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- W2550873475 startingPage "14041" @default.
- W2550873475 abstract "Abstract. The largest 7 Southeast Asian Studies (7SEAS) operation period within the Maritime Continent (MC) occurred in the August–September 2012 biomass burning season. Included was an enhanced deployment of Aerosol Robotic Network (AERONET) sun photometers, multiple lidars, and field measurements to observe transported smoke and pollution as it left the MC and entered the southwest monsoon trough. Here we describe the nature of the overall 2012 southwest monsoon (SWM) and biomass burning season to give context to the 2012 deployment. The MC in 2012 was in a slightly warm El Niño/Southern Oscillation (ENSO) phase and with spatially typical burning activity. However, overall fire counts for 2012 were 10 % lower than the Reid et al. (2012) baseline, with regions of significant departures from this norm, ranging from southern Sumatra (+30 %) to southern Kalimantan (−42 %). Fire activity and monsoonal flows for the dominant burning regions were modulated by a series of intraseasonal oscillation events (e.g., Madden–Julian Oscillation, or MJO, and boreal summer intraseasonal oscillation, or BSISO). As is typical, fire activity systematically progressed eastward over time, starting with central Sumatran fire activity in June related to a moderately strong MJO event which brought drier air from the Indian Ocean aloft and enhanced monsoonal flow. Further burning in Sumatra and Kalimantan Borneo occurred in a series of significant events from early August to a peak in the first week of October, ending when the monsoon started to migrate back to its wintertime northeastern flow conditions in mid-October. Significant monsoonal enhancements and flow reversals collinear with tropical cyclone (TC) activity and easterly waves were also observed. Islands of the eastern MC, including Sulawesi, Java, and Timor, showed less sensitivity to monsoonal variation, with slowly increasing fire activity that also peaked in early October but lingered into November. Interestingly, even though fire counts were middling, resultant AERONET 500 nm aerosol optical thickness (AOT) from fire activity was high, with maximums of 3.6 and 5.6 in the Sumatra and Kalimantan source regions at the end of the burning season and an average of ∼ 1. AOTs could also be high at receptor sites, with a mean and maximum of 0.57 and 1.24 in Singapore and 0.61 and 0.8 in Kuching Sarawak. Ultimately, outside of the extreme 2015 El Niño event, average AERONET AOT values were higher than any other time since sites were established. Thus, while satellite fire data, models, and AERONET all qualitatively agree on the nature of smoke production and transport, the MC's complex environment resulted in clear differences in quantitative interpretation of these datasets." @default.
- W2550873475 created "2016-11-30" @default.
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- W2550873475 date "2016-11-15" @default.
- W2550873475 modified "2023-10-15" @default.
- W2550873475 title "Aerosol meteorology of the Maritime Continent for the 2012 7SEAS southwest monsoon intensive study – Part 1: regional-scale phenomena" @default.
- W2550873475 cites W1517586166 @default.
- W2550873475 cites W1552878622 @default.
- W2550873475 cites W1670727398 @default.
- W2550873475 cites W1777755047 @default.
- W2550873475 cites W1973401183 @default.
- W2550873475 cites W1975278507 @default.
- W2550873475 cites W1975875502 @default.
- W2550873475 cites W1978811262 @default.
- W2550873475 cites W1979268012 @default.
- W2550873475 cites W1980301788 @default.
- W2550873475 cites W1984004659 @default.
- W2550873475 cites W1988889904 @default.
- W2550873475 cites W1995570940 @default.
- W2550873475 cites W1996076162 @default.
- W2550873475 cites W2001182515 @default.
- W2550873475 cites W2008656738 @default.
- W2550873475 cites W2011329066 @default.
- W2550873475 cites W2013376231 @default.
- W2550873475 cites W2015896147 @default.
- W2550873475 cites W2015980123 @default.
- W2550873475 cites W2020306346 @default.
- W2550873475 cites W2022315359 @default.
- W2550873475 cites W2022467764 @default.
- W2550873475 cites W2023227600 @default.
- W2550873475 cites W2025453528 @default.
- W2550873475 cites W2025713353 @default.
- W2550873475 cites W2029823326 @default.
- W2550873475 cites W2030115968 @default.
- W2550873475 cites W2046684780 @default.
- W2550873475 cites W2050460160 @default.
- W2550873475 cites W2053338693 @default.
- W2550873475 cites W2059603179 @default.
- W2550873475 cites W2062301433 @default.
- W2550873475 cites W2062454942 @default.
- W2550873475 cites W2064784699 @default.
- W2550873475 cites W2068166470 @default.
- W2550873475 cites W2069785523 @default.
- W2550873475 cites W2071123370 @default.
- W2550873475 cites W2071352614 @default.
- W2550873475 cites W2071562732 @default.
- W2550873475 cites W2081155601 @default.
- W2550873475 cites W2082426215 @default.
- W2550873475 cites W2089433206 @default.
- W2550873475 cites W2101394945 @default.
- W2550873475 cites W2103226654 @default.
- W2550873475 cites W2103977502 @default.
- W2550873475 cites W2104083727 @default.
- W2550873475 cites W2113458380 @default.
- W2550873475 cites W2134144766 @default.
- W2550873475 cites W2135832014 @default.
- W2550873475 cites W2140936007 @default.
- W2550873475 cites W2149888895 @default.
- W2550873475 cites W2150516764 @default.
- W2550873475 cites W2151585494 @default.
- W2550873475 cites W2160508458 @default.
- W2550873475 cites W2160818201 @default.
- W2550873475 cites W2166229287 @default.
- W2550873475 cites W2173251738 @default.
- W2550873475 cites W2174111397 @default.
- W2550873475 cites W2176050019 @default.
- W2550873475 cites W2320145997 @default.
- W2550873475 cites W2339405093 @default.
- W2550873475 cites W2555833850 @default.
- W2550873475 cites W4232453345 @default.
- W2550873475 doi "https://doi.org/10.5194/acp-16-14041-2016" @default.
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