Articles | Volume 17, issue 6
https://doi.org/10.5194/acp-17-3987-2017
https://doi.org/10.5194/acp-17-3987-2017
Research article
 | 
24 Mar 2017
Research article |  | 24 Mar 2017

Satellite retrievals of dust aerosol over the Red Sea and the Persian Gulf (2005–2015)

Jamie R. Banks, Helen E. Brindley, Georgiy Stenchikov, and Kerstin Schepanski

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Cited articles

Abdou, W. A., Diner, D. J., Martonchik, J. V., Bruegge, C. J., Kahn, R. A., Gaitley, B. J., and Crean, K. A.: Comparison of coincident Multiangle Imaging Spectroradiometer and Moderate Resolution Imaging Spectroradiometer aerosol optical depths over land and ocean scenes containing Aerosol Robotic Network sites, J. Geophys. Res., 110, D10S07, https://doi.org/10.1029/2004JD004693, 2005.
Abed, A. M., Al-Kuisi, M., and Khair, H. A.: Characterization of the Khamaseen (spring) dust in Jordan, Atmos. Environ., 43, 2868–2876, https://doi.org/10.1016/j.atmosenv.2009.03.015, 2009.
Alpert, P. and Ziv, B.: The Sharav Cyclone: Observations and some theoretical considerations, J. Geophys. Res.-Atmos., 94, 18495–18514, https://doi.org/10.1029/JD094iD15p18495, 1989.
Banks, J. R. and Brindley, H. E.: Evaluation of MSG-SEVIRI mineral dust retrieval products over North Africa and the Middle East, Remote Sens. Environ., 128, 58–73, https://doi.org/10.1016/j.rse.2012.07.017, 2013.
Banks, J. R., Brindley, H. E., Flamant, C., Garay, M. J., Hsu, N. C., Kalashnikova, O. V., Klüser, L., and Sayer, A. M.: Intercomparison of satellite dust retrieval products over the west African Sahara during the Fennec campaign in June 2011, Remote Sens. Environ., 136, 99–116, https://doi.org/10.1016/j.rse.2013.05.003, 2013.
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Short summary
From an 11-year analysis of satellite measurements of atmospheric dust presence over the Red Sea, it is clear that there is a strong north–south gradient in dust activity and a pronounced interannual variability in this activity. Analysing two commonly used satellite retrieval methods to quantify dust presence, we find that under the most extreme dust storm conditions the measured dust optical thicknesses can diverge strongly between the two methods.
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