NOx and O3 above a tropical rainforest: an analysis with a global and box model

被引:19
作者
Pike, R. C. [1 ]
Lee, J. D. [2 ]
Young, P. J. [1 ,3 ,4 ]
Carver, G. D. [1 ,5 ]
Yang, X. [1 ]
Warwick, N. [1 ]
Moller, S. [6 ]
Misztal, P. [7 ,8 ]
Langford, B. [9 ]
Stewart, D. [10 ]
Reeves, C. E. [10 ]
Hewitt, C. N. [9 ]
Pyle, J. A. [1 ,5 ]
机构
[1] Univ Cambridge, Dept Chem, Ctr Atmospher Sci, Cambridge CB2 1EW, England
[2] Univ York, NCAS, York YO10 5DD, N Yorkshire, England
[3] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[4] NOAA Earth Syst Res Lab, Boulder, CO USA
[5] Univ Cambridge, Natl Ctr Atmospher Sci Climate, Cambridge CB2 1TN, England
[6] Univ York, Dept Chem, York YO10 5DD, N Yorkshire, England
[7] Ctr Ecol & Hydrol Edinburgh, Penicuik EH26 0QB, Midlothian, Scotland
[8] Univ Edinburgh, Sch Chem, Edinburgh EH9 3JJ, Midlothian, Scotland
[9] Univ Lancaster, Lancaster Environm Ctr, Lancaster LA1 4YQ, England
[10] Univ E Anglia, Sch Environm Sci, Norwich NR4 7TJ, Norfolk, England
基金
英国自然环境研究理事会;
关键词
VOLATILE ORGANIC-COMPOUNDS; NITROGEN-OXIDES; TROPOSPHERIC OZONE; ATMOSPHERIC CHEMISTRY; DRY DEPOSITION; SENSITIVITY; ISOPRENE; IMPACT; PARAMETERIZATION; EMISSIONS;
D O I
10.5194/acp-10-10607-2010
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A cross-platform field campaign, OP3, was conducted in the state of Sabah in Malaysian Borneo between April and July of 2008. Among the suite of observations recorded, the campaign included measurements of NOx and O-3-crucial outputs of any model chemistry mechanism. We describe the measurements of these species made from both the ground site and aircraft. We then use the output from two resolutions of the chemistry transport model p-TOMCAT to illustrate the ability of a global model chemical mechanism to capture the chemistry at the rainforest site. The basic model performance is good for NOx and poor for ozone. A box model containing the same chemical mechanism is used to explore the results of the global model in more depth and make comparisons between the two. Without some parameterization of the nighttime boundary layer - free troposphere mixing (i.e. the use of a dilution parameter), the box model does not reproduce the observations, pointing to the importance of adequately representing physical processes for comparisons with surface measurements. We conclude with a discussion of box model budget calculations of chemical re-action fluxes, deposition and mixing, and compare these results to output from p-TOMCAT. These show the same chemical mechanism behaves similarly in both models, but that emissions and advection play particularly strong roles in influencing the comparison to surface measurements.
引用
收藏
页码:10607 / 10620
页数:14
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