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Preliminary results for HCHO and BrO from the EOS-Aura Ozone Monitoring Instrument

机译:来自EOS-Aura臭氧监测仪的HCHO和BRO的初步结果

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The Ozone Monitoring Instrument (OMI), a nadir-viewing near-UV/Visible CCD spectrometer, was launched on NASA's EOS-Aura satellite platform on 15 July 2004 into a sun-synchronous, polar orbit with an equator crossing time of 13:45h (ascending node). OMI measurements cover the spectral region of 270-500 nm with a spectral resolution between 0.42 nm and 0.63 nm and a nominal ground footprint of 13x24 km2 at nadir. Global coverage is achieved in one day. The very high spatial resolution of OMI measurements set a new standard for trace gas and air quality monitoring from space. Combined with daily global coverage, this significantly advances our ability to answer outstanding questions on air chemistry, including the determination of BrO sources in mid and low latitudes, BrO-O3 anti-correlations as a function of latitude, and the production of formaldehyde in cities of the developing world. We give an overview of the OMI instrument and introduce the operational trace gas retrieval scheme for BrO, HCHO, and OClO that is based on a direct, non-linear fitting approach of observed radiances, including corrections for spectral undersampling. We present first results for tropospheric BrO and HCHO, an important element in air quality monitoring. Only limited results are currently available for OClO, an element in the destruction cycle of polar stratospheric ozone, due to the lack of OMI observations at a time of the year where OClO loading is significantly above the detection limit from space.
机译:臭氧监测仪(OMI)是在NASA的EOS-AURA卫星平台上在2004年7月15日推出的Nadir-View-UV /可见CCD光谱仪,进入Sun-Synchone,极性轨道,赤道交叉时间为13:45H (升序节点)。 OMI测量覆盖270-500nm的光谱区域,光谱分辨率在0.42nm和0.63nm之间,在Nadir的标称接地占地面积为13x24mm2。全球覆盖在一天内实现。 OMI测量的非常高的空间分辨率设定了从空间的痕量气体和空气质量监测的新标准。结合日常全球覆盖范围,这显着推进了对空气化学的突出问题的能力大大提高,包括测定中低纬度的兄弟源,作为纬度的职能,以及城市中甲醛的生产。发展中国家。我们概述了OMI仪器,并介绍了基于观察到的广告的直接,非线性拟合方法的兄弟,HCHO和OCLO的操作跟踪气体检索方案,包括用于光谱欠采样的校正。我们首先为对流层兄弟和Hcho提供的首先结果,是空气质量监测的重要因素。目前只有有限的结果可用于OCLO,由于缺乏OMI观测的oomlo载荷从空间的检测极限显着高于检测极限,因此偏离偏极平流层臭氧的破坏周期元素。

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