Articles | Volume 16, issue 11
https://doi.org/10.5194/acp-16-6977-2016
https://doi.org/10.5194/acp-16-6977-2016
Research article
 | 
07 Jun 2016
Research article |  | 07 Jun 2016

Fennec dust forecast intercomparison over the Sahara in June 2011

Jean-Pierre Chaboureau, Cyrille Flamant, Thibaut Dauhut, Cécile Kocha, Jean-Philippe Lafore, Chistophe Lavaysse, Fabien Marnas, Mohamed Mokhtari, Jacques Pelon, Irene Reinares Martínez, Kerstin Schepanski, and Pierre Tulet

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Cited articles

Allen, C. J. T., Washington, R., and Engelstaedter, S.: Dust emission and transport mechanisms in the central Sahara: Fennec ground-based observations from Bordj Badji Mokhtar, June 2011, J. Geophys. Res., 118, 6212–6232, https://doi.org/10.1002/jgrd.50534, 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 Sensing Env., 136, 99–116, https://doi.org/10.1016/j.rse.2013.05.003, 2013.
Bou Karam, D., Flamant, C., Knippertz, P., Reitebuch, O., Pelon, J., Chong, M., and Dabas, A.: Dust emissions over the Sahel associated with the West African monsoon intertropical discontinuity region: A representative case-study, Q. J. Roy. Meteor. Soc., 134, 621–634, https://doi.org/10.1002/qj.244, 2008.
Bou Karam, D., Flamant, C., Tulet, P., Chaboureau, J.-P., Dabas, A., and Todd, M. C.: Estimate of Sahelian dust emissions in the inter-tropical discontinuity region of the West African Monsoon, J. Geophys. Res., 114, D13106, https://doi.org/10.1029/2008JD011444, 2009.
Bou Karam, D., Flamant, C., Cuesta, J., Pelon, J., and Williams, E.: Dust emission and transport associated with a Saharan depression: February 2007 case, J. Geophys. Res., 115, D00H27, https://doi.org/10.1029/2009JD012390, 2010.
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Short summary
The Fennec field campaign conducted in June 2011 led to the first observational data set ever obtained that documents the Saharan atmospheric boundary layer under the influence of the heat low. In addition to the aircraft operation, four dust forecasts were run at low and high resolutions with convection-parameterizing and convection-permitting models, respectively. The unique airborne and ground-based data sets allowed the first ever intercomparison of dust forecasts over the western Sahara.
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