The low-level jet dust emission mechanism in the central Sahara: Observations from Bordj-Badji Mokhtar during the June 2011 Fennec Intensive Observation Period, Journal of Geophysical Research: Atmospheres, vol.17, issue.3, pp.2990-301510, 2011. ,
DOI : 10.1029/2006GL025827
Dust emission and transport mechanisms in the central Sahara: Fennec ground-based observations from Bordj Badji Mokhtar, June 2011, Journal of Geophysical Research: Atmospheres, vol.91, issue.2-4, pp.6212-6232, 2011. ,
DOI : 10.1029/2005JD006502
Saharan Mineral Dust Experiments SAMUM???1 and SAMUM???2: what have we learned?, Tellus B: Chemical and Physical Meteorology, vol.26, issue.54, pp.403-429, 2011. ,
DOI : 10.1029/2004JDO05276
The Role of the Sahara Low in Summertime Sahel Rainfall Variability and Change in the CMIP3 Models, Journal of Climate, vol.22, issue.21, pp.5755-577110, 2001. ,
DOI : 10.1175/2009JCLI2969.1
Synoptic-scale dust emissions over the Sahara Desert initiated by a moist convective cold pool in early August 2006, Quarterly Journal of the Royal Meteorological Society, vol.108, issue.685, pp.2591-2607, 2006. ,
DOI : 10.1002/qj.2326
URL : https://hal.archives-ouvertes.fr/hal-00932338
Intraseasonal Variability of the Saharan Heat Low and Its Link with Midlatitudes, Journal of Climate, vol.23, issue.10, pp.2544-2561, 2010. ,
DOI : 10.1175/2010JCLI3093.1
Multiplatform observations of the seasonal evolution of the Saharan atmospheric boundary layer in Tamanrasset, Algeria, in the framework of the African Monsoon Multidisciplinary Analysis field campaign conducted in, J. Geophys. Res, vol.113, pp.0-0710, 2006. ,
URL : https://hal.archives-ouvertes.fr/hal-00311302
Northward bursts of the West African monsoon leading to rainfall over the Hoggar Massif, Algeria, Quarterly Journal of the Royal Meteorological Society, vol.34, issue.s1, pp.174-189, 2010. ,
DOI : 10.1002/qj.439
URL : https://hal.archives-ouvertes.fr/hal-00401335
The Unified Forecast Climate Model, Meteorol. Mag, vol.122, pp.81-94, 1449. ,
Diurnal and Semidiurnal Tides in Global Surface Pressure Fields, Journal of the Atmospheric Sciences, vol.56, issue.22, pp.3874-3891, 1999. ,
DOI : 10.1175/1520-0469(1999)056<3874:DASTIG>2.0.CO;2
The ERA-Interim reanalysis: configuration and performance of the data assimilation system, Quarterly Journal of the Royal Meteorological Society, vol.91, issue.656, pp.553-597, 2011. ,
DOI : 10.1002/qj.828
North African dust emissions and transport, Earth-Science Reviews, vol.79, issue.1-2, pp.73-100, 2006. ,
DOI : 10.1016/j.earscirev.2006.06.004
Influence of African dust on ocean???atmosphere variability in the tropical Atlantic, Nature Geoscience, vol.4, issue.11, pp.762-76510, 2011. ,
DOI : 10.1029/2007GC001774
Water Vapor???Forced Greenhouse Warming over the Sahara Desert and the Recent Recovery from the Sahelian Drought, Journal of Climate, vol.28, issue.1, pp.108-123, 2015. ,
DOI : 10.1175/JCLI-D-14-00039.1
URL : https://hal.archives-ouvertes.fr/hal-01112972
The impact of a mesoscale convective system cold pool on the northward propagation of the intertropical discontinuity over West Africa, Quarterly Journal of the Royal Meteorological Society, vol.131, issue.638, pp.139-159, 2009. ,
DOI : 10.1002/qj.357
URL : https://hal.archives-ouvertes.fr/hal-00358608
The evolution of the Saharan Boundary layer thermodynamics and composition in connection with intra-seasonal pulsations of the West African Heat Low, 4th AMMA Conference, pp.2-6, 2012. ,
