In situ measurements of HNO3, NOy, NO, and O3 in the lower stratosphere and upper troposphere

被引:46
|
作者
Neuman, JA
Gao, RS
Fahey, DW
Holecek, JC
Ridley, BA
Walega, JG
Grahek, FE
Richard, EC
McElroy, CT
Thompson, TL
Elkins, JW
Moore, FL
Ray, EA
机构
[1] NOAA, Aeron Lab, Boulder, CO 80305 USA
[2] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[3] Natl Ctr Atmospher Res, Boulder, CO 80307 USA
[4] Meteorol Serv Canada, Downsview, ON M3H 5T4, Canada
[5] NOAA, Climate Monitoring & Diagnost Lab, Boulder, CO 80305 USA
基金
美国国家航空航天局; 美国国家科学基金会;
关键词
photochemistry; tropopause; CIMS; ACCENT; nitrogen oxides;
D O I
10.1016/S1352-2310(01)00354-5
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In situ measurements of nitric acid (HNO3), reactive nitrogen (NOgamma), nitric oxide (NO), and ozone (O-3) made in the upper troposphere (UT) and lower stratosphere (LS) between 29 degrees and 33 degreesN latitudes during September 1999 are used to examine NOgamma partitioning and correlations between the measured species in these regions. The fast-response (1 s) HNO3 measurements are acquired with a new autonomous CIMS instrument. In the LS, HNO3 accounts for the majority of NOgamma and the sum of HNO3 and NOx accounts for approximately 90% of NOgamma. In the UT, the sum of HNO3 and NOx varies between 40% and 100% of NOgamma. Both HNO3 and NOgamma are strongly positively correlated with O-3, with larger correlation slopes in the UT than in the LS. In the UT at low values of the quantity (NOgamma-NOx-HNO3) it is uncorrelated with O-3, while at higher values, a positive correlation with O-3 is found. Of these two air mass types, those with higher (NOgamma NOx-HNO3) mixing ratios are likely associated with the presence of peroxyacetyl nitrate (PAN) that is produced by NOx-hydrocarbon chemistry. (C) 2001 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:5789 / 5797
页数:9
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