An internally consistent set of globally distributed atmospheric carbon monoxide mixing ratios developed using results from an intercomparison of measurements

被引:54
作者
Novelli, PC
Connors, VS
Reichle, HG
Anderson, BE
Brenninkmeijer, CAM
Brunke, EG
Doddridge, BG
Kirchhoff, VWJH
Lam, KS
Masarie, KA
Matsuo, T
Parrish, DD
Scheel, HE
Steele, LP
机构
[1] NOAA, Climate Monitoring & Diagnost Lab, Boulder, CO 80303 USA
[2] NASA, Langley Res Ctr, Hampton, VA 23681 USA
[3] Natl Inst Water & Atmospher Res, Inst Geol & Nucl Sci, Lower Hutt, New Zealand
[4] CSIR, EMATEK, AIM, Stellenbosch, South Africa
[5] Univ Maryland, Dept Meteorol, College Pk, MD 20742 USA
[6] Inst Nacl Pesquisas Espaciais, Sao Paulo, Brazil
[7] Hong Kong Polytech Inst, Dept Civil & Struct Engn, Hong Kong, Peoples R China
[8] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[9] Japan Meteorol Agcy, Tokyo, Japan
[10] NOAA, Aeron Lab, Boulder, CO 80303 USA
[11] Fraunhofer Inst Atmosphar Umweltforsch, D-8100 Garmisch Partenkirchen, Germany
[12] CSIRO, Div Atmospher Res, Aspendale, Vic 3195, Australia
关键词
D O I
10.1029/97JD00031
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The Measurement of Air Pollution from Satellite (MAPS) instrument measures carbon monoxide (CO) in the middle troposphere from a space platform. In anticipation of the deployment of MAPS aboard the space shuttle. Endeavor for two 10-day missions in 1994, plans were made to prepare a set of correlative measurements which would be used as part of the mission validation program. Eleven laboratories participated in the correlative measurement program by providing NASA with the results of their CO field programs during April and October 1994. Measurements of CO in the boundary layer, while not used in the MAPS validation, provide a picture of CO in the lower troposphere. Because measurements of CO made by different laboratories have been known to differ significantly, all correlative team members participated in an intercomparison of their measurements to define potential differences in techniques and calibration scales. While good agreement was found between some laboratories, there were differences between others. The use of similar analytical techniques and calibration scales did not always provide similar results. The results of the intercomparisons were used to normalize all ground-based measurements to the National Oceanic and Atmospheric Administration/Climate Monitoring and Diagnostics Laboratory CO reference scale. These data provide an internally consistent picture of CO in the lower atmosphere during spring and fall 1994.
引用
收藏
页码:19285 / 19293
页数:9
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