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Horizontal variability of aerosol optical depth observed during the ARCTAS airborne experiment

机译:在ARCTAS机载实验期间观察到的气溶胶光学深度的水平变化

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摘要

We present statistics on the horizontal variability of aerosol optical depth(AOD) directly measured from the NASA P-3 aircraft. Our measurements duringtwo contrasting phases (in Alaska and Canada) of the ARCTAS mission arguablyconstrain the variability in most aerosol environments common over theglobe. In the Canada phase, which features local emissions, 499 nm AOD has amedian relative standard deviation (stdrel, med) of 19 % and 9 % andan autocorrelation (r) of 0.37 and 0.71 over 20 km and 6 km horizontalsegments, respectively. In the Alaska phase, which features long-rangetransport, the variability is considerably lower (stdrel, med = 3 %, r = 0.92 even over 35.2 km). Compared to the magnitude of AOD, its wavelengthdependence varies less in the Canada phase, more in the Alaska phase. Wetranslate these findings from straight-line flight tracks into grid boxesand points, to help interpretation and design of satellite remote sensing,suborbital observations and transport modeling.
机译:我们提供了直接从NASA P-3飞机测量的气溶胶光学深度(AOD)的水平变化的统计数据。我们在ARCTAS任务的两个对比阶段(在阿拉斯加和加拿大)的测量结果可以说限制了地球上常见的大多数气溶胶环境中的变异性。在具有局部发射特征的加拿大阶段,499 nm AOD的中位相对标准偏差(std rel,med )为19%和9%,自相关( r )为在20 km和6 km水平段上分别为0.37和0.71。在具有远程传输功能的阿拉斯加阶段,变异性要低得多(即使在35.2公里以上,std rel,med = 3%, r = 0.92)。与AOD的大小相比,其波长依赖性在加拿大阶段变化较小,在阿拉斯加阶段变化较大。我们将这些发现从直线飞行轨迹转换为网格框和点,以帮助解释和设计卫星遥感,亚轨道观测和运输模型。

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