2004
DOI: 10.5194/acp-4-1311-2004
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Around the world in 17 days - hemispheric-scale transport of forest fire smoke from Russia in May 2003

Abstract: Abstract. In May 2003, severe forest fires in southeast Russia resulted in smoke plumes extending widely across the Northern Hemisphere. This study combines satellite data from a variety of platforms (Moderate Resolution Imaging Spectroradiometer (MODIS), Sea-viewing Wide Field-of-view Sensor (SeaWiFS), Earth Probe Total Ozone Mapping Spectrometer (TOMS) and Global Ozone Monitoring Experiment (GOME)) and vertical aerosol profiles derived with Raman lidar measurements with results from a Lagrangian particle dis… Show more

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Cited by 258 publications
(243 citation statements)
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“…Damoah et al (2004) found good agreement between these both data sets for 17 days for trajectories along the Arctic circumference. For the data presented here a connection between the Khabarovsk or biomass burning event and the observations on NP-35 on March 17 seems to be clear.…”
Section: Discussionsupporting
confidence: 51%
“…Damoah et al (2004) found good agreement between these both data sets for 17 days for trajectories along the Arctic circumference. For the data presented here a connection between the Khabarovsk or biomass burning event and the observations on NP-35 on March 17 seems to be clear.…”
Section: Discussionsupporting
confidence: 51%
“…One such example was detected at Tõravere by observations of two instruments, actinometer and the AERONET photometer, on 28 May 2003. However, this kind of global-scale transport of forest fire smoke is rather exceptional [Damoah et al, 2004].…”
Section: Some Regional Features In Variability Of Column Transparencymentioning
confidence: 99%
“…Subsequently, only the data relative to the four summer months from June to September were considered when calculating the long-term variations of AOD, with the background contribution hereafter referred to as BG, and enhancements attributed to extinction mainly by smoke particles from boreal forest fires (hereafter referred to as FFS) in North America and Siberia (Forster et al, 2001;Damoah et al, 2004;Stohl et al, 2006;Tunved et al, 2006). Following the same approach used by Tomasi et al (2007), this summer-time analysis ignores influences of AH and/or Asian dust (AD) that occur mainly during late winter and spring (Rahn et al, 1977;Shaw, 1982Shaw, , 1983VanCuren and Cahill, 2002;Stone et al, 2007;Quinn et al, 2007).…”
Section: Long-term Variations In Aerosol Optical Depth At Arctic Sitesmentioning
confidence: 99%