第七章

C. Marley
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引用次数: 0

摘要

本文利用一种新的反演技术对来自GOME/ERS-2和GOME-2/MetOp-A卫星最低点紫外可见仪器的测量结果进行了分析,该技术结合了测量的BrO倾斜柱和使用第6章中介绍的气气学对平流层BrO含量的估计。使用辐射传输模型计算的气团因子被用于解释观测几何形状、云层、地表反照率和BrO剖面形状对测量结果的影响。结果表明,该方法能较好地分离和量化极态BrO表面辐射。此外,将观测到的总BrO柱的平流层和对流层部分分离,可以更详细地研究BrO羽流在平流层和对流层中的输送。在相关地面资料和综合误差预算的支持下,提供了1-3 × 10分子/cm2的全球自由对流层BrO背景的证据。该对流层BrO背景没有明显的季节或纬度变化迹象。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Chapter 7
Measurements from the GOME/ERS-2 and GOME-2/MetOp-A satellite nadir UV-visible instruments have been analyzed for tropospheric BrO using a new retrieval technique that combines measured BrO slant columns and estimates of the stratospheric BrO content using the climatology presented in chapter 6. Air mass factors calculated using a radiative transfer model, are applied to account for the impact of observation geometry, clouds, surface albedo and BrO profile shape on the measurements. It is shown that this method enables to better isolate and quantify the polar BrO surface emissions. Moreover, the separation of stratospheric and tropospheric fractions of the observed total BrO columns allows studying the transport of BrO plumes in both stratosphere and troposphere in more detail. Supported by correlative ground-based data and a comprehensive error budget, evidences are provided for a global free-tropospheric BrO background with columns of 1-3 x 10 molec/cm2. No sign of significant seasonal or latitudinal variation of this tropospheric BrO background could be found.
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