印度恒河平原中部吸收气溶胶的来源解析

Aditya Vaishya, Prayagraj Singh, S. Rastogi, S. Babu
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引用次数: 4

摘要

印度恒河平原大气气溶胶的辐射特性具有高度的时空异质性。尽管在表征IGP中气溶胶的辐射和物理化学性质方面已经取得了重大进展,但关于总吸收气溶胶预算的有机含量的信息仍然缺乏。在本研究中,我们分析了来自Gorakhpur中央igp(26.75°N, 83.38°E, 85m amsl)的两年气溶胶光谱光吸收测量,以研究它们的季节性行为,并根据吸收气溶胶负荷和源物种来量化它们的大小。利用MODIS Terra的“云校正火数”和OMI卫星平台的“吸收气溶胶指数”形式的遥感数据来确定吸收气溶胶的源区域。光谱吸收分析显示,由于生物量气溶胶对总吸收气溶胶负荷的贡献增加,冬季(W)和季风后(PoM)季节紫外线波长的吸收比880 nm增加了四倍。尽管在季风前(PM)季节,来自生物质源的气溶胶在总吸收气溶胶含量中所占的比例在W和PM季节为27%,而PM季节为17%。这是由于在西季和东季风季,接近停滞的风况和较浅的气团高度移动到IGP中部造成的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Source apportionment of absorbing aerosols in the central Indo-Gangetic Plain
Atmospheric aerosols in the Indo-Gangetic Plain (IGP) depicts high spatial and temporal heterogeneity in their radiative properties. Despite the fact that significant advancement in terms of characterizing aerosols radiative and physiochemical properties in the IGP have been made, information regarding the organic content towards total absorbing aerosol budget is lacking. In the present study we have analyzed two years of aerosol spectral light absorption measurements from the central-IGP, Gorakhpur (26.75°N, 83.38°E, 85m amsl), in order to study their seasonal behavior and to quantify their magnitude in terms of absorbing aerosols loading and source speciation. Remote sensing data in the form of 'Cloud corrected Fire Count' from MODIS Terra and 'Absorption Aerosol Index' from OMI satellites platform have been used to identify absorbing aerosol source regions. Spectral absorption analysis reveals a four-fold enhancement in absorption in the winter (W) and the post-monsoon (PoM) seasons at UV wavelengths as compared to 880 nm on account of increased biomass aerosol contribution to total absorbing aerosol load. Despite having higher fire events and absorption aerosol index, both indicating high biomass burning activities, in the pre-monsoon (PM) season, aerosols from the biomass sources contribute ~ 27% during the W and the PoM seasons as against ~17% in the PM season to the total absorbing aerosol content. This is due to near stagnant wind conditions and shallow height of air masses travelling to the central IGP in the W and the PoM seasons.
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