Validation of the MetOp-A total ozone data from GOME-2 and IASI using reference ground-based measurements at the Iberian Peninsula

被引:39
|
作者
Anton, M. [1 ]
Loyola, D. [2 ]
Clerbaux, C. [3 ]
Lopez, M. [4 ]
Vilaplana, J. M. [5 ]
Banon, M. [4 ]
Hadji-Lazaro, J. [3 ]
Valks, P. [2 ]
Hao, N. [2 ]
Zimmer, W. [2 ]
Coheur, P. F. [6 ]
Hurtmans, D. [6 ]
Alados-Arboledas, L. [1 ]
机构
[1] Univ Granada, Dept Fis Aplicada, Granada 18006, Spain
[2] German Aerosp Ctr DLR, Remote Sensing Technol Inst IMF, Wessling, Germany
[3] Univ Versailles, Univ Paris 06, CNRS INSU, LATMOS IPSL, Paris, France
[4] AEMet, Madrid, Spain
[5] INTA, Estn Sondeos Atmosfer El Arenosillo, Huelva, Spain
[6] Univ Libre Bruxelles, CQP, Brussels, Belgium
关键词
Ozone; Validation; MetOp-A; GOME-2; IASI; Brewer spectrophotometer; BREWER; DISTRIBUTIONS;
D O I
10.1016/j.rse.2011.01.018
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
One of the most important atmospheric composition products derived from the first EUMETSAT Meteorological Operational satellite (MetOp-A) is the total ozone column (TOC). For this purpose, MetOp-A has two instruments on board: the Global Ozone Monitoring Experiment 2 (GOME-2) that retrieves the TOC data from the backscattered solar ultraviolet-visible (UV-Vis) radiance, and the Infrared Atmospheric Sounding Interferometer (IASI) that uses the thermal infrared radiance to derive TOC data. This paper focuses on the simultaneous validation of the TOC data provided by these two MetOp-A instruments using the measurements recorded by five well-calibrated Brewer UV spectrophotometers located at the Iberian Peninsula during the complete 2009. The results show an excellent correlation between the ground-based data and the GOME-2 and IASI satellite observations (R-2 higher than 0.91). Differences between the ground-based and satellite TOC data show that the IASI instrument significantly overestimates the Brewer measurements (about 4.4% when all five ground-based stations are jointly used). In contrast, the GOME-2 instrument shows a slight underestimation (similar to 1.6%). In addition, the absolute relative differences between the Brewer and GOME-2 data are quite smaller (about a factor higher than 2) than the Brewer-IASI absolute differences. The satellite viewing geometry (solar zenith angle and the view zenith angle) has no significant influence on the Brewer-satellite relative differences. Moreover, the analysis of these relative differences with respect to the ground-based TOC data indicates that GOME-2 instrument presents a slight underestimation for high TOC values. Finally, the IASI-GOME-2 correlation is high (R-2 similar to 0.92), but with a mean relative difference of about +/- 6% which could be associated with the bias between UV-Vis and infrared spectroscopy used in the retrieval processes. (C) 2011 Elsevier Inc. All rights reserved.
引用
收藏
页码:1380 / 1386
页数:7
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