G2TT
来源类型Articles
规范类型论文
DOIhttps://doi.org/10.1029/2018JD028533
ISSN2169-8996
Role of the Madden-Julian Oscillation in the transport of smoke from Sumatra to the Malay Peninsula during severe non-El Nino haze events
Boyd, W.; Stickler, C.; Duchelle, A.E.; Seymour, F.; Nepstad, D.; Bahar, N.H.A.; Rodriguez-Ward, D.
发表日期2018
出处Journal of Geophysical Research: Atmospheres
出版年2018
语种英语
摘要

In June 2013, the Malay Peninsula experienced severe smoke pollution, with daily surface particulate matter (PM) concentrations in Singapore greater than 350 µg m-3, over two times the air quality standard for daily mean PM10 set by the U.S. Environmental Protection Agency. Unlike most haze episodes in the Malay Peninsula in recent decades (e.g., the September 2015 event), the June 2013 haze occurred in the absence of an El Nino, during negative Indian Ocean Dipole conditions, with smoke carried eastward to the Peninsula from fires in the Riau province of central Sumatra. We show that June 2013 was not an exceptional event; inspection of visibility data during 2005-2015 reveals two other severe haze events in the Malay Peninsula (August 2005 and October 2010) occurring under similar conditions. Common to all three events was a combination of anomalously strong westerly winds over Riau province concurrent with late phases of the Realtime Multivariate Madden-Julian Oscillation (RMM) Index, during negative phases of the Indian Ocean Dipole. Our work suggests that identifying the meteorological mechanism driving these westerly wind anomalies could help stakeholders prepare for future non-El Nino haze events in Singapore and the Malay Peninsula.

主题fire ; fire effects ; smoke ; air pollution ; El Nino-Southern Oscillation
区域Indonesia
URLhttps://www.cifor.org/library/6910/
来源智库Center for International Forestry Research (Indonesia)
引用统计
资源类型智库出版物
条目标识符http://119.78.100.153/handle/2XGU8XDN/93893
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Boyd, W.,Stickler, C.,Duchelle, A.E.,et al. Role of the Madden-Julian Oscillation in the transport of smoke from Sumatra to the Malay Peninsula during severe non-El Nino haze events. 2018.
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