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THREE VALIDATION METHODS of SCIAMACHY and MIPAS-E DATA WITH DOAS MEASUREMENTS OBTAINED by the GASCOD/A4π SPECTROMETER on BOARD the GEOPHYSICA-M55 AIRCRAFT

机译:GEOPHYSICA-M55飞机板上GASCOD /A4π谱仪获得的Doas测量结果用于SCIAMACHY和MIPAS-E数据的三种验证方法

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The aim of this paper is to present three methods for the validation of the SCIAMACHY and MIPAS-E data using the UV/Vis. DOAS spectrometer, called GASCOD/A4π, installed on board the Geophysica M-55 aircraft, which can fly up to 20 km of altitude. The first method is the classic one of the cross-crossing that requires the temporal and spatial simultaneity of the measurements on board both the ENVISAT-1 satellite and the M55 aircraft. The second one is based on a Lagrangian approach, which allows for the identification of the best flight trajectory of the M55, on the basis of the dynamic and chemical "history" of the air masses at the aircraft altitude. In this case the comparison can be extended for longer time periods. The latter method is proposed to validate the tropospheric amounts of O_3 and NO_2. In fact, from SCIAMACHY data it can be possible to infer the tropospheric amounts of minor gases subtracting the stratospheric column, detected with limb measurements, from the total column obtained with subsequent nadir measurements. In the GASCOD/A4πdata the tropospheric gases amounts are directly observed by means of the nadir measurements, if the flight altitude is close up the tropopause level. Especially the latter two methods can be consider innovative techniques in the field of satellite data validation.
机译:本文的目的是介绍使用UV / Vis验证SCIAMACHY和MIPAS-E数据的三种方法。安装在地球物理M-55飞机上的DOAS光谱仪,称为GASCOD /A4π,可以飞行高达20 km的高度。第一种方法是经典的交叉方法,需要在ENVISAT-1卫星和M55飞机上同时进行时间和空间测量。第二种方法基于拉格朗日方法,该方法基于飞机高度处的空气团的动态和化学“历史”,可以确定M55的最佳飞行轨迹。在这种情况下,比较可以延长更长的时间。提出了后一种方法来验证对流层O_3和NO_2的量。实际上,从SCIAMACHY数据中,可以推断出对流层中的少量气体的对流层量,这些对流层中的气体减去了用肢体测量值测得的平流层柱,再减去随后的最低测量值获得的总柱数。如果飞行高度接近对流层顶水平,则在GASCOD /A4π数据中,对流层气体量可通过天底测量直接观察到。特别是后两种方法可以被认为是卫星数据验证领域中的创新技术。

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