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    John Marsham
    School of Earth and Environment
    University of Leeds, United Kingdom

    The atmosphere of West Africa provides the setting for a unique
    variety of convective phenomena: the Sahara in the north has the
    deepest dry convective boundary layer in the world (reaching 6 km) and
    to the south in the Sahel mesoscale convective systems embedded in the
    West African monsoon provide the majority of the rainfall. The talk
    will describe work centered on the GERB Intercomparison of Longwave
    and Shortwave radiation (GERBILS) field campaign, which took place on
    the southern border of the Sahara during June 2007.

    Our current failure to represent the Saharan atmosphere accurately in
    weather and climate models has important implications. The Saharan
    Heat Low is a major control on regional dynamics,especially of the
    West African monsoon. Hurricane precursors are also generated by the
    African Easterly Jet. The Sahara is the world's largest source of
    desert dust, and dust loadings have been linked to hurricane activity.
    Dust is a key component of our climate, interacting with radiation
    (affecting regional dynamics), nucleating ice clouds and providing
    iron to the biosphere.

    In the Sahara, observations show the common persistence of a split
    boundary layer, with a residual layer above a convective boundary
    layer. Complex layerings of dust and moisture and are frequently
    observed in this residual layer. Dynamical mechanisms that allow
    exchange between the convective and residual layers, and the
    maintenance of the residual layers, will be discussed. Recent field
    campaigns have also highlighted the role of convection in the uplift
    of Saharan and Sahelian dust - through nocturnal low-level jets, the
    diurnal cycle of the monsoon flow, and outflows from deep convective
    storms. Results from GERBILS will be presented in the context of these
    recent studies, focusing on the potential role of convective outflows
    in the seasonal cycle of dust in the region.

    Friday, 9 January 2009, 9:30 AM
    Refreshments 9:15 AM
    NCAR-Foothills Laboratory
    3450 Mitchell Lane
    Bldg 2 Auditorium (Rm1022)

    For more information, contact Petter Weibring at ext. 2052, weibring@ucar.edu.

    Fri, Dec 26, 2008 to Fri, Jan 9, 2009