Lb. Nance et Br. Colman, Evaluating the use of a nonlinear two-dimensional model in downslope windstorm forecasts, WEATHER FOR, 15(6), 2000, pp. 715-729
Severe downslope windstorms are a mesoscale, primarily wintertime, phenomen
on that affect regions in the lee of large mountain ranges. The resolution
of current weather prediction models is too coarse to explicitly predict do
wnslope windstorms. Hence, additional operational tools are needed for maki
ng downslope windstorm forecasts. Current windstorm forecast techniques com
monly utilize a tool referred to as a " decision tree. '' Although decision
trees provide valuable guidance, operational forecasters have not found th
is type of tool to be highly reliable. With recent advances in computer tec
hnology, a new type of operational tool is available for forecasting downsl
ope windstorms: two- dimensional, nonlinear, mesoscale numerical models. Th
is study investigates whether this type of model, initialized with upstream
profiles taken from operational Eta Model forecasts, can produce accurate
downslope windstorm forecasts.
Numerical simulations for high- wind events that affected seven regions in
the United States between January 1993 and April 1997 indicate this tool is
able to produce lee- slope wind speeds that meet the local peak gust thres
hold for a High Wind Warning for a majority of those cases where observed w
inds met this threshold. These simulations were initialized with upstream s
oundings taken from the 12- and 18- h Eta forecasts valid at the time of ea
ch high- wind event. A comparison for one region between the number of even
ts for which High Wind Watches were posted and the number of events for whi
ch the two- dimensional model prediction met the peak gust threshold sugges
ts this new tool would be a definite improvement over the current forecast
technique. On the other hand, a preliminary test of the model's ability to
differentiate between windstorm and nonwindstorm events suggests the false
warning rate for this tool may be high. Further testing of this tool is ong
oing and will continue through the winter months of 2000/ 01.