Tropospheric and stratospheric ozone profiles during the 2019 TROpomi vaLIdation eXperiment (TROLIX-19)

被引:6
作者
Sullivan, John T. [1 ]
Apituley, Arnoud [2 ]
Mettig, Nora [3 ]
Kreher, Karin [4 ]
Knowland, K. Emma [1 ,5 ]
Allaart, Marc [2 ]
Piters, Ankie [2 ]
Van Roozendael, Michel [6 ]
Veefkind, Pepijn [2 ]
Ziemke, Jerry R. [1 ,5 ]
Kramarova, Natalya [1 ]
Weber, Mark [3 ]
Rozanov, Alexei [3 ]
Twigg, Laurence [1 ,7 ]
Sumnicht, Grant [1 ,7 ]
McGee, Thomas J. [1 ]
机构
[1] NASA, Goddard Space Flight Ctr, Code 916, Greenbelt, MD 20771 USA
[2] Royal Netherlands Meteorol Inst KNMI, De Bilt, Netherlands
[3] Univ Bremen, Inst Environm Phys, Bremen, Germany
[4] BK Sci GmbH, Mainz, Germany
[5] Morgan State Univ, Goddard Earth Sci Technol & Res GESTAR II, Baltimore, MD 21239 USA
[6] Royal Belgian Inst Space Aeron BIRA IASB, Uccle, Belgium
[7] Sci Syst & Applicat Inc, Lanham, MD 20706 USA
关键词
MAX-DOAS; RETRIEVAL; LIDAR; UV; OZONESONDES; ALGORITHMS; RESOLUTION; TRENDS;
D O I
10.5194/acp-22-11137-2022
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A TROPOspheric Monitoring Instrument (TROPOMI) validation campaign was held in the Netherlands based at the CESAR (Cabauw Experimental Site for Atmospheric Research) observatory during September 2019. The TROpomi vaLIdation eXperiment (TROLIX-19) consisted of active and passive remote sensing platforms in conjunction with several balloon-borne and surface chemical (e.g., ozone and nitrogen dioxide) measurements. The goal of this joint NASA-KNMI geophysical validation campaign was to make intensive observations in the TROPOMI domain in order to be able to establish the quality of the L2 satellite data products under realistic conditions, such as non-idealized conditions with varying cloud cover and a range of atmospheric conditions at a rural site. The research presented here focuses on using ozone lidars from NASA's Goddard Space Flight Center to better evaluate the characterization of ozone throughout TROLIX-19. Results of comparisons to the lidar systems with balloon, space-borne and ground-based passive measurements are shown. In addition, results are compared to a global coupled chemistry meteorology model to illustrate the vertical variability and columnar amounts of both tropospheric and stratospheric ozone during the campaign period.
引用
收藏
页码:11137 / 11153
页数:17
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