2010
DOI: 10.1029/2010jd013994
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Analysis of the origin of the distribution of CO in the subtropical southern Indian Ocean in 2007

Abstract: International audienceWe show carbon monoxide (CO) distributions at different vertical levels over the subtropical southern Indian Ocean, analyzing an observation campaign using Fourier transform infrared (FTIR) solar absorption spectrometry performed in 2007 at Reunion Island (21°S, 55°E). The CO pollution levels detected by the FTIR measurements during the campaign show a doubling of the CO total columns during the Southern Hemisphere biomass burning season. Using correlative data from the Measurement of Pol… Show more

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Cited by 56 publications
(91 citation statements)
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“…LACYTRAJ is a kinematic back trajectory code using the ECMWF wind field developed at the Laboratoire de l'Atmosphere et des Cyclones (LACy, France) (Baray et al, 2012;Clain et al, 2010;Duflot et al, 2010). This code was used to determine the sources of the air masses arriving above Cabauw.…”
Section: Back Trajectory Model: Lacytrajmentioning
confidence: 99%
“…LACYTRAJ is a kinematic back trajectory code using the ECMWF wind field developed at the Laboratoire de l'Atmosphere et des Cyclones (LACy, France) (Baray et al, 2012;Clain et al, 2010;Duflot et al, 2010). This code was used to determine the sources of the air masses arriving above Cabauw.…”
Section: Back Trajectory Model: Lacytrajmentioning
confidence: 99%
“…Reunion Island is a tropical island located in the southwestern part of the Indian Ocean at 20.8 • S and 55.5 • E. It is seasonally impacted by biomass burning plumes transported from southern Africa, South America and south-eastern Asia which can significantly affect the free tropospheric concentrations of O 3 and other pollutants like CO (Edwards et al, 2006 ;Duflot et al, 2010). Moreover, it is affected by stratospheric intrusions associated with the dynamical influence of the subtropical jet stream (Baray et al, 1998;Clain et al, 2010) and the tropical cyclone deep convection (Leclair De Bellevue et al, 2006).…”
Section: Introductionmentioning
confidence: 99%
“…Each cluster of trajectories is calculated every 15 min for 48 h of back-trajectories, for each day of precipitation sampling with a starting vertical level defined using ERA-Interim humidity and cloud parameters, and varying from 1 to 5 km. LACYTRAJ has previously been used to study long-range inter-hemispheric transport of carbon monoxide [38], interactions between the mixing layer and the free troposphere [39] or jet stream dynamics [40]. Based on previous studies of the atmosphere at this site [41], we distinguished categories in the geographical origin of air masses; here 3 sectors were defined: West (air masses from the Atlantic Ocean), North-East (Continental source) and South (Mediterranean Sea).…”
Section: Meteorological Data and Backward Trajectory Plotsmentioning
confidence: 99%