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Differences between ground Dobson, Brewer and satellite TOMS-8, GOME-WFDOAS total ozone observations at Hradec Kralove, Czech

机译:Dobson,Brewer地面卫星和TOMS-8卫星,GOME-WFDOAS卫星在捷克赫拉德茨Kralove的总臭氧观测值之间的差异

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This paper presents key results achieved by an analysis of the relationbetween high-quality simultaneous Dobson, Brewer ground and TOMS-V8,GOME-WFDOAS satellite total ozone observations for Hradec Kralove, CzechRepublic. Statistically significant seasonal differences with maxima up to4% of monthly averages have been found between Dobson and Brewermeasurements during the winter/spring months. These differences caninfluence estimations of ozone trends if combined data series are used afterreplacing a Dobson instrument by a Brewer spectrophotometer. The differencescan be attributed mostly to the influence of temperature on ozone absorptioncoefficients and to total sulphur dioxide. Similar seasonal differencesexist between Dobson, GOME and Brewer, TOMS data sets at Hradec Kralovewhile Dobson versus TOMS and Brewer versus GOME observations fit well witheach other within the instrumental accuracy of spectrophotometers. The abovefindings are supposed to be relevant to other mid and high latitude stationsand they have been confirmed by several independent analyses. Theconclusions should be considered by data users because the differencesbetween particular ground and satellite data sets can influence validationof satellite ozone observing systems and analyses of recovery of the ozonelayer in mid and high latitudes, among others.
机译:本文通过分析捷克共和国赫拉德茨·克拉洛韦的高质量同时多布森,布鲁尔地面和TOMS-V8,GOME-WFDOAS卫星总臭氧观测值之间的关系,得出了重要成果。在冬季/春季月份之间,在Dobson和Brewermeasurements之间发现了具有统计意义的季节性差异,最大值最高达到月平均值的4%。如果在用Brewer分光光度计替换Dobson仪器后使用组合数据序列,则这些差异可能会影响臭氧趋势的估计。差异主要归因于温度对臭氧吸收系数的影响以及总二氧化硫的影响。 Dobson,GOME和Brewer之间也存在类似的季节性差异,Hradec Kralove的TOMS数据集与此同时Dobson与TOMS和Brewer与GOME的观测值在分光光度计的仪器精度范围内彼此吻合。以上发现应该与其他中高纬度站有关,并且已经通过数次独立分析得到了证实。数据用户应考虑这一结论,因为特定地面和卫星数据集之间的差异会影响卫星臭氧观测系统的验证以及中高纬度臭氧层恢复的分析等。

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