URL : https://hal.archives-ouvertes.fr/hal-00723562
Thickness of the dry convection and large-scale subsidence above deserts, Boundary-Layer Meteorology, vol.40, issue.3, pp.265-27810, 1996. ,
DOI : 10.1007/BF00119441
The impact of convective cold pool outflows on model biases in the Sahara, Geophysical Research Letters, vol.4, issue.10, pp.1647-1652, 2013. ,
DOI : 10.1002/qj.991
The Turbulent Structure and Diurnal Growth of the Saharan Atmospheric Boundary Layer, Journal of the Atmospheric Sciences, vol.72, issue.2, 2014. ,
DOI : 10.1175/JAS-D-13-0384.1
The Atlantic inflow to the Saharan heat low: observations and modelling, Quarterly Journal of the Royal Meteorological Society, vol.131, issue.s1, pp.125-140, 2010. ,
DOI : 10.1002/qj.429
Motivation, rationale and key results from the GERBILS Saharan dust measurement campaign, Quarterly Journal of the Royal Meteorological Society, vol.23, issue.658, pp.1106-1116, 2011. ,
DOI : 10.1002/qj.797
The Fennec Automatic Weather Station (AWS) Network: Monitoring the Saharan Climate System, Journal of Atmospheric and Oceanic Technology, vol.30, issue.4, pp.709-724, 2012. ,
DOI : 10.1175/JTECH-D-12-00037.1
Annual variations of physical properties of desert dust over Israel, Journal of Geophysical Research: Atmospheres, vol.107, issue.D23, pp.438110-1029, 2003. ,
DOI : 10.1029/2002JD003163
Measurements of aerosol properties from aircraft, satellite and ground-based remote sensing: a case-study from the Dust and Biomass-burning Experiment (DABEX), Quarterly Journal of the Royal Meteorological Society, vol.113, issue.641, pp.922-934, 2009. ,
DOI : 10.1002/qj.420
Tropical???extratropical interactions related to upper-level troughs at low latitudes, Dynamics of Atmospheres and Oceans, vol.43, issue.1-2, pp.36-62, 2007. ,
DOI : 10.1016/j.dynatmoce.2006.06.003
URL : http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.465.498
Progress in understanding of weather systems in West Africa, Atmospheric Science Letters, vol.114, issue.15, pp.7-12, 2011. ,
DOI : 10.1002/asl.335
URL : https://hal.archives-ouvertes.fr/hal-00569956
Seasonal evolution of the West African heat low: a climatological perspective, Climate Dynamics, vol.11, issue.555, pp.313-33010, 2009. ,
DOI : 10.1007/s00382-009-0553-4
URL : https://hal.archives-ouvertes.fr/hal-00383908
Regional-scale convection patterns during strong and weak phases of the Saharan heat low, Atmospheric Science Letters, vol.79, issue.555, pp.255-264, 2010. ,
DOI : 10.1002/asl.284
URL : https://hal.archives-ouvertes.fr/hal-00554966
Links between African easterly waves, midlatitude circulation and intraseasonal pulsations of the West African heat low, Quarterly Journal of the Royal Meteorological Society, vol.132, issue.s1, pp.141-158, 2010. ,
DOI : 10.1002/qj.555
URL : https://hal.archives-ouvertes.fr/hal-00450863
Monitoring the West African heat low at seasonal and intra-seasonal timescales using AMSU-A sounder, Atmospheric Science Letters, vol.27, issue.20, pp.263-2710, 2013. ,
DOI : 10.1002/asl2.449
URL : https://hal.archives-ouvertes.fr/hal-00849824
The AMMA field campaigns: multiscale and multidisciplinary observations in the West African region, Quarterly Journal of the Royal Meteorological Society, vol.132, issue.s1, pp.8-33, 2010. ,
DOI : 10.1002/qj.486
URL : https://hal.archives-ouvertes.fr/hal-00605940
