Tropospheric ozone variability over Singapore from August 1996 to December 1999

被引:10
作者
Yonemura, S
Tsuruta, H
Maeda, T
Kawashima, S
Sudo, S
Hayashi, M
机构
[1] Natl Inst Agroenvironm Sci, Tsukuba, Ibaraki 3058604, Japan
[2] AIST, Natl Inst Adv Ind Sci & Technol, Inst Environm Management Technol, Tsukuba, Ibaraki 3058569, Japan
[3] Tokyo Univ Informat Sci, Inage Ku, Chiba 2658501, Japan
关键词
ozonesonde; ENSO; biomass burning; tropics; Pacific Ocean;
D O I
10.1016/S1352-2310(01)00574-X
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Vertical ozone profiles over Singapore (lat 1degrees20'N, long 103degrees53'E) have been monitored by ozonesondes twice a month since August 1996. We report the vertical ozone profiles over Singapore from August 1996 to the end of 1999. During this time, large ozone enhancements occurred during three periods: March-June 1997, September-November 1997, and February-May 1998. These ozone enhancements were larger over Singapore than over Malaysia. Backward trajectory analyses revealed that the enhancements during September November 1997, and February-May 1998 were associated with biomass burning in Indonesia and Southeast Asia. Outside the three periods, ozone concentrations over Singapore differed from those over Malaysia by not more than 2.5% at altitudes of between 2.6 and 7.6 km and by not more than 12% at altitudes of between 1 and 13.5 km. The minimum ozone concentrations in the middle and the upper troposphere were about 20ppbv and were observed when the wind was easterly from the Pacific Ocean. Ozone concentrations at the bottom of the troposphere were near zero when the wind was southerly to westerly (from the larger, more urbanized and industrialized part of Singapore and the Strait of Malacca), implying that ozone-destroying reactions were occurring with high concentrations of urban pollutants. We conclude that the ozone enhancements observed in the free troposphere resulted from the effects of extensive biomass burning combined with the modified circulation (suppressed convection of maritime air masses) that occurs during El Nino events. (C) 2002 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:2061 / 2070
页数:10
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