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VALIDATION OF GOMOS VERTICAL PROFILES USING THE STRATOSPHERIC BALLOON-BORNE AMON AND SALOMON UV-VISIBLE SPECTROMETERS

机译:用球形球状硼原子和所罗门紫外可见分光光度计验证GOMOS垂直轮廓

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The stratospheric balloon-borne UV-visible spectrometers AMON and SALOMON, which use stars and Moon as light source, respectively, are involved in the validation of the UV-visible spectrometer GOMOS onboard ENVISAT, which uses also stars as light source. A low spectral resolution UV-visible spectrometer, AMON-RA, is also implanted in the AMON gondola, for the analysis of the chromatic scintillation effect. A flight of SALOMON occurred in September 19, 2002, at mid latitude from Aire sur l'Adour, France. An AMON (and AMON-RA) flight occurred at high latitude from Kiruna (northern Sweden) on March 1, 2003. The vertical profiles are compared to those obtained by GOMOS. Taking into account the effect of the chromatic scintillation on the transmission spectra, recommendations will be proposed in order to improve the GOMOS retrievals.
机译:平流层气球式紫外可见光谱仪AMON和SALOMON分别使用星和月亮作为光源,参与了ENVISAT机载紫外可见光谱仪GOMOS的验证,该光谱仪也使用星作为光源。低光谱分辨率的紫外可见光谱仪AMON-RA也被植入AMON吊篮中,用于分析彩色闪烁效应。 SALOMON航班于2002年9月19日从法国艾尔河畔阿杜尔中纬度发生。 2003年3月1日,从基律纳(瑞典北部)发生了一次高纬度的AMON(和AMON-RA)飞行。将垂直剖面与GOMOS获得的垂直剖面进行了比较。考虑到彩色闪烁对透射光谱的影响,将提出一些建议,以改进GOMOS的检索。

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