6533b820fe1ef96bd1279c93

RESEARCH PRODUCT

EARLINET observations of the 14-22-may long-range dust transport event during SAMUM 2006: validation of results from dust transport modelling

Rodanthi-elisavet MamouriEvangelos GerasopoulosMatthias TescheDietrich AlthausenPeter KnippertzElina GiannakakiA. TafuroDetlef MüllerGiuseppe D'amicoIna TegenA. PapayannisV. AmiridisL. Alados ArboledasJuan Luis Guerrero-rascadoG. PisaniDimitris BalisAdolfo ComerónBernd HeinoldMatthias WiegnerR. M PerroneGelsomina PappalardoLucia MonaMarco IarloriBirgit HeeseAldo AmodeoVolker FreudenthalerMichaël SicardAlbert AnsmannNicola SpinelliVincenzo Rizi

subject

Atmospheric ScienceEnvironmental EngineeringAerosol Robotic Network (AERONET)010504 meteorology & atmospheric sciencesMeteorologySaharan dustAEROSOL OPTICAL-PROPERTIES010501 environmental sciencesMineral dust01 natural sciencesMineral dustSun photometerLIDARSouth EuropeSKY RADIANCE MEASUREMENTSNETWORKAerosolOptical depth0105 earth and related environmental sciencesOptical propertiesEuropean Aerosol Research Lidar Network (EARLINET)Geometrical propertiesAtmosphärische SpurenstoffeDustNorth AfricaAerosolAERONETPlumeSAMUMLidarEnvironmental scienceAeolian processesEngineering and TechnologyDust aerosolsSaharan Mineral Dust Experiment (SAMUM)Sun photometersAERONET

description

We observed a long-range transport event of mineral dust from North Africa to South Europe during the Saharan Mineral Dust Experiment (SAMUM) 2006. Geometrical and optical properties of that dust plume were determined with Sun photometer of the Aerosol Robotic Network (AERONET) and Raman lidar near the North African source region, and with Sun photometers of AERONET and lidars of the European Aerosol Research Lidar Network (EARLINET) in the far field in Europe. Extinction-to-backscatter ratios of the dust plume over Morocco and Southern Europe do not differ. Ångstr¨om exponents increase with distance from Morocco. We simulated the transport, and geometrical and optical properties of the dust plume with a dust transport model. The model results and the experimental data show similar times regarding the appearance of the dust plume over each EARLINET site. Dust optical depth from the model agrees in most cases to particle optical depth measured with the Sun photometers. The vertical distribution of the mineral dust could be satisfactorily reproduced, if we use as benchmark the extinction profiles measured with lidar. In some cases we find differences. We assume that insufficient vertical resolution of the dust plume in the model calculations is one reason for these deviations.

10.1111/j.1600-0889.2008.00400.xhttp://hdl.handle.net/10481/33159