Measurements of trace gases in the tropical tropopause layer

被引:25
作者
Marcy, T. P.
Popp, P. J.
Gao, R. S.
Fahey, D. W.
Ray, E. A.
Richard, E. C.
Thompson, T. L.
Atlas, E. L.
Loewenstein, M.
Wofsy, S. C.
Park, S.
Weinstock, E. M.
Swartz, W. H.
Mahoney, M. J.
机构
[1] Natl Ocean & Atmospher Adm, Earth Syst Res Lab, Div Chem Sci, Boulder, CO 80305 USA
[2] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[3] Univ Colorado, Atmospher & Space Phys Lab, Boulder, CO 80309 USA
[4] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Miami, FL 33149 USA
[5] NASA, Ames Res Ctr, Moffett Field, CA 94035 USA
[6] Harvard Univ, Natl Inst Global & Environm Change, Cambridge, MA 02138 USA
[7] Harvard Univ, Dept Chem & Chem Biol, Cambridge, MA 02138 USA
[8] Johns Hopkins Univ, Appl Phys Lab, Laurel, MD 20723 USA
[9] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
基金
美国国家航空航天局;
关键词
tropical; tropopause; stratosphere; hydrochloric acid; ozone;
D O I
10.1016/j.atmosenv.2007.05.032
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A unique dataset of airborne in situ observations of HCl, O-3, HNO3, H2O, CO, CO2 and CH3Cl has been made in and near the tropical tropopause layer (TTL). A total of 16 profiles across the tropopause were obtained at latitudes between 10 degrees N and 3 degrees S from the NASA WB-57F high-altitude aircraft flying from Costa Rica. Few in situ measurements of these gases, particularly HCl and HNO3, have been reported for the TTL. The general features of the trace gas vertical profiles are consistent with the concept of the TTL as distinct from the lower troposphere and lower stratosphere. A combination of the tracer profiles and correlations with O-3 is used to show that a measurable amount of stratospheric air is mixed into this region. The HCl measurements offer an important constraint on stratospheric mixing into the TTL because once the contribution from halocarbon decomposition is quantified, the remaining HCl (> 60% in this study) must have a stratospheric source. Stratospheric HCl in the TTL brings with it a proportional amount of stratospheric O-3. Quantifying the sources Of O-3 in the TTL is important because O-3 is particularly effective as a greenhouse gas in the tropopause region. (c) 2007 Elsevier Ltd. All rights reserved.
引用
收藏
页码:7253 / 7261
页数:9
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