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Lidar ratios of stratospheric volcanic ash and sulfate aerosols retrieved from CALIOP measurements

机译:从CALIOP测量获得的平流层火山灰和硫酸盐气溶胶的激光雷达比率

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We apply a two-way transmittance constraint to nighttime CALIOP (Cloud-Aerosol Lidar with Orthogonal Polarization) observations of volcanic aerosol layers to retrieve estimates of the particulate lidar ratio (iS/isubp/sub) at 532?nm. This technique is applied to three volcanic eruption case studies that were found to have injected aerosols directly into the stratosphere. Numerous lidar observations permitted characterization of the optical and geometric properties of the volcanic aerosol layers over a time period of 1–2 weeks. For the volcanic ash-rich layers produced by the Puyehue-Cordón Caulle eruption (June 2011), we obtain mean and median particulate lidar ratios of 69?±?13?sr and 67?sr, respectively. For the sulfate-rich aerosol layers produced by Kasatochi (August 2008) and Sarychev Peak (June 2009), the means of the retrieved lidar ratios were 66?±?19?sr (median 60?sr) and 63 ± 14?sr (median 59?sr), respectively. The 532?nm layer-integrated particulate depolarization ratios (iδ/isubp/sub) observed for the Puyehue layers (iδ/isubp/sub = 0.33?±?0.03) were much larger than those found for the volcanic aerosol layers produced by the Kasatochi (iδ/isubp/sub = 0.09?±?0.03) and Sarychev (iδ/isubp/sub = 0.05 ± 0.04) eruptions. However, for the Sarychev layers we observe an exponential decay (ie/i-folding time of 3.6?days) in iδ/isubp/sub with time from 0.27 to 0.03. Similar decreases in the layer-integrated attenuated colour ratios with time were observed for the Sarychev case. In general, the Puyehue layers exhibited larger colour ratios (iχ/i′ = 0.53?±?0.07) than what was observed for the Kasatochi (iχ/i′ = 0.35?±?0.07) and Sarychev (iχ/i′ = 0.32?±?0.07) layers, indicating that the Puyehue layers were generally composed of larger particles. These observations are particularly relevant to the new stratospheric aerosol subtyping classification scheme, which has been incorporated into version 4 of the level 2 CALIPSO (Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation) data products.
机译:我们对火山气溶胶层的夜间CALIOP(正交偏振云气溶胶激光雷达)观测值应用双向透射率约束,以获取颗粒物激光雷达比( S p )在532?nm。这项技术适用于三个火山喷发案例研究,这些案例研究发现将气溶胶直接注入平流层。多次激光雷达观测可以表征1-2周内火山气溶胶层的光学和几何特性。对于Puyehue-CordónCaulle喷发(2011年6月)产生的火山灰富集层,我们得出的平均和中值激光雷达的激光雷达比分别为69?±?13?sr和67?sr。对于Kasatochi(2008年8月)和Sarychev Peak(2009年6月)产生的富含硫酸盐的气溶胶层,检索到的激光雷达比的平均值为66?±?19?sr(中值60?sr)和63±14?sr(中位数59?sr)。在Puyehue层(δ p )观察到的532?nm层积分颗粒去极化率(δ p ) = 0.33?±?0.03)远大于Kasatochi(δ p = 0.09?±?0.03)和Sarychev(< i>δ p = 0.05±0.04)爆发。但是,对于Sarychev层,我们观察到δ p 中的指数衰减( e 折叠时间为3.6?days),时间从0.27到0.03。对于Sarychev案例,观察到随着时间的推移,层积分的衰减颜色比率的下降类似。通常,Puyehue层显示出比Kasatochi(χ'= 0.35?±?0.07)更大的色比(χ'= 0.53?±?0.07)。 )和Sarychev(χ'= 0.32?±?0.07)层,表明Puyehue层通常由较大的颗粒组成。这些观测结果与新的平流层气溶胶亚型分类方案特别相关,该方案已纳入2级CALIPSO(云气溶胶激光雷达和红外探路者卫星观测)数据产品的第4版。

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