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Validation and data characteristics of methane and nitrous oxide profiles observed by MIPAS and processed with Version 4.61 algorithm

The ENVISAT validation programme for the atmospheric instruments MIPAS, SCIAMACHY and GOMOS is based on a number of balloon-bone, aircraft and ground-based correlative measurements. In particular the activities of validation scientists were coordinated by ESA within the ENVISAT Stratospheric Aircraf...

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Bibliographic Details
Published in:Atmospheric chemistry and physics discussions 2007-12, Vol.7 (6), p.18043-18111
Main Authors: Payan, S, Camy-Peyret, C, Oelhaf, H, Wetzel, G, Maucher, G, Keim, C, Pirre, M, Huret, N, Engel, A, Volk, M C, Kuellmann, H, Kuttippurath, J, Cortesi, U, Bianchini, G, Mencaraglia, F, Raspollini, P, Redaelli, G, Vigouroux, C, Maziere, MDe, Mikuteit, S, Blumenstock, T, Velazco, V, Notholt, J, Mahieu, M, Duchatelet, P, Smale, D, Wood, S, Jones, N, Piccolo, C, Payne, V, Bracher, A, Glatthor, N, Stiller, G, Grunow, K, Jeseck, P, Te, Y, Pfeilsticker, K, Butz, A
Format: Article
Language:English
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Summary:The ENVISAT validation programme for the atmospheric instruments MIPAS, SCIAMACHY and GOMOS is based on a number of balloon-bone, aircraft and ground-based correlative measurements. In particular the activities of validation scientists were coordinated by ESA within the ENVISAT Stratospheric Aircraft and Balloon Campaign of ESABC. As part of a series of similar papers on other species [this issue] and in parallel to the contribution of the individual validation teams, the present paper provides a synthesis of comparisons performed between MIPAS CH sub(4) and N sub(2)O profiles produced by the current ESA operational software (Instrument Processing Facility version 4.61 or IPF v4.61) and correlative measurements obtained from balloon and aircraft experiments as well as from satellite sensors or from ground-based instruments. The MIPAS-E CH sub(4) values show a positive bias in the lower stratosphere of about 10%. In case of N sub(2)O no systematic deviation with respect to the validation experiments could be identified. The individual used MIPAS data version 4.61 still exhibits some unphysical oscillations in individual CH sub(4) and N sub(2)O profiles caused by the processing algorithm (with almost no regularization). Taking these problems into account, the MIPAS CH sub(4) and N sub(2)O profiles are behaving as expected from the internal error estimation of IPF v4.61.
ISSN:1680-7367
1680-7375