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Influence of Desert Dust Intrusions on Ground-based and Satellite Derived Ultraviolet Irradiance in Southeastern Spain

机译:沙漠尘埃入侵对西班牙东南部地面和人造卫星紫外线辐射的影响

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摘要

The desert dust aerosols strongly affect propagation of solar radiation through the atmosphere, reducing surface irradiance available for photochemistry and photosynthesis. This paper evaluates effects of desert dust on surface UV erythemal irradiance (UVER), as measured by a ground-based broadband UV radiometer and retrieved from the satellite Ozone Monitoring Instrument (OMI) at Granada (southern Spain) from January 2006 to December 2010. The dust effects are characterized by the transmittance ra tio of the measured UVER to the corresponding modeled clear sky value. The transmittance has an exponential dependency on aerosol optical depth (AOD), with minimum values of approximately 0.6 (attenuation of approximately 40%). The OMI UVER algorithm does not account for UV aerosol absorption, which results in overestimation of the ground-based UVER especially during dust episodes with a mean relative difference up to 40%. The application of aerosol absorption post-correction method reduces OMI bias up to approximately 13%. The results highlight great effect of desert dust on the surface UV irradiance in regions like southern Spain, where dust intrusions from Sahara region are very frequent.
机译:沙漠尘埃气溶胶强烈影响太阳辐射通过大气的传播,从而减少了可用于光化学和光合作用的表面辐照度。本文评估了沙漠尘埃对地面紫外线红斑辐照度(UVER)的影响,该辐照度是通过地面宽带紫外线辐射计测量的,并从2006年1月至2010年12月从格拉纳达(西班牙南部)的卫星臭氧监测仪(OMI)检索到。尘埃效应的特征在于,所测得的UVER对相应建模的晴空值的透射率比值。透射率与气溶胶光学深度(AOD)呈指数关系,最小值约为0.6(衰减约40%)。 OMI UVER算法不考虑紫外线气溶胶的吸收,这会导致高估基于地面的UVER,特别是在沙尘暴期间,其平均相对差异高达40%。气溶胶吸收后校正方法的应用将OMI偏差降低了大约13%。结果突出表明,在西班牙南部等地区,沙漠尘埃对撒哈拉沙漠地区的灰尘入侵非常频繁,这对地表紫外线辐射具有巨大影响。

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