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Intercomparison of ILAS-II version 1.4 and version 2 target parameters with MIPAS-Envisat measurements

机译:ILAS-II 1.4版和2版目标参数与MIPAS-Envisat测量值之间的比较

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This paper assesses the mean differences between the two ILAS-II dataversions (1.4 and 2) by comparing them with MIPAS measurements made betweenMay and October 2003. For comparison with ILAS-II results, MIPAS dataprocessed at the Institut für Meteorologie und Klimaforschung, Karlsruhe,Germany (IMK) in cooperation with the Instituto de Astrofísica deAndalucía (IAA) in Granada, Spain, were used. The coincidencecriteria of ±300 km in space and ±12 h in time for H2O,N2O, and CH4 and the coincidence criteria of ±300 km in space and±6 h in time for ClONO2, O3, and HNO3 were used. The ILAS-IIdata were separated into sunrise (= Northern Hemisphere) and sunset (=Southern Hemisphere). For the sunrise data, a clear improvement from version1.4 to version 2 was observed for H2O, CH4, ClONO2, and O3. Inparticular, the ILAS-II version 1.4 mixing ratios of H2O and CH4 wereunrealistically small, and those of ClONO2 above altitudes of 30 kmunrealistically large. For N2O and HNO3, there were no largedifferences between the two versions. Contrary to the Northern Hemisphere,where some exceptional profiles deviated significantly from knownclimatology, no such outlying profiles were found in the Southern Hemispherefor both versions. Generally, the ILAS-II version 2 data were in betteragreement with the MIPAS data than the version 1.4, and are recommended forquantitative analysis in the stratosphere. For H2O data in the Southern Hemisphere, further data quality evaluation is necessary.
机译:本文通过将两个ILAS-II数据版本(1.4和2)与2003年5月至2003年10月之间进行的MIPAS测量结果进行比较,来评估它们之间的平均差异。为了与ILAS-II结果进行比较,MIPAS数据由位于卡尔斯鲁厄的气象学与气候研究所进行了处理,使用了德国(IMK)与西班牙格拉纳达的安达卢西亚大学(IAA)合作。 H 2 O,N 2 O和CH 4 在空间上±300 km,时间±12 h的重合标准和重合ClONO 2 ,O 3 和HNO 3 的空间±300 km和时间±6 h的标准。 ILAS-II数据分为日出(=北半球)和日落(=南半球)。对于日出数据,H 2 O,CH 4 ,ClONO 2 和CH 2 O的版本从版本1.4明显改善到版本2。 O 3 。特别是,H 2 O和CH 4 的ILAS-II版本1.4混合比过小,而ClONO 2 高于30非常大。对于N 2 O和HNO 3 ,两个版本之间没有很大差异。与北半球相反,在北半球,一些例外的剖面与已知的气候学有显着差异,而在南半球,两个版本都没有发现这样的异常剖面。通常,与1.4版相比,ILAS-II第2版数据与MIPAS数据具有更好的一致性,建议在平流层中进行定量分析。对于南半球的H 2 O数据,有必要进一步评估数据质量。

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