The 11 August 2006 squall-line system as observed from MIT Doppler radar during the AMMA SOP

On the evening of 9 August 2006. a mesoscale convective system (MCS) having a north-south oriented squall-line organization formed over the border between Chad and Niegeria It propagated westward, in over Nigeria on 10 August. and reached Niamey (Niger) at 0320 UTC on 11 August Its passage over Niamey was accompanied by dust lifting and was well tracked by the Massachusetts Institute of Technology (MIT) Doppler radar The three-dimensional structure of the airflow and precipitation pattern is investigated from regular radar volume scans performed every ten minutes between 0200 and 0321 UTC The 3D wind components are deduced from the multiple-Doppler synthesis and continuity adjustment technique (MUSCAT) applied to a set of three volume scans obtained over a time period of one hour. which are equivalent to a three-radar observation of the squall line when considering a reference frame moving with the system and the hypothesis of a stationary held Results of the wind synthesis reveal several features commonly observed in tropical squall lines, such as the deep convective cells in front of the system. fed by the monsoon air and extending up to 15 km altitude, and the well-marked strati form ram region at the rear, associated with mesoscale vertical motions Forward and trailing an are clearly identified as resulting from the outflow of air reaching the tropopause and transported to this level by the sloping convective updraughts occuring in a sheared environment In the northern part. a deeper and stronger front-to-rear flow at mid-levels is found to contribute to the rearward deflection of the leading line and to promote a broader (over 300 km) stratiform cloud region Eddy vertical transports of the cross-line momentum mainly accounts for the mid-level flow acceleration clue to a momentum redistribution from low to higher levels The her distribution or hydrometeors and their associated production terms derived from a one-dimensional microphysical retrieval model indicate the distinct roles of the convective and stratiform regions in the formation of graupel and lam. and the respective contributions of cold (riming.) and warm (coalescence. inciting) processes Cooling from melting and heating/cooling, from condensation/evaporation processes yield a net decrease and increase of the potential temperature at low and mid-to-upper levels. respectively. with respect to an environmental thermodynamic profile taken three hours ahead of the analysis Finally. the upper-level rearward flow could convey the ion-negligible proportion of ice particles farther from the lead rig deep convection to the trailing: stratiform region. thereby favouring the extent of this region Copyright (C) 2009 Royal Meteorological Society