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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >High altitude (~4520 m amsl) measurements of black carbon aerosols over western trans-Himalayas: Seasonal heterogeneity and source apportionment
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High altitude (~4520 m amsl) measurements of black carbon aerosols over western trans-Himalayas: Seasonal heterogeneity and source apportionment

机译:喜马拉雅山西缘黑碳气溶胶的高海拔(〜4520 m amsl)测量:季节性非均质性和源分配

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The first ever, year-round measurements of aerosol black carbon (BC) over the western part of trans- Himalayas are reported from Hanle (~4520 m above mean sea level). The daily mean BC concentrations varied from as low as 7 ng m~(-3) to as high as 296 ng m~(-3) with an annual average of 77 ± 64 ng m~(-3), indicating significant BC burden even at freetropospheric altitudes. Variation with in the day as well as from day to day were highly subdued during winter season (December to February) while they used to be the highest in Spring (March to May). In general, the less frequently occurring high BC values contributed more to the annual and seasonal means, while 64% of the values were below the annual mean. Seasonally, highest BC concentration (109 ± 78 ng m~(-3)) occurred during Spring and lowest (66 ± 42/66 ± 62 ng m~3) during Summer/Winter season(June to August/December to February). Diurnal variations in general were very weak, except during Spring and Summer when the effects of convective boundary layer dynamics is discernible. Back trajectory clustering and concentration weighted trajectory (CWT) analyses indicated that, most time of the year the sampling location is influenced by the advection from West and Southwest Asia, while the contribution from the Indo-Gangetic Plains (IGP) remained very low during Spring and Summer. The seasonal and annual mean BC at Hanle are significantly lower than the corresponding values reported for other Himalayan stations, while they were quite higher than those reported from the South Pole and pristine Antarctic environments.
机译:据报道,汉勒(距平均海平面约4520 m)对跨喜马拉雅山脉西部地区的气溶胶黑碳(BC)进行了全年的首次测量。每日平均BC浓度从低至7 ng m〜(-3)到高达296 ng m〜(-3)不等,年平均为77±64 ng m〜(-3),表明BC负担很重即使在对流层高度。在冬季(12月至2月),每天和每天的变化都比较低,而在春季(3月至5月)则是最高的。通常,较少出现的高BC值对年平均值和季节平均值的贡献更大,而64%的值低于年平均值。季节上,春季的BC浓度最高(109±78 ng m〜(-3)),而在夏季/冬季(6月至8月/ 12月至2月)最低(66±42/66±62 ng m〜(3))。除了春季和夏季期间,对流边界层动力学的影响是可辨别的,一般而言,昼夜变化很小。反向轨迹聚类和集中加权轨迹(CWT)分析表明,一年中的大部分时间,采样位置受到西亚和西南亚对流的影响,而春季时印度-恒河平原(IGP)的贡献仍然很低和夏天。 Hanle的季节和年均BC显着低于其他喜马拉雅气象站报告的相应值,但远高于南极和原始南极环境的报告值。

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