An amazing mini cyclone hit western Washington late this afternoon.
Take a look at the visible satellite picture at 1 PM today (Sunday). You see the beautiful hooked shaped cloud just off the southern WA coast? That's it. Stunning.
The radar image at 1:28 PM from the Langley Hill radar was amazing...it looks like a tiny cyclone with a beautiful inner vortex, which is associated with a low pressure center. Precipitation intensity was enough with this vortex to drive the snow level to the surface along the coast.
As the low tracked northeast across Puget Sound the winds surged. As West Point (WPOW1) near Seattle the maximum gusts increased to 46 knots (53 mph).
While at the University of Washington wind gusted to 27 knots.
At 6 PM, a number of locations observed 30-40 mph gusts, and winds were strong enough at Seattle Tacoma Airport (40 mph gust) to result in 1-h delays for arriving planes.
The mini-vortex was embedded in an area of unstable, convective showers, which in turn were associated with a larger upper-level trough moving across our region.
Take a look at the visible satellite picture at 1 PM today (Sunday). You see the beautiful hooked shaped cloud just off the southern WA coast? That's it. Stunning.
The radar image at 1:28 PM from the Langley Hill radar was amazing...it looks like a tiny cyclone with a beautiful inner vortex, which is associated with a low pressure center. Precipitation intensity was enough with this vortex to drive the snow level to the surface along the coast.
As the low tracked northeast across Puget Sound the winds surged. As West Point (WPOW1) near Seattle the maximum gusts increased to 46 knots (53 mph).
While at the University of Washington wind gusted to 27 knots.
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