

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Dust invasion is an important type of particle pollution in China. During 1to 6 May in 2011, a dust event was observed in the Yangtze River Deltaregion (YRD). The highest PM10 (particles up to 10 μ in diameter) concentration reached over 1000 μg m?3and the visibility was below 3 km. In this study, the CommunityMulti-scale Air Quality modeling system (CMAQ5.0) coupled with an in-linewindblown dust model was used to simulate the formation, spatial andtemporal characteristics of this dust event, and analyze its impacts. Thethreshold friction velocity for loose, fine-grained soil with low surfaceroughness in the dust model was revised based on Chinese data to improve themodel performance. This dust storm broke out in Xinjiang and Mongolia during28 to 30 April and arrived in the YRD region on 1 May. The transported dustparticles contributed to the mean surface layer concentrations of PM10in the YRD region 78.9% during 1 to 6 May with their impact weakeningfrom north to south due to the removal of dust particles along the path. Thedry deposition, wet deposition and total deposition of PM10 in the YRDreached 184.7 kt, 172.6 kt and 357.32 kt, respectively. The dust particles alsohad significant impacts on optical/radiative characteristics by absorptionand scattering. In Shanghai, the largest perturbations of aerosol optical depth (AOD) and irradiancewere about 0.8 DU and ?130 W m?2, which could obviously influence theradiation balance in this region. The decrease of actinic fluxesimpacts future photochemistry. In Shanghai, the negative effects on theNO2 and O3 photolysis could be −35% when dust particlesarrived. The concentrations of O3 and OH were reduced by 1.5% and3.1% in the whole of China, and by 9.4% and 12.1% in the YRD region,respectively. Such changes in O3 and OH levels can affect thefuture formation of secondary aerosols in the atmosphere by directly determining theoxidation rate of their precursors. The work of this manuscript ismeaningful for understanding the dust emissions in China as well as for theapplication of CMAQ in Asia. It is also helpful for understanding the formationmechanism and impacts of dust pollution in the YRD.
机译:灰尘入侵是中国一种重要的颗粒物污染类型。 2011年5月1日至6日,长江三角洲(YRD)发生了一次沙尘事件。 PM 10 (直径最大为10μs)的最高浓度超过1000μgm ?3 ,可见度在3 km以下。在这项研究中,社区多尺度空气质量建模系统(CMAQ5.0)与在线风吹尘埃模型一起用于模拟该尘埃事件的形成,空间和时间特征,并分析其影响。根据中国资料对粉尘模型中表面粗糙度低的疏松细颗粒土的极限摩擦速度进行了修正,以提高模型性能。这次沙尘暴在4月28日至30日在新疆和蒙古爆发,并于5月1日到达长三角地区。 5月1日至6日,输送的尘埃颗粒使长三角地区PM 10 的平均表层浓度达到78.9%,其影响从北向南减弱,这是由于沿途尘埃颗粒被清除。长三角地区PM 10 的干沉降,湿沉降和总沉降分别达到184.7 kt,172.6 kt和357.32 kt。灰尘颗粒还因吸收和散射而对光学/辐射特性产生重大影响。在上海,气溶胶光学深度(AOD)和辐照度的最大扰动约为0.8 DU和?130 W m ?2 ,这可能明显影响该区域的辐射平衡。光化通量的减少影响未来的光化学。在上海,到达尘埃粒子对NO 2 和O 3 光解的负面影响可能为-35%。在整个中国,O 3 和OH的浓度分别降低了1.5%和3.1%,在长三角地区分别降低了9.4%和12.1%。 O 3 和OH含量的这种变化可通过直接确定其前体的氧化速率来影响大气中次级气溶胶的未来形成。该手稿的工作对于理解中国的粉尘排放以及CMAQ在亚洲的应用具有重要意义。这也有助于了解长三角地区扬尘污染的形成机理和影响。

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