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Last Thursday
through Sunday, a cyclonic circulation off the
coast of Californiatransported a deep plume of warm, moist air over Colorado.
The plume had moisture characteristics of a spring-time airmass, with
vertically
integrated water vapor values exceeding twice their winter-time
climatological levels.
Despite weak
dynamical forcing and only
modest orographic forcing, efficient high-density snowfall processes
were
sustained by the warm, moist, and thermodynamically unstable airmass.
The Park Range,
west of RMNP, was the big precipitation winner with 4-6 inches of new
snow
water equivalence (SWE) in four days, while the mountains of RMNP
received
around 2 inches of SWE during the same period.
Winds during the storm were from the south through
west, and produced
drifting on north- through east-facing aspects.
Deep, stable northwesterly flow
developed once again
on Tuesday through Thursday, which induced mountain-wave accelerations
east of
the Divide. As a
result, strong
down-sloping westerly winds have been continuously cranking over the
Park.
Alpine terrain with western
exposure was once
again scoured, and significant transport produced healthy snow drifts
in the
sub-alpine regions (see Eli’s conditions report).
A cold disturbance in the
northwesterly flow
produced additional low-density snows on Wednesday and Thursday,
supplying more
available mass for the drifting machine.
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