A persistent imbalance in HOx and NOx photochemistry of the upper troposphere driven by deep tropical convection

被引:152
作者
Prather, MJ [1 ]
Jacob, DJ
机构
[1] Univ Calif Irvine, Earth Syst Sci Dept, Irvine, CA 92697 USA
[2] Harvard Univ, Div Engn & Appl Sci, Dept Earth & Planetary Sci, Cambridge, MA 02138 USA
关键词
D O I
10.1029/97GL03027
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Convection in the tropics turns over the upper troposphere at rates (0.08 d(-1)) comparable to photochemical processes controlling the absolute abundance of HOx (OH + HO2) and the abundance of NOx (NO + NO2) relative to HNO3. Here we identify convection of boundary-layer CH3OOH as a primary source of HO, to the upper troposphere. Turnover of NOx leads to NO/HNO3 ratios much higher than predicted for local photochemical steady-state. Through convective transport the upper troposphere is more photochemically active in producing O-3, an important greenhouse gas.
引用
收藏
页码:3189 / 3192
页数:4
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