Day 4-8 Outlook
Day 4-8 Convective Outlook
NWS Storm Prediction Center Norman OK
0402 AM CDT Sat Mar 29 2025
Valid 011200Z - 061200Z
...DISCUSSION...
Medium-range models appear to be in fairly good agreement through
much of the medium-range period, with respect to large-scale pattern
evolution/placement of the main synoptic-scale features. One
primary difference between the GFS and ECMWF at this time is that
the EC is more highly amplified with the upper pattern through the
period, and thus -- in general -- depicting stronger surface
features and greater flow aloft/wind shear.
One result of the higher amplitude of the ECMWF manifests Day
4/Tuesday April 1. As the eastern U.S. trough moves off the
Atlantic Coast, and the cold front stalls over the northern Gulf of
America early, northward return of this boundary as a warm front is
forecast over the southern and eventually the central Plains.
Central High Plains cyclogenesis is expected along this front as it
shifts northward. However, given the more amplified nature of
western troughing within the ECMWF, a much stronger surface cyclone
is progged by the EC as compared to the GFS (984 mb vs. 991 mb
respectively). The result is much stronger low-level theta-e
advection across the central/southern Plains depicted by the EC,
driving a much more rapid northward advance of the warm front. Both
models suggest after-dark convective development, but where the GFS
depicts weaker, elevated CAPE across Kansas, the EC's more robust,
potentially near surface-based CAPE suggests greater, more
widespread severe potential than the GFS. At this time, a small 15%
area will be introduced, centered over the mid Missouri Valley area,
mainly for the potential for hail with stronger storms. Later
refinements of the risk area will likely be required.
Day 5/Wednesday, a widespread, potentially substantial severe event
remains apparent, and with greater agreement within the models with
respect to the upper trough advance and associated positioning of
the surface low/cold front, greater confidence with respect to the
degree of risk exists. While a very similar 15% risk area will be
depicted as in yesterday's outlook, a 30% area is being introduced
from Arkansas northeastward to the mid Ohio Valley. It appears that
the environment will become conducive for supercells, with very
large hail, damaging winds, and strong tornadoes all possible during
the afternoon and evening hours.
From Day 6 onward, the cold front will continue its eastward advance
across the Ohio Valley and into/across the Northeast/New England.
However, much slower southward progression of the cold front is
expected, with an eventual drift northward as a warm front that then
lingers/oscillates across the Ohio Valley/Mid South/central and
southern Plains through the end of the period. This will occur as
a slow-moving trough moves into the West, and eventually evolves
into a cut-off low. While weak disturbances eject eastward through
southwesterly flow aloft across the central U.S. -- each of which
may bring rounds of convection/severe potential in the day 6-8 time
frame, narrowing down specific/greater areas of potential is
difficult at this time.
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