Mesoscale convective systems (MCSs) are organized convective storm complexes, which extend over several 100°km and produce large areas of convective and stratiform precipitation (Houze, 2004). MCSs have more complex dynamics than unicellular convective storms, but are primarily defined by their spatial extent (Houze, 2004). Many different forces can drive mesoscale organisation of convection. Thus, the structure and precipitation characteristics of MCSs can take different forms depending on the region of genesis and underlying processes. In the continental mid-latitudes, MCSs often occur in areas downstream regions of high-altitude regions, as MCS formation is related to mountain flow dynamics. On the leeside of the Rocky Mountains (over the Great Plains)