Please use this identifier to cite or link to this item: http://197.159.135.214/jspui/handle/123456789/684
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dc.contributor.authorTiemoko, Toure Dro-
dc.contributor.authorRamonet, Michel-
dc.contributor.authorYoroba, Fidele-
dc.contributor.authorKouassi, Kobenan Benjamin-
dc.contributor.authorKouadio, Kouakou-
dc.contributor.authorKazan, Victor-
dc.contributor.authorKaiser, Claire-
dc.contributor.authorTruong, François-
dc.contributor.authorVuillemin, Cyrille-
dc.contributor.authorDelmotte, Marc-
dc.contributor.authorWastine, Benoit-
dc.contributor.authorCiais, Phillipe-
dc.date.accessioned2023-01-24T16:18:36Z-
dc.date.available2023-01-24T16:18:36Z-
dc.date.issued2020-12-
dc.identifier.otherhttps://doi.org/10.1080/16000889.2020.1863707-
dc.identifier.urihttp://197.159.135.214/jspui/handle/123456789/684-
dc.descriptionResearch Articleen_US
dc.description.abstractThe 10-year observations of the atmospheric molar fractions of CO2, CH4 and CO in West Africa were analyzed using a high precision measurement of the Lamto (LTO) station (6 31N and 5 02W) in C^ote d’Ivoire. At daily scale, high concentrations appear at night with significant peaks around 7 a.m. local time and minimum concentrations in the afternoon for CO2 and CH4. The CO concentrations show two peaks around 8 h and 20 h corresponding to the maximum in road traffic of a northern motorway located 14km from the station. The long-term increase rates of CH4 ( 7 ppb year 1) and CO2 ( 2.24ppm year 1) at Lamto are very close to global trends. The variations of the concentrations of the three gases show strong seasonality with a peak in January for all gases and minima in September for CO2 and CH4, and in June for CO. The CO variation suggests a significant impact of fires on the CO, CO2 and CH4 anomalies in the Lamto region during the dry season (December to February). CO and CH4 show strong correlations (at synoptic-scale and monthly based) in January (r¼0.84), February (r¼0.90), April (r¼0.74), November (r¼0.79) and December (r¼0.72) reflecting similar sources of emission for both gases. The trajectories of polluted air masses at LTO, also indicate continental sources of emission associated with Harmattan winds.en_US
dc.language.isoenen_US
dc.publisherTellus B: Chemical and Physical Meteorologyen_US
dc.subjectgreenhouse gasesen_US
dc.subjectcarbon dioxideen_US
dc.subjectmethaneen_US
dc.subjectcarbon monoxideen_US
dc.subjectLamtoen_US
dc.titleAnalysis of the temporal variability of CO2, CH4 and CO concentrations at Lamto, West Africaen_US
dc.typeArticleen_US
Appears in Collections:West African Climate Systems



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