OMEGA long wavelength channel: Data reduction during non-nominal stages

被引:11
|
作者
Jouglet, Denis [1 ]
Poulet, Francois [1 ]
Langevin, Yves [1 ]
Bibring, Jean-Pierre [1 ]
Gondet, Brigitte [1 ]
Vincendon, Mathieu [1 ]
Berthe, Michel [1 ]
机构
[1] Univ Paris 11, Inst Astrophys Spatiale, F-91405 Orsay, France
关键词
Mars Express; OMEGA; Imaging spectroscopy; Calibration; Data analysis procedures; MARS; EXPRESS; PERFORMANCES; SURFACE; CLIMATE;
D O I
10.1016/j.pss.2008.07.025
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The Observatoire pour la Mineralogie, l'Eau, les Glaces et l'Activite (OMEGA) instrument is a visible and near-infrared imaging spectrometer on board the European Mars Express (MEx) mission. The on-board calibration (OBC) performed at the beginning of observations on each orbit reveals that the photometric response of the C channel (1.0-2.5 mu m) has been very stable since orbit insertion in January 2004. On the contrary the L channel (2.5-5.1 mu m) response has varied significantly during the mission, and only orbits for which the response is close to nominal could be used with confidence. The spatial coverage of ice-free surfaces in this wavelength range is consequently limited to only similar to 30%, mainly during northern spring and summer. This paper presents the empirical method used to derive new instrumental transfer functions (ITF) for the non-nominal orbits. This method consists of analyzing the variation of the signal between several observations of a same region acquired at nominal and non-nominal calibration states. In the cases where the mineralogy and the atmospheric conditions between the two observations are the same, the variation in reflectance spectra is only due to the ITF variation, which provides a new ITF. We then associate these new ITFs with their corresponding OBCs to model a relationship between both. The resulting model enables us to provide a new ITF for each orbit for which the OBC is available. The new ITFs derived for the entire dataset have been validated (1) through a comparison of the C and L channel global albedo trends and (2) through a comparison of the surface temperatures derived from the L channel with those calculated from the General Circulation Model (GCM) numerical simulation of the LIVID released in the Martian Climate Database. The non-nominal data processed with adapted ITFs for orbits up to 3050 increase the non-icy surface coverage of Mars to similar to 70% including all seasons. (C) 2008 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1032 / 1042
页数:11
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