0000000000467663

AUTHOR

Cyrille Flamant

showing 7 related works from this author

Dust emissions over the Sahel associated with the West African monsoon intertropical discontinuity region: A representative case-study

2008

Near-dawn airborne lidar and dropsonde observations acquired on 7 July 2006, during the African Monsoon Multidisciplinary Analysis (AMMA) Special Observing Period 2a1, were used to investigate dust mobilization, lifting and transport in the intertropical discontinuity (ITD) region over western Niger. Atmospheric reflectivity data from the LEANDRE 2 lidar system enabled us to analyse the structure of dust plumes in the context of wind and thermodynamic information provided by the WIND lidar system and dropsondes. Dust mobilization was mainly observed in two locations: (a) within the monsoon flow as the result of the passage of a density current originating from a mesoscale convective system …

Earth's energy budgetAtmospheric ScienceMesoscale convective systemLidar010504 meteorology & atmospheric sciencesHarmattanWind LidarDust[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology010502 geochemistry & geophysicsMonsoon01 natural sciencesHaboobLidar13. Climate actionClimatologyPanacheEnvironmental scienceAMMADropsonde0105 earth and related environmental sciences
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A multi-instrument approach for characterizing the atmospheric aerosol optical thickness during the STAAARTE/DAISEX-99 campaign

2002

This work deals with the retrieval of the aerosol optical thickness (AOT) needed to carry out the atmospheric correction of remote sensing data measured in Barrax (Spain) on 4 June 1999 in the framework of 1999 Digital Airbone Imaging Spectrometer Experiment (DAISEX'99). The AOT was estimated through three approaches based on: spectral extinction of direct solar irradiance at ground level, airborne nephelometer measurements at different altitudes, and backscatter lidar in the lower troposphere. We found extremely low AOT values due to a cold Atlantic front that swept across the Iberian Peninsula from west to east producing light rain over the test area on 2 June 1999. The results were solar…

NephelometerBackscatterSingle-scattering albedoAtmospheric correctionImaging spectrometerGeofísicaSolar irradianceAtmospheric sciencesSpectrometerGeophysicsLidarExtinction (optical mineralogy)Aerosol optical thicknessGeneral Earth and Planetary SciencesEnvironmental scienceAtmospheric aerosolRemote sensing
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Initiation of deep convection at marginal instability in an ensemble of mesoscale models: a case-study from COPS

2011

The present study investigates the initiation of precipitating deep convection in an ensemble of convection-resolving mesoscale models. Results of eight different model runs from five non-hydrostatic models are compared for a case of the Convective and Orographically-induced Precipitation Study (COPS). An isolated convective cell initiated east of the Black Forest crest in southwest Germany, although convective available potential energy was only moderate and convective inhibition was high. Measurements revealed that, due to the absence of synoptic forcing, convection was initiated by local processes related to the orography. In particular, the lifting by low-level convergence in the planet…

Convection021110 strategic defence & security studiesAtmospheric ScienceConvective inhibition010504 meteorology & atmospheric sciencesMeteorologyPlanetary boundary layer0211 other engineering and technologiesMesoscale meteorologyOrography02 engineering and technologyForcing (mathematics)01 natural sciencesConvective available potential energyFree convective layerPhysics::Fluid Dynamics13. Climate actionClimatologyPhysics::Atmospheric and Oceanic PhysicsGeology0105 earth and related environmental sciencesQuarterly Journal of the Royal Meteorological Society
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The impact of a mesoscale convective system cold pool on the northward propagation of the intertropical discontinuity over West Africa

2009

The interaction between a mesoscale convection system cold pool and the intertropical discontinuity (ITD) is investigated on two consecutive days (5 and 6 June 2006), in the framework of the African Monsoon Multidisciplinary Analysis Special Observing Period (SOP 1a). Satellite imagery and surface meteorological observations are used to track the movement of the ITD prior to and after its interaction with the cold pool. The impact of the northward propagating cold pool on the Sahelo-Saharan planetary boundary layer (PBL) thermodynamics and aerosol vertical distribution is analyzed by means of airborne and ground-based measurements over the two-day period. Complementary European Centre for M…

