Studies on CO variation and trends over South Africa and the Indian Ocean using TES satellite data

Abstract : In this study, we used measurements from the tropospheric emission spectrometer aboard the Earth Observing System's Aura satellite over South Africa, Madagascar and Reunion Island to investigate variations and trends in tropospheric carbon monoxide (CO) over 5 years, from 2005 to 2009, and at 47 pressure levels from 1000 hPa to 10 hPa. We believe that the study is the first of its kind to address the use of space-borne data for CO distribution over southern Africa. Maximum CO was recorded during spring and minimum during summer. Positive anomalies were identified in 2005 and 2007 during the spring and negative anomalies in the beginning of the year (especially in 2006, 2008 and 2009). The estimated trends based on a linear regression method on inter-annual distribution predicted a decreasing rate of 2.1% per year over South Africa, 1.8% per year over Madagascar and 1.7% per year over Reunion Island. The surface CO measurements made at Cape Point station (34.35°S, 18.48°E) showed an average decline of 0.1 ppb per month, which corresponded to 2.4% of the average annual mean for the studied period. The observed decrease in CO was linked to the La Niña event which occurred in 2006 and 2008 and a declining rate of biomass burning activity in the southern hemisphere over the observation period. TES measurements are in agreement with ground-based measurements and can be used with confidence to complement CO measurements for future analyses over the southern tropics and middle latitude.
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Article dans une revue
South African Journal of Science, AOSIS, 2015, 111 (9/10), 〈10.17159/ sajs.2015/20140174〉
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Mohamed Toihir Abdoulwahab, Sivakumar Venkataraman, Nkanyiso Mbatha, Sivakumar Sangeetha, Hassan Benchérif, et al.. Studies on CO variation and trends over South Africa and the Indian Ocean using TES satellite data. South African Journal of Science, AOSIS, 2015, 111 (9/10), 〈10.17159/ sajs.2015/20140174〉. 〈hal-01389450〉



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