6533b7d2fe1ef96bd125e075

RESEARCH PRODUCT

Dust mobilization and transport in the northern Sahara during SAMUM 2006 – a meteorological overview

Peter KnippertzKerstin SchepanskiEike BierwirthThomas MüllerDietrich AlthausenAndreas PetzoldWolfgang Von Hoyningen-hueneKonrad KandlerDetlef MüllerTilman DinterLothar SchützAlbert AnsmannManfred WendischMatthias TescheIna TegenBernd Heinold

subject

LidarAtmospheric ScienceSaharan dustMeteorology010504 meteorology & atmospheric sciencesAtmosphärische Spurenstoffe010501 environmental sciencesMineral dustConvective Boundary Layer01 natural scienceslaw.invention010305 fluids & plasmasSAMUMHabooblaw13. Climate actionClimatologySynoptic scale meteorology0103 physical sciencesRadiosondeThunderstormEnvironmental scienceAeolian processesAir mass0105 earth and related environmental sciences

description

The SAMUM field campaign in southern Morocco in May/June 2006 provides valuable data to study the emission, and the horizontal and vertical transports of mineral dust in the Northern Sahara. Radiosonde and lidar observations show differential advection of air masses with different characteristics during stable nighttime conditions and up to 5-km deep vertical mixing in the strongly convective boundary layer during the day. Lagrangian and synoptic analyses of selected dust periods point to a topographic channel from western Tunisia to central Algeria as a dust source region. Significant emission events are related to cold surges from the Mediterranean in association with eastward passing upper-level waves and lee cyclogeneses south of the Atlas Mountains. Other relevant events are local emissions under a distinct cut-off low over northwestern Africa and gust fronts associated with dry thunderstorms over the Malian and Algerian Sahara. The latter are badly represented in analyses from the European Centre for Medium–Range Weather Forecasts and in a regional dust model, most likely due to problems with moist convective dynamics and a lack of observations in this region. This aspect needs further study. The meteorological source identification is consistent with estimates of optical and mineralogical properties of dust samples.DOI: 10.1111/j.1600-0889.2008.00380.x

https://doi.org/10.3402/tellusb.v61i1.16794