Tuesday, 16 January 2001
Most numerical studies of mesoscale structures
of midlatitude weather systems are conducted with
models in which the horizontal resolution is focused
over a limited region (using grid-nesting or variable
resolution). With such models, the predictability of
weather systems critically depends on the quality of
the lower-resolution solution outside the domain of
interest. Because of the always increasing computer
power, it is now possible to integrate a global
uniform-resolution model with a mesoscale resolution.
In this study, a 0.28 degree (~ 30 km at midlatitudes)
version of the Global Environmental Model (GEM) is used
to simulate two severe weather events: a synoptic-scale
winter storm that occurred in northeastern United States,
and a mesoscale convective system that propagated over
the central United States. The short-to-medium-range
predictability of these events is investigated by examining
forecasts up to five days before the events. This
predictability is also investigated in the context of
a variable-grid configuration which is currently used
operationally for regional forecasting at the Canadian
Meteorological Center.
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