Hello, I had a couple of questions about URMA winds over the Great
Lakes. I am basing some of these questions off the kml files of the
sites used in RTMA/URMA for 20250828 at 0600Z.
1) Even after the GLERL "synthetic" obs were removed in
March 2025, we are still noticing suspiciously low sustained wind
values in the same location as before east of the Keweenaw Peninsula
in Lake Superior in the NBM. The gusts do not look as bad. We are
wondering if this is due to one of the synthetic obs still being in
the URMA analysis: https://docs.google.com/presentation/d/1DSudKLNwZF676A6QBj-BTVlHFaKdgyPanK9Hykjjj9U/edit?slide=id.p#slide=id.p
2) If I understand correctly, wind observations at varying heights
are supposed to be normalized to 10m. However, when I look at the obs
in Google Earth for a site that has its anemometer at 46.9 m AGL
(ROAM4), it looks like its sensor height is noted at 10m for the
sustained file. Some other sites that show the same behavior: PILM4
(15.5m), DISW3 (25.3m), and STDM4 (35.1m). When I look at the gust
file, it looks like the station height is listed as 20m. I may be
missing something here.
3) Why are the NDBC buoys not used in the analysis (e.g., 45006)?
4) We have a pretty reliable site just offshore in Lake Superior
(GISM4), can the winds and gusts be turned on at this site?
Thank you for your time.
Dan Thompson