Mount Rainier and Camp Muir from the south. Photo: Wikipedia Commons |
The NAM analysis for 0000 UTC 13 Feb, just after the time of peak winds, shows a very strong 500 mb height gradient between a short-wave trough off the Pacific Northwest coast and the long-wave ridge that is parked over the interior western United States. At 700 mb, very near the altitude of Camp Muir, analyzed free-atmosphere winds near Mount Rainier are 70 knots (77 miles per hour). Jet level winds are around 125 knots (138 miles per hour).
Presumably flow-mountain interactions led to further acceleration of the flow near Camp Muir. This is a good example of why the climber's shelter there is built out of stone.
Camp Muir climber's shelter. Photo: Wikipedia Commons |
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