Atmospheric Sciencedensity currents010504 meteorology & atmospheric sciencesPlanetary boundary layer0207 environmental engineeringMesoscale meteorology02 engineering and technology[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/MeteorologyMonsoon01 natural sciencesSEVIRI imageryECMWF analysesharmattanmonsoonSurge020701 environmental engineeringDropsondeComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]Mesoscale convective systemHarmattanFront (oceanography)airborne lidar13. Climate actionClimatologydropsondesEnvironmental scienceAMMAQuarterly Journal of the Royal Meteorological Society
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Advances in understanding mineral dust and boundary layer processes over the Sahara from Fennec aircraft observations

2015

Abstract. The Fennec climate programme aims to improve understanding of the Saharan climate system through a synergy of observations and modelling. We present a description of the Fennec airborne observations during 2011 and 2012 over the remote Sahara (Mauritania and Mali) and the advances in the understanding of mineral dust and boundary layer processes they have provided. Aircraft instrumentation aboard the UK FAAM BAe146 and French SAFIRE (Service des Avions Français Instrumentés pour la Recherche en Environnement) Falcon 20 is described, with specific focus on instrumentation specially developed for and relevant to Saharan meteorology and dust. Flight locations, aims and associated met…

Atmospheric Science010504 meteorology & atmospheric sciencesMeteorologyPlanetary boundary layerCONVECTIVE SYSTEMEnvironmental Sciences & EcologyAEROSOL OPTICAL-PROPERTIESMineral dust010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesCOARSE MODElcsh:ChemistryHaboobDust storm0201 Astronomical and Space SciencesMeteorology & Atmospheric SciencesSatellite imagerySOUTHERN MOROCCO0105 earth and related environmental sciences[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]GBScience & TechnologyHEAT LOWAIRBORNE OBSERVATIONSRETRIEVAL PRODUCTSOzone depletionlcsh:QC1-999PARTICLE-SIZEAERONETBoundary layerlcsh:QD1-99913. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyPhysical SciencesWEST-AFRICAN MONSOONEnvironmental science0401 Atmospheric SciencesNORTH-ATLANTIC OCEANLife Sciences & Biomedicinelcsh:PhysicsEnvironmental SciencesAtmospheric Chemistry and Physics
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Northward bursts of the West African monsoon leading to rainfall over the Hoggar Massif, Algeria

2009

The Hoggar Massif is a comparatively populated region in the Sahara, where water supply is a critical problem due to the lack of nearby sources and unaffordable water pumping. In the present paper, we analyse the influence of the West African monsoon (WAM) on precipitation over the Hoggar during summer. We investigate (1) two rainfall events during 23-27 July 2006, accounting for almost half of the precipitation of this year, and (2) the representativity of this period with regard to ERA-40 ECMWF re-analyses (1979 to 2001). By the end of July 2006, two consecutive northward bursts of the WAM flow reached the Hoggar and caused an increase in low-level humidity. In the afternoon of these days…

Atmospheric Sciencegeographygeography.geographical_feature_category010504 meteorology & atmospheric sciences0207 environmental engineeringTropical waveHumidity02 engineering and technologyMassifMonsoonThermal low01 natural sciencesConvective Boundary Layer13. Climate actionClimatologyPrecipitation020701 environmental engineeringSea levelGeology0105 earth and related environmental sciencesQuarterly Journal of the Royal Meteorological Society
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Sensitivity of low-level clouds and precipitation to anthropogenic aerosol emission in southern West Africa: a DACCIWA case study

2021

Abstract. During the West African summer monsoon, pollutants emitted in urbanized coastal areas modify cloud cover and precipitation patterns. The Dynamics-Aerosol-Chemistry-Cloud-Interactions in West Africa (DACCIWA) field campaign provided numerous aircraft-based and ground-based observations, which are used here to evaluate two experiments made with the coupled WRF-CHIMERE model, integrating both the direct and indirect aerosol effect on meteorology. During one well-documented week (1–7 July 2016), the impacts of anthropogenic aerosols on the diurnal cycle of low-level clouds and precipitation are analyzed in detail using high and moderate intensity of anthropogenic emissions in the expe…

PollutionAtmospheric Scienceaerosolmedia_common.quotation_subjectCloud covercloudsMonsoonAtmospheric sciencescomplex mixturesWest africaDiurnal cycleaerosol emissionddc:550DACCIWAPrecipitationlow-level cloudsmedia_commonPollutant[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]AerosolEarth sciences13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology[SDE]Environmental SciencesEnvironmental sciencesummer monsoonDynamics-Aerosol-Chemistry-Cloud Interactions in West Africaanthropogenic aerosol emission
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