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首页> 外文期刊>Atmospheric Measurement Techniques >Aerosol measurements with a shipborne Sun–sky–lunar photometer and collocated multiwavelength Raman polarization lidar over the Atlantic Ocean
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Aerosol measurements with a shipborne Sun–sky–lunar photometer and collocated multiwavelength Raman polarization lidar over the Atlantic Ocean

机译:用船载阳光 - 天空光度计和大西洋的搭配多波长拉曼偏振光仪的气溶胶测量

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A shipborne Sun–sky–lunar photometer of type CE318-T was tested during two trans-Atlantic cruises aboard the German research vessel Polarstern from 54° N to 54° S in May/June and December?2018. The continuous observations of the motion-stabilized shipborne CE318-T enabled the first-time observation of a full diurnal cycle of aerosol optical depth (AOD) and column-mean ?ngstr?m coefficient of a mixed dust–smoke episode. The latitudinal distribution of the AOD from the shipborne CE318-T, Raman lidar and MICROTOPS II shows the same trend with highest values in the dust belt from 0 to 20° N and overall low values in the Southern Hemisphere. The linear-regression coefficients of determination between MICROTOPS II and the CE318-T were 0.988, 0.987, 0.994 and 0.994 for AODs at 380, 440, 500 and 870 nm and 0.896 for the ?ngstr?m exponent at 440–870 nm. The root-mean-squared differences of AOD at 380, 440, 500 and 870 nm were 0.015, 0.013, 0.010 and 0.009, respectively.
机译:在5月/ 6月至6月和12月5日和12月的德国研究船偏光剧中,在德国研究容器偏光的两次跨大西洋巡航中,测试了CE318-T型型CE318-T的船载Sun-Sun-Sunar-Chopet达。运动稳定的船载CE318-T的连续观察使得首次观察气溶胶光学深度(AOD)的全昼夜周期和混合粉尘烟雾发作的柱式αm系数。 AOD的延伸来自船载CE318-T,拉曼LIDAR和MICROTOPS II的趋势显示出与南半球的0至20°N的灰尘带中的最高值相同的趋势。微量球体II和CE318-T之间测定的线性回归系数为0.988,0.987,0.994和0.994,用于380,440,500和870nm和0.896的AODS,在440-870nm处为ΔM指导。 380,440,500和870nm处的AOD的根平均平均差异分别为0.015,0.013,0.010和0.009。

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