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Deriving Aerosol Absorption Properties from Solar Ultraviolet Radiation Spectral Measurements at Thessaloniki, Greece

机译:从希腊萨洛尼卡的太阳紫外线辐射光谱测量推导气溶胶吸收特性

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The gap in knowledge regarding the radiative effects of aerosols in the UV region of the solar spectrum is large, mainly due to the lack of systematic measurements of the aerosol single scattering albedo (SSA) and absorption optical depth (AAOD). In the present study, spectral UV measurements performed in Thessaloniki, Greece by a double monochromator Brewer spectrophotometer in the period 1998–2017 are used for the calculation of the aforementioned optical properties. The main uncertainty factors have been described and there is an effort to quantify the overall uncertainties in SSA and AAOD. Analysis of the results suggests that the absorption by aerosols is much stronger in the UV relative to the visible. SSA follows a clear annual pattern ranging from ~0.7 in winter to ~0.85 in summer at wavelengths 320–360 nm, while AAOD peaks in summer and winter. The average AAOD for 2009–2011 is ~50% above the 2003–2006 average, possibly due to increased emissions of absorbing aerosols related to the economic crisis and the metro-railway construction works in the city center.
机译:关于气溶胶在太阳光谱的紫外线区域中的辐射效应的知识差距很大,这主要是由于缺乏对气溶胶单散射反照率(SSA)和吸收光学深度(AAOD)的系统测量。在本研究中,使用双单色仪Brewer分光光度计在希腊塞萨洛尼基进行的1998-2017年光谱UV测量用于计算上述光学性能。已经描述了主要的不确定性因素,并且正在努力量化SSA和AAOD的总体不确定性。结果分析表明,相对于可见光,气溶胶在紫外线中的吸收要强得多。 SSA遵循清晰的年度模式,从冬季的〜0.7到夏季的〜0.85,波长在320-360 nm之间,而AAOD在夏季和冬季达到峰值。 2009-2011年的平均AAOD比2003-2006年的平均水平高约50%,这可能是由于与经济危机和市中心的地铁建设相关的吸收性气溶胶排放量增加。

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