Reactive nitrogen over the Pacific Ocean during PEM-West A

被引:53
作者
Kondo, Y
Ziereis, H
Koike, M
Kawakami, S
Gregory, GL
Sachse, GW
Singh, HB
Davis, DD
Merrill, JT
机构
[1] GEORGIA INST TECHNOL, SCH EARTH & ATMOSPHER SCI, ATLANTA, GA 30332 USA
[2] NASA, LANGLEY RES CTR, DIV ATMOSPHER SCI, HAMPTON, VA 23681 USA
[3] UNIV RHODE ISL, GRAD SCH OCEANOG, CTR ATMOSPHER CHEM STUDIES, NARRAGANSETT, RI 02882 USA
[4] NASA, AMES RES CTR, MOFFETT FIELD, CA 94035 USA
[5] DLR, INST PHYS ATMOSPHARE, D-82234 WESSELING, GERMANY
关键词
D O I
10.1029/95JD02611
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Measurements of NO and NOy were carried out during NASA's Pacific Exploratory Mission-West A. In total, 18 aircraft flights were made over the Pacific Ocean, predominantly over the western Pacific Ocean in September and October 1991. NO and NOy were measured using a chemiluminescence instrument, and NOx was calculated from NO using a chemical box model. The measurements were carried out from 0.3 to 12 km in altitude. The NO, calculated NOx ((NOx)(mc)), and NOy mixing ratios in continental air were significantly higher than in maritime air. In maritime air, NO increased with altitude. The median values of NO in the boundary layer and the lower, middle; and upper troposphere were 3.7, 5.1, 11.5, and 26.6 parts per trillion by volume (pptv), respectively. In continental air, NO and (NOx)(mc) mixing ratios revealed a C-shaped profile. The median NO values observed in the four altitude regions were 37.8, 17.5, 18.2, and 53.2 pptv, respectively. NOy did not show any apparent altitude dependence either in maritime or in continental air. In maritime air, median NOy values in the lower, middle, and upper troposphere ranged between 211 and 226 pptv and in continental air between 382 and 401 pptv. The lowest values of NOy, PAN, and O-3 were observed in tropical air masses throughout the entire altitude region. In the middle and upper troposphere of the high-latitude air masses, NO and (NOx)(mc) values were the lowest, although NOy mixing ratios were similar to those in continental air masses. PAN, O-3, CO, CH4, and C2H6 data were used to study the budget of reactive nitrogen over the Pacific Ocean. O-3 mixing ratios were found to be correlated with those of (NOx)(mc), NOy, PAN, and CH4, although the degree of correlation varied with air mass and altitude. These correlations, together with the profiles of these species, suggest that photochemical production of O-3 from precursor species over the continent is important for the O-3 budget in the troposphere over, the western Pacific Ocean.
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页码:1809 / 1828
页数:20
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