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首页> 外文期刊>Atmospheric environment >Long-term observations of black carbon aerosol over a rural location in southern peninsular India: Role of dynamics and meteorology
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Long-term observations of black carbon aerosol over a rural location in southern peninsular India: Role of dynamics and meteorology

机译:印度南部半岛农村地区黑碳气溶胶的长期观测:动力学和气象学的作用

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Ten years (2008–2017) of Black Carbon (BC) observations obtained using Aethalometer (AE-31) are analyzed to investigate the seasonal trends and temporal variabilities over a tropical site Gadanki (13.5° N, 79.2° E) located in south-east India. Diurnal variations of BC have two peak structures one in the morning (∼08 IST) in all seasons and second in the evening (∼20 IST) only during the pre-monsoon (March–May). Intra-annual variation in BC indicated February and March months as the bio-mass burning with highest BC mass concentration (3000–5000 ng/m3). About 46% of air parcel back trajectories found passing across the in-land regions of southern peninsular India brining transported aerosol to the source location during pre-monsoon. The lowest BC (∼1500 ng/m3) is noticed during the monsoon months (June–September). The average BC (2200 ng/m3) represents observational site as a typical rural site. The inter-annual variability of BC did not show any significant trend. However, trends in the maximum (March) and minimum (July) BC values show statistically significant decreasing trend suggesting reduction in bio-mass burning sources during March supported by the decrease in the fire counts. Diurnal variation in the absorption angstrom exponent indicates that the morning and evening peaks are contributed by the bio-mass combustion with values above threshold of 1. However, angstrom exponent values are found below 1 during noon time of monsoon season suggesting fossil fuel contribution. Strong coupling is found between aerosol concentration and tropospheric dynamics, meteorology in addition to the sources. The present study is expected to provide valuable input to the modelers and observational physicists as BC is climate sensitive variable.
机译:分析了使用Aethalometer(AE-31)获得的十年(2008-2017)黑炭(BC)观测资料,以调查位于南南部的加丹基(13.5°N,79.2°E)热带站点的季节性趋势和时间变化。印度东部。 BC的昼夜变化有两个高峰结构,一个在所有季节的早晨(〜08 IST),另一个在晚上的第二个(〜20 IST),仅在季风前(3月至5月)。 BC的年内变化表明2月和3月为生物量燃烧,BC质量浓度最高(3000-5000–ng / m3)。在季风爆发前,发现穿越印度南部半岛内陆地区的空气包裹回航轨迹中约有46%会将气溶胶运输到源头位置。在季风月份(6月至9月),发现最低的BC(约1500 / ng / m3)。平均BC(2200 ng / m3)代表观察点为典型的农村站点。 BC的年际变化没有显示任何显着趋势。但是,最大(3月)和最小(7月)BC值的趋势显示出统计学上显着的下降趋势,表明3月份生物量燃烧源的减少受到火计数的减少的支持。吸收埃指数的日变化表明,早晨和傍晚的峰值是由生物质燃烧贡献的,其值高于阈值1。但是,在季风季节中午发现埃指数值小于1,表明化石燃料的贡献。除气源外,还发现气溶胶浓度与对流层动力学,气象学之间存在强耦合。由于BC是气候敏感变量,因此本研究有望为建模者和观察物理学家提供有价值的输入。

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