A combined observational and numerical modeling methodology was employed to
examine the interaction of large-scale quasi-stationary waves with regiona
l forcing in the drought of 1988 and flood of 1993 in the north-central Uni
ted States. The study implements and tests a new lateral boundary condition
closure approach enabling regional climate modeling sensitivity studies to
account for anomalies external to the simulated domain.
Thirty-day regional simulations of the continental United States using the
MM5 regional model successfully reproduced the anomalous drought and flood
conditions. In an additional set of simulations the observed large-scale qu
asi-stationary wave anomalies in the dynamic and thermodynamic fields were
filtered our through adjustment of the observationally based lateral bounda
ry conditions. In these filtered simulations the simulated meteorological f
ields over the drought/flood areas for both years tended toward those for n
ormal years, suggesting that the proposed filtering technique can be used a
s a tool to rest the regional response to external forcing. Comparisons of
the control and filtered simulations illustrated the significant influence
of large-scale anomalies on the strength and geographical distribution of t
he low-level jet and related impacts on rainfall in the central United Stat
es.