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T. C. Bond, D. G. Streets, K. F. Yarber, K. F. Nelson, S. M. J. H. Woo and Z. Klimont, “A Technology-Based Global Inventory of Black and Organic Carbon Emissions from Combustion,” Journal of Geophysical Research, Vol. 109, No. D14, 2004, p. D14203. doi:10.1029/2003JD003697

has been cited by the following article:

• TITLE: Intra-Seasonal Variability of Aerosols and Their Radiative Impacts on Sahel Climate during the Period 2000-2010 Using AERONET Data

  AUTHORS: Mamadou Simina Drame, Moctar Camara, Amadou T. Gaye

  KEYWORDS: AERONET; Aerosol Optical Depth; Radiative Forcing

  JOURNAL NAME: International Journal of Geosciences, Vol.4 No.1A, January 29, 2013

  ABSTRACT: This paper presents a study using in situ measurements (AERONET data) to characterize the intra-seasonal variability of aerosols and their shortwave radiative impacts on Sahel (11N - 18N and 20W - 15E) climate using a long time series (2000 to 2010) from AERONET data. We first used the MISR aerosol optical depth (AOD) averaged between 2000 and 2010 to identify dust maxima regions. They are mainly located over Eastern Mauritania-Northern Mali and Eastern Niger-Western Tchad (near the Bodele depression). Moreover the aerosol loading is stronger during the spring (MAM) and particularly during the summer (JJA). The analysis of AERONET data at 4 Sahelian stations (Dakar, Agoufou, Banizoumbou and Ouagadougou) shows that Sahel is under dust influence all year long. The dust season is mainly located between March and October, with two peaks of AOD recorded in March and June; while the maximum of biomass burning activity is recorded in winter (December to February). The radiative forcing of aerosols on the Sahelian climate results mainly in a cooling as well as at the surface than at the top of the atmosphere (TOA) but the forcing is stronger at the surface and particularly during the summer (JJA) and spring (MAM) periods. Although there is not a sharp difference between DJF and SON periods from a station to another one when considering the aerosol loading (AOD), the radiative forcing is stronger at the surface and weaker at the TOA during DJF for most stations. The analysis of the force effectiveness (ratio between AOD and the radiative forcing) suggests that the BOA radiative forcing is mainly influenced by the nature of aerosols.