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The effects of smoke and dust aerosols on UV-B radiation in Australia from ground-based and satellite measurements

机译:通过地面和卫星测量,烟雾和粉尘气溶胶对澳大利亚UV-B辐射的影响

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An understanding of the effect of aerosols on biologically- and photochemically-active UV radiation reaching the Earth's surface is important for many ongoing climate, biophysical, and air pollution studies. In particular, estimates of the UV characteristics of the most common Australian aerosols will be valuable inputs to UV Index forecasts, air quality studies, and assessments of the impact of regional environmental changes. Based on MODIS fire maps and MISR aerosol property retrievals, we analyzed the climatological distributions of Australian dust and smoke particles and identified two sites where ground-based UV-B spectra were available during episodes of relatively high aerosol activity. Since mid-2003, surface UV spectra (285-450 nm) have been measured routinely at Darwin and Alice Springs in Australia by the Australian Bureau of Meteorology (BoM). Using collocated AERO NET sunphotometer measurements at Darwin and collocated BoM sunphotometer measurements at Darwin and Alice Springs, we identified several episodes of relatively high aerosol activity that could be used to study the effects of dust and smoke on the UV-B solar irradiance at the Earth's surface. To assess smoke effects we compared the measured UV irradiances at Darwin with irradiances simulated with the libRadtran radiative transfer model for aerosol-free conditions. We found that for otherwise similar atmospheric conditions, aerosols reduced the UVB irradiance by 50% near the fire source and up to 15% downwind. We also found the effect of smoke particles to be 5 to 10% larger in the UV-B than in the UV-A. For the selected period at Darwin, changes in the aerosol loading gave larger variations in the surface UV irradiances than previously reported changes seen in the ozone column. We are continuing similar investigations for the Alice Springs site to assess spectral differences between smoke and dust aerosols.
机译:对于许多正在进行的气候,生物物理和空气污染研究,了解气溶胶对到达地球表面的生物和光化学活性紫外线辐射的影响至关重要。特别是,对澳大利亚最常见的气溶胶的紫外线特性的估计将对紫外线指数预测,空气质量研究以及区域环境变化的影响评估提供有价值的输入。基于MODIS火图和MISR气溶胶特性检索,我们分析了澳大利亚尘埃和烟尘颗粒的气候分布,并确定了在气溶胶活动相对较高的时期有地面UV-B光谱的两个位置。自2003年中以来,澳大利亚气象局(BoM)定期在澳大利亚的达尔文和爱丽斯泉测量了表面紫外线光谱(285-450 nm)。通过在达尔文使用并置的AERO NET太阳光度计测量以及在达尔文和爱丽斯泉并置的BoM太阳光度计测量,我们确定了一些相对较高的气溶胶活动事件,这些事件可以用来研究尘埃和烟雾对地球UV-B太阳辐照度的影响。表面。为了评估烟雾影响,我们将在达尔文测量的紫外线辐照度与使用libRadtran辐射传递模型模拟的无气雾条件下的辐照度进行了比较。我们发现,在其他类似的大气条件下,气溶胶可在火源附近将UVB辐照度降低50%,在顺风方向将其降低15%。我们还发现,烟雾颗粒的影响在UV-B中比在UV-A中大5至10%。在达尔文的选定时期,与臭氧柱中先前报道的变化相比,气溶胶载量的变化使表面紫外线辐照度变化更大。我们正在继续对爱丽斯泉(Alice Springs)站点进行类似调查,以评估烟雾和粉尘气溶胶之间的光谱差异。

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