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Simulation of aerosol radiative properties with the ORISAM-RAD model during a pollution event (ESCOMPTE 2001)

机译:在污染事件中使用ORISAM-RAD模型模拟气溶胶的辐射特性(ESCOMPTE 2001)

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The aim of this study is to present the organic and inorganic spectral aerosol module-radiative (ORISAM-RAD) module, allowing the 3D distribution of aerosol radiative properties (aerosol optical depth, single scattering albedo and asymmetry parameter) from the ORISAM module. In this work, we test ORISAM-RAD for one selected day (24th June) during the ESCOMPTE (experience sur site pour contraindre les modeles de pollution atmospherique et de transport d'emissions) experiment for an urban/industrial aerosol type. The particle radiative properties obtained from in situ and AERONET observations are used to validate our simulations. In a first time, simulations obtained from ORISAM-RAD indicate high aerosol optical depth (AOD)~0.50-0.70 ± 0.02 (at 440 nm) in the aerosol pollution plume, slightly lower (~10-20%) than AERONET retrievals. In a second time, simulations of the single scattering albedo (ω_o) have been found to well reproduce the high spatial heterogeneities observed over this domain. Concerning the asymmetry parameter (g), ORISAM-RAD simulations reveal quite uniform values over the whole ESCOMPTE domain, comprised between 0.61 ± 0.01 and 0.65 ± 0.01 (at 440 nm), in excellent agreement with ground based in situ measurements and AERONET retrievals. Finally, the outputs of ORISAM-RAD have been used in a radiative transfer model in order to simulate the diurnal direct radiative forcing at different locations (urban, industrial and rural). We show that anthropogenic aerosols strongly decrease surface solar radiation, with diurnal mean surface forcings comprised between -29.0 ± 2.9 and -38.6 ± 3.9Wm~(-2), depending on the sites. This decrease is due to the reflection of solar radiations back to space (-7.3 ± 0.8 < ΔF_(TOA) < -12.3 ± 1.2 Wm~(-2)) and to its absorption into the aerosol layer (21.1 ± 2.1 < ΔF_(ATM) < 26.3 ± 2.6 W m~(-2)). These values are found to be consistent with those measured at local scale.
机译:这项研究的目的是介绍有机和无机光谱气溶胶模块辐射(ORISAM-RAD)模块,允许ORISAM模块的3D气溶胶辐射特性分布(气溶胶光学深度,单散射反照率和不对称参数)。在这项工作中,我们在城市/工业气溶胶类型的ESCOMPTE(污染大气和运输排放污染物的现场模拟实验)实验的选定日期(6月24日)进行了ORISAM-RAD测试。从原位和AERONET观测获得的粒子辐射特性用于验证我们的模拟。首次从ORISAM-RAD获得的模拟结果表明,气溶胶污染羽流中的气溶胶光学深度(AOD)高至0.50-0.70±0.02(在440 nm处),比AERONET检索略低(约10-20%)。第二次,发现单散射反照率(ω_o)的模拟很好地重现了在该域上观察到的高空间异质性。关于不对称参数(g),ORISAM-RAD模拟显示整个ESCOMPTE域的值非常均匀,介于0.61±0.01到0.65±0.01(在440 nm)(与440纳米),与基于地面的原位测量和AERONET检索非常吻合。最后,ORISAM-RAD的输出已用于辐射传递模型中,以模拟不同位置(城市,工业和农村)的日直接辐射强迫。我们发现,人为气溶胶强烈地减少了表面太阳辐射,其日平均表面强迫在-29.0±2.9和-38.6±3.9Wm〜(-2)之间,具体取决于位置。这种减少是由于太阳辐射反射回太空(-7.3±0.8 <ΔF_(TOA)<-12.3±1.2 Wm〜(-2))并被吸收到气溶胶层中(21.1±2.1 <ΔF_( ATM)<26.3±2.6 W m〜(-2))。发现这些值与在当地规模下测得的值一致。

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