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First observations of iodine oxide from space

机译:太空中氧化碘的初步观察

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摘要

We present retrievals of IO total columns from the Scanning Imaging Absorption Spectrometer for Atmospheric Chartography (SCIAMACHY) satellite instrument. We analyze data for October 2005 in the polar regions to demonstrate for the first time the capability to measure IO column abundances from space. During the period of analysis (i.e. Southern Hemisphere springtime), enhanced IO vertical columns over 3 x 10(13) molecules cm(-2) are observed around coastal Antarctica; by contrast during that time in the Artic region IO is consistently below the calculated instrumental detection limit for individual radiance spectra ( 2 - 4 x 10(12) molecules cm(-2) for slant columns). The levels reported here are in reasonably good agreement with previous ground-based measurements at coastal Antarctica. These results also demonstrate that IO is widespread over sea-ice covered areas in the Southern Ocean. The occurrence of elevated IO and its hitherto unrecognized spatial distribution suggest an efficient iodine activation mechanism at a synoptic scale over coastal Antarctica.
机译:我们介绍了从大气成图扫描成像吸收光谱仪(SCIAMACHY)卫星仪器获得的IO总柱数。我们分析了极地地区2005年10月的数据,首次证明了从空间测量IO柱丰度的能力。在分析期间(即南半球春季),在南极沿海地区观察到了超过3 x 10(13)分子cm(-2)的增强的IO垂直列;相反,在此期间,动脉区域IO始终低于针对单个辐射光谱(倾斜列为2-4 x 10(12)个分子cm(-2)的分子)的计算出的仪器检测极限。此处报告的水平与南极沿海地区以前的地面测量值相当吻合。这些结果还表明,IO在南部海洋的海冰覆盖区域广泛分布。 IO升高及其迄今无法识别的空间分布的发生表明,南极沿海沿海地区天气尺度上有一个有效的碘激活机制。

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