Understanding the long-term variability of African dust transport across the Atlantic as recorded in both Barbados surface concentrations and large-scale TOMS optical thickness

HR: 0800h
AN: A11C-0061 [Abstracts]
TI: Understanding the long-term variability of African dust transport across the Atlantic as recorded in both Barbados surface concentrations and large-scale TOMS optical thickness
AU: Chiapello, I
EM: chiapello@loa.univ-lille1.fr
AF: LOA, CNRS-USTL,, USTL, Bat. P5,, Villeneuve d'Ascq, 59655 France
AU: * Moulin, C
EM: cyril.moulin@cea.fr
AF: IPSL/LSCE, CEA-CNRS,, CEA Saclay, Bat. 701,, Gif-sur-Yvette, 91191 France
AU: Prospero, J M
EM: jprospero@rsmas.miami.edu
AF: RSMAS, Univ. of Miami,, 4600 Rickenbacker Causeway, Miami, FL 33149 United States
AB: Mineral dust is by far the most variable aerosol in the troposphere because its generation processes are highly sensitive to climate through both wind speed and rainfall. Assessing the radiative impact of mineral dust in numerical models is thus unrealistic as long as the causes of this variability are not fully understand and accounted for. The inter-annual variability of African dust transport over the north tropical Atlantic is monitored using in-situ surface concentrations measurements performed at Barbados since 1966, along with the TOMS and METEOSAT dust optical thickness (DOT) records covering the last two decades. Despite their differences in spatial coverage, the two dust records are in good agreement at both monthly and annual time scales over the 22 years of common operation. This demonstrates that the Barbados dust record is representative of the year-to-year variability of dust export over the north tropical Atlantic during both winter and summer. The satellite DOT are then used to assess the characteristics of the impact of climate factors, i.e., North Atlantic Oscillation (NAO) and Sahel drought, on dust emission and export as a function of season, and in terms of spatial extend of their influence. The analysis shows a large regional impact of Sahel drought on dust emissions and transport both in winter and in summer, whereas the influence of the NAO dominates the winter export and is more geographically limited to the eastern Atlantic north of 15鑞, and possibly some localized source-regions (south Mauritania and Bodele depression). Overall the combination of the 35 years of Barbados measurements of African dust with 22 years of satellite dust survey over the Atlantic highlights the very high dust loads in the mid 1980s related to the severe Sahel drought (maximum impact in 1983), and the persistently high dusty conditions in the 1990s, most probably due to the continuation of relatively dry conditions in Sahel in the recent years.
DE: 0305 Aerosols and particles (0345, 4801)
DE: 0340 Middle atmosphere--composition and chemistry
SC: Atmospheric Sciences [A]
MN: 2004 AGU Fall Meeting