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半干旱热带地区乌代布尔气溶胶黑碳浓度的多年特征分析。

Multi-year characterization of aerosol black carbon concentrations over a semiarid tropical site Udaipur.

作者信息

Vyas Brij Mohan, Gogoi Mukunda M, Jose Subin

机构信息

Department of Physics, Pacific College of Basic & Applied Sciences, Pacific University, Udaipur, 313 024, India.

Space Physics Laboratory, Vikram Sarabhai Space Centre, Indian Space Research Organization, Trivandrum, 695 022, India.

出版信息

Environ Sci Pollut Res Int. 2021 May;28(18):22864-22877. doi: 10.1007/s11356-020-12300-y. Epub 2021 Jan 11.

Abstract

Continuous and multi-year (2008-2012) measurements of black carbon (BC) mass concentrations (M), carried out from the semiarid tropical site Udaipur (24.6° N, 74° E, 580 m a.s.l.) near the western Indian desert, are analyzed for their region-specific features. M varied over a wide range during the period of study, with the hourly mean values occurring as low as 0.09 to as high as 49.1 μg m, with the multi-year average ~ 4.5 ± 2.6 μg m. Annual variations showed the highest concentrations during November and December (winter seasonal mean = 7.4 ± 3.3 μg m) and the lowest in the monsoon months of July and August (monsoon seasonal mean = 2.5 ± 2.2 μg m). M showed significant inverse relationship with the planetary boundary layer height (ρ ~ - 0.50) as well as ventilation coefficient (ρ ~ - 0.72). Alike aforesaid atmospheric dynamic parameters, T, WS, and RH also possessed statistically significant negative correlations with monthly M. Enhancement in annual as well as diurnal amplitude in M during deficient monsoon years relative to excessive monsoon years have given marked indication of BC sink mechanism due to precipitation. Roles of long-range regional air pollutant transport also have been identified. Identical and consistent seasonal variation in percentage contribution of M with PM (varying from 2.6 to 9.1%) and absorption Angstrom exponent (α, monthly mean values varying from 0.77 ± 0.04 to 1.16 ± 0.08) gives evidence of substantial amount of enhanced anthropogenic source activities of fossil fuel incomplete combustion in post-monsoon and winter period.

摘要

对印度西部沙漠附近半干旱热带地区乌代布尔(北纬24.6°,东经74°,海拔580米)在2008 - 2012年期间进行的连续多年的黑碳(BC)质量浓度(M)测量数据进行了区域特征分析。在研究期间,M的变化范围很广,每小时平均值低至0.09微克/立方米,高至49.1微克/立方米,多年平均值约为4.5±2.6微克/立方米。年度变化显示,11月和12月浓度最高(冬季季节平均值 = 7.4±3.3微克/立方米),7月和8月季风月份浓度最低(季风季节平均值 = 2.5±2.2微克/立方米)。M与行星边界层高度(ρ约为 - 0.50)以及通风系数(ρ约为 - 0.72)呈显著负相关。与上述大气动力学参数一样,温度(T)、风速(WS)和相对湿度(RH)与月度M也具有统计学上的显著负相关。相对于季风过剩年份,季风不足年份M的年度和日变化幅度增大,这明显表明降水导致了黑碳汇机制。还确定了远距离区域空气污染物传输的作用。M在PM中的贡献百分比(从2.6%到9.1%不等)以及吸收埃指数(α,月平均值从0.77±0.04到1.16±0.08不等)呈现相同且一致的季节性变化,这证明在季风后和冬季期间,化石燃料不完全燃烧的人为源活动大量增加。

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