Open AccessRegional background ozone and carbon monoxide variations in remote Siberia/East Asia
Author(s) -
Pochanart Pakpong,
Akimoto Hajime,
Kajii Yoshizumi,
Potemkin Vladimir M.,
Khodzher Tamara V.
Publication year - 2003
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2001jd001412
Subject(s) - air mass (solar energy) , environmental science , troposphere , atmospheric sciences , latitude , mixing ratio , northern hemisphere , climatology , atmosphere (unit) , ozone , southern hemisphere , east asia , air pollution , geology , geography , meteorology , chemistry , physics , geodesy , boundary layer , archaeology , organic chemistry , china , thermodynamics
Continuous measurements of O 3 and CO were made during 1997–1999 at Mondy, a remote mountain site in East Siberia, in order to quantify their mixing ratios and their climatology in the “background” troposphere of continental Eurasia. The seasonal cycles of O 3 and CO show the spring maximum‐summer minimum similar to that previously reported in the remote Northern Hemisphere. The influences of Siberian forest fires on the variations of CO mixing ratios at Mondy were observed both on a local and a regional scale during spring 1997 and fall 1998, respectively. We further evaluate the possible impact of European pollution export to the remote atmosphere of Siberia using trajectory analysis. It was found that the O 3 and CO mixing ratios in the air masses transported from Europe are higher than those from Siberia and high‐latitude regions for most of the year. The medians of O 3 and CO mixing ratios associated with the European air masses are 44.2 and 134 ppb, respectively, in comparison with 42.7 and 128 ppb in the Siberian air masses, and 41.0 and 110 ppb in the high‐latitude air masses. The residence time analysis of air masses transported from the European continent indicates that CO mixing ratios significantly decrease with longer transport time of air masses from Europe, while rapid air motion retains higher CO mixing ratios in every season due to the admixture of polluted European air into the continental background air during air mass transport over Eurasia and photochemical loss by OH. Because of a shorter lifetime in summer, CO mixing ratios decrease at a rate of 6–7 ppb per day, while they decrease at a rate of 2–4 ppb per day in winter and spring. The similar trend is found for O 3 but only in summer, at a rate of 2–3 ppb per day. From this analysis, we are able to identify that European pollution exerts an influence, though not very strong, on the background O 3 and CO at Mondy in remote Siberia/East Asia.