Hello
Jeff. I obviously have a keen interest in this because of the
impact of the URMA on NBM. I took a look and this is not an easy
problem to fix.
The
valley is rather narrow, and there appear to be observations both in
the valley floor and also on the ridges either side of the valley.
So looking at 20F differences in MaxT as a result. Elevation
differences in this short distance for the observations range from
2,000 to 8,000 feet MSL.
I
drew a black line on the approximate location of the valley/Merced
River. MatchObsAll in this plot appears to be offset about one to
two grid points to the south of the actual location (not sure if
this is a real problem or just an issue with NBM Viewer).
I
looked at the current plot (around 1100 UTC) this morning and there
is a 50F spread in observations across a short distance. Omitting
the 13F observation from a HADS (hopefully this is blacklisted),
there still appears to be roughly a 25F difference in observations
close to the Merced River Valley in this area. The HADs (AHIC1)
appears to be accepted by the URMA analysis.
Here
is a recent example showing URMA, URMA First Guess, MatchObsAll, and
the difference between MOA and URMA.
The
URMA FG in this case for AHIC1 grid point was raised 4F to account
for that observation.
Here
is another day, where an observed 2,000 foot observation downstream
on Merced River was 101F, and the URMA analyzed about 98F. The
AHIC1 HADS site was 87F, after being raised 5F from the first Guess.
JPC