Geophysical validation and long-term consistency between GOME-2/MetOp-A total ozone column and measurements from the sensors GOME/ERS-2, SCIAMACHY/ENVISAT and OMI/Aura

被引:29
作者
Koukouli, M. E. [1 ]
Balis, D. S. [1 ]
Loyola, D. [2 ]
Valks, P. [2 ]
Zimmer, W. [2 ]
Hao, N. [2 ]
Lambert, J. -C. [3 ]
Van Roozendael, M. [3 ]
Lerot, C. [3 ]
Spurr, R. J. D. [4 ]
机构
[1] Aristotle Univ Thessaloniki, Lab Atmospher Phys, GR-54006 Thessaloniki, Greece
[2] Deutsch Zentrum Luft & Raumfahrt DLR, Inst Method Fernerkundung IMF, D-82234 Oberpfaffenhofen, Germany
[3] Belgian Inst Space Aeron BIRA IASB, B-1180 Brussels, Belgium
[4] RT Solut Inc, Cambridge, MA USA
关键词
GOME;
D O I
10.5194/amt-5-2169-2012
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The main aim of the paper is to assess the consistency of five years of Global Ozone Monitoring Experiment2/Metop-A [GOME-2] total ozone columns and the long-term total ozone satellite monitoring database already in existence through an extensive inter-comparison and validation exercise using as reference Brewer and Dobson ground-based measurements. The behaviour of the GOME-2 measurements is being weighed against that of GOME (19952011), Ozone Monitoring Experiment [OMI] (since 2004) and the Scanning Imaging Absorption spectroMeter for Atmospheric CartograpHY [SCIAMACHY] (since 2002) total ozone column products. Over the background truth of the ground-based measurements, the total ozone columns are inter-evaluated using a suite of established validation techniques; the GOME-2 time series follow the same patterns as those observed by the other satellite sensors. In particular, on average, GOME-2 data underestimate GOME data by about 0.80 %, and underestimate SCIAMACHY data by 0.37% with no seasonal dependence of the differences between GOME-2, GOME and SCIAMACHY. The latter is expected since the three datasets are based on similar DOAS algorithms. This underestimation of GOME-2 is within the uncertainty of the reference data used in the comparisons. Compared to the OMI sensor, on average GOME-2 data underestimate OMI DOAS (collection 3) data by 1.28 %, without any significant seasonal dependence of the differences between them. The lack of seasonality might be expected since both the GOME data processor [GDP] 4.4 and OMI DOAS are DOAS-type algorithms and both consider the variability of the stratospheric temperatures in their retrievals. Compared to the OMI TOMS (collection 3) data, no bias was found. We hence conclude that the GOME-2 total ozone columns are well suitable to continue the long-term global total ozone record with the accuracy needed for climate monitoring studies.
引用
收藏
页码:2169 / 2181
页数:13
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