Ozone destruction and production rates between spring and autumn in the Arctic stratosphere
Ozone destruction and production rates between spring and autumn in the Arctic stratosphere
复制标题
北极平流层春季和秋季之间的臭氧破坏和生产率
DOI:
10.1029/2000gl011404
复制
发表时间:
2000
影响因子:
5.2
通讯作者:
T. Bui
中科院分区:
文献类型:
--
作者:
D. W. Fahey;R. Gao;L. A. D. Negro;E. Keim;S. R. Kawa;R. Salawitch;P. Wennberg;T. Hanisco;E. Lanzendorf;K. K. Perkins;Steven A. Lloyd;William H. Swartz;M. Proffitt;J. Margitan;James C. Wilson;R. Stimpfle;R. C. Cohen;C. T. McElroy;C. R. Webster;M. Loewenstein;J. W. Elkins;T. Bui
In situ measurements of radical and long‐lived species were made in the lower Arctic stratosphere (18 to 20 km) between spring and early autumn in 1997. The measurements include O3, ClO, OH, HO2, NO, NO2, N2O, CO, and overhead O3. A photochemical box model constrained by these and other observations is used to compute the diurnally averaged destruction and production rates of O3 in this region. The rates show a strong dependence on solar exposure and ambient O3. Total destruction rates, which reach 19%/month in summer, reveal the predominant role of NOx and HOx catalytic cycles throughout the period. Production of O3 is significant only in midsummer air parcels. A comparison of observed O3 changes with destruction rates and transport effects indicates the predominant role of destruction in spring and an increased role of transport by early autumn.