The 1 PM Sunday visible satellite imagery shows the incipient storm, nearly due west of the CA/OR border. Can you see the swirl of clouds around the low and the very unstable air (with popcorn-looking clouds) to the storm's west?
By 10 AM, Monday morning, the system has revved up as a double-barrel low, with an intense pressure gradient (change of pressure with distance) along the Washington Coast. That will bring very strong winds.
The low pressure sweeps northwestward, bringing a strong north-south pressure gradient over western Washington, which will experience strong winds.
How strong?
Here are the wind gusts forecast by the ultra-high resolution (1.3 km grid spacing) UW WRF system.
By 6 AM Monday morning, strong winds have reached the coast (50-60 knots) and over portions of NW Washington.
By 11 AM (19 UTC), crazy strong gusts (above 70 knots have reached the SW coast of Washington) as the low center approaches the NW tip of WA.
By 1 PM, the low center is over Tatoosh Island and winds over Puget Sound are revving, with gusts to 50 knots over south Seattle and more around the San Juans.
The action continues through 3 PM, with the winds starting to back off along the southern WA coast.
But what about other models and ensemble (many forecast) products? The NWS SREF ensemble system's forecast of sustained winds at Sea Tac shows that most runs indicate windy conditions, with an average sustained wind of about 20 knots, which would imply gusts to around 25-30 knots. There is considerable uncertainty, with some of the runs with much stronger winds.
The vaunted European Center model is taking the low farther offshore with the gusts over Puget Sound reaching 40-45 knots, with more over the coast and San Juans (see graphics of pressure and wind gusts below for 4 PM Monday).
from Cliff Mass Weather and Climate Blog http://ift.tt/2zRDUKi
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