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Transport of regional pollutants through a remote trans-Himalayan valley in Nepal

机译:通过尼泊尔的远程跨喜马拉雅山谷运输区域污染物

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Anthropogenic emissions from the combustion of fossil fuels and biomass in Asia have increased in recent years. High concentrations of reactive trace gases and light-absorbing and light-scattering particles from these sources form persistent haze layers, also known as atmospheric brown clouds, over the Indo-Gangetic plains (IGP) from December through early June. Models and satellite imagery suggest that strong wind systems within deep Himalayan valleys are major pathways by which pollutants from the IGP are transported to the higher Himalaya. However, observational evidence of the transport of polluted air masses through Himalayan valleys has been lacking to date. To evaluate this pathway, we measured black carbon (BC), ozone (O-3), and associated meteorological conditions within the Kali Gandaki Valley (KGV), Nepal, from January 2013 to July 2015. BC and O-3 varied over both diurnal and seasonal cycles. Relative to nighttime, mean BC and O-3 concentrations within the valley were higher during daytime when the up-valley flow (average velocity of 17 m s(-1)) dominated. BC and O-3 concentrations also varied seasonally with minima during the monsoon season (July to September). Concentrations of both species subsequently increased post-monsoon and peaked during March to May. Average concentrations for O3 during the seasonally representative months of April, August, and November were 41.7, 24.5, and 29.4 ppbv, respectively, while the corresponding BC concentrations were 1.17, 0.24, and 1.01 mu g m(-3), respectively. Up-valley fluxes of BC were significantly greater than down-valley fluxes during all seasons. In addition, frequent episodes of BC concentrations 2-3 times higher than average persisted from several days to a week during non-monsoon months. Our observations of increases in BC concentration and fluxes in the valley, particularly during pre-monsoon, provide evidence that trans-Himalayan valleys are important conduits for transport of pollutants from the IGP to
机译:近年来,亚洲化石燃料燃烧和生物质的燃烧的人为排放量增加。来自这些来源的高浓度的反应性痕量气体和光吸收和光散射颗粒形成持续的雾度层,在12月至6月初,在12月的印度难潮平原(IGP)上也称为大气棕色云。模型和卫星图像表明,喜马拉雅山谷内的强风系统是来自IGP的污染物被运送到更高的喜马拉雅山脉的主要途径。然而,通过喜马拉雅山谷的污染空气群众运输的观察证据一直缺乏迄今为止。评估该途径,从2013年1月到2015年1月,我们测量了Kali Gandaki谷(KGV)内的黑碳(BC),臭氧(O-3)和相关的气象状况.BC和O-3各种各样的变化昼夜季节循环。相对于夜间,当谷谷流动(平均速度为17 m s(-1))时,谷的平均Bc和O-3浓度在白天期间较高。在季风季节(7月至9月)期间,BC和O-3浓度也在很小上季节性化。两种物种的浓度随后增加了季风后,并在3月至5月期间达到峰值。 4月,8月和11月季节性代表的O3期间O3的平均浓度分别为41.7,20.5和29.4ppbv,而相应的BC浓度分别为1.17,0.24和1.01μgm(-3)。在所有季节期间,BC的Up-Valley Fluxes显着大于下谷助焊剂。此外,在非季风月期间,BC浓度常见的BC浓度比平均水平高2-3倍。我们对山谷中BC浓度和助熔剂增加的观察,特别是在季风前,提供跨喜马拉雅山谷的证据是,用于将污染物从IGP运输到的重要导管

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