The importance of the representation of deep convection for modeled dust-generating winds over West Africa during summer, Geophysical Research Letters, vol.91, issue.D15, p.1680310, 1029. ,
DOI : 10.1029/2011GL048368
Meteorology and dust in the central Sahara: Observations from Fennec supersite-1 during the June 2011 Intensive Observation Period, Journal of Geophysical Research: Atmospheres, vol.93, issue.124, pp.4069-4089, 2011. ,
DOI : 10.1111/1467-8306.9302003
The Australian nocturnal jet and diurnal variations of boundary-layer winds over Mt. Isa in North-eastern Australia, Quarterly Journal of the Royal Meteorological Society, vol.32, issue.525, pp.987-1003, 1995. ,
DOI : 10.1002/qj.49712152503
Using aircraft measurements to determine the refractive index of Saharan dust during the DODO experiments, Atmos. Chem. Phys, vol.105194, issue.6, pp.3081-309810, 2010. ,
Moisture Variability and Multiscale Interactions during Spring in West Africa, Monthly Weather Review, vol.142, issue.9, pp.3178-3198, 2014. ,
DOI : 10.1175/MWR-D-13-00175.1
The diurnal cycle of the West African monsoon circulation, Quarterly Journal of the Royal Meteorological Society, vol.129, issue.611, pp.2839-2860, 2005. ,
DOI : 10.1256/qj.04.52
An Idealized Two-Dimensional Framework to Study the West African Monsoon. Part I: Validation and Key Controlling Factors, Journal of the Atmospheric Sciences, vol.64, issue.8, pp.2765-2782, 2007. ,
DOI : 10.1175/JAS3919.1
Environmental characterization of global sources of atmospheric soil dust identified with the NIMBUS 7 Total Ozone Mapping Spectrometer (TOMS) absorbing aerosol product, Reviews of Geophysics, vol.103, issue.2, p.100210, 1029. ,
DOI : 10.1029/2000RG000095
10???25-Day Intraseasonal Variability of Convection over the Sahel: A Role of the Saharan Heat Low and Midlatitudes, Journal of Climate, vol.24, issue.22, pp.5863-587810, 2001. ,
DOI : 10.1175/2011JCLI3960.1
Meteorological processes forcing Saharan dust emission inferred from MSG-SEVIRI observations of subdaily dust source activation and numerical models, Journal of Geophysical Research, vol.108, issue.D17, p.1020110, 1029. ,
DOI : 10.1029/2008JD010325
An introduction to Meteosat Second Generation (MSG), Bull. Am, 083<0977:AITMSG>2.3.CO, pp.977-99210, 2002. ,
Density currents as a desert dust mobilization mechanism, Atmos. Chem. Phys, vol.12211, issue.11, pp.199-210, 2012. ,
The West African Monsoon Dynamics. Part II: The ???Preonset??? and ???Onset??? of the Summer Monsoon, 016<3407:TWAMDP>2.0.CO, pp.3407-342710, 2003. ,
DOI : 10.1175/1520-0442(2003)016<3407:TWAMDP>2.0.CO;2
URL : https://hal.archives-ouvertes.fr/hal-00155510
Maintenance of the African easterly jet, Quarterly Journal of the Royal Meteorological Society, vol.30, issue.555, pp.763-786, 1999. ,
DOI : 10.1002/qj.49712555502
Meteorological and dust aerosol conditions over the western Saharan region observed at Fennec Supersite-2 during the intensive observation period in June 2011, Journal of Geophysical Research: Atmospheres, vol.111, issue.12, pp.8426-8447, 2011. ,
DOI : 10.1029/2005JD006502
URL : https://hal.archives-ouvertes.fr/hal-00829054
The Met Office Unified Model Global Atmosphere 3, Geosci. Model Dev, vol.1, issue.44, pp.919-94110, 2011. ,
Dust-Storm Source Areas Determined by the Total Ozone Monitoring Spectrometer and Surface Observations, Annals of the Association of American Geographers, vol.50, issue.2, pp.297-31310, 2003. ,
DOI : 10.1029/97JD02300