National Weather Service United States Department of Commerce
A Puget Sound Convergence Zone (PSCZ) forms when strong westerly winds flow around the Olympic Peninsula and converge over Puget Sound. It generally forms north of Seattle, and may move southward to as far as Boeing Field or SeaTac Airport. A PSCZ can cause a narrow band of convective precipitation along it, which can include rain showers, thunderstorms, or snowfall. Strong south to southwest winds are to the south of the PSCZ and north to northwest winds to the north.





 
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Wind Barbs, PIREPs, Radar, 10nm Range Rings, all sites except CWOP


676
FTUS46 KSEW 211124
TAFSEA
TAF
KSEA 211124Z 2112/2218 12006KT P6SM OVC080
FM211800 15005KT P6SM OVC050
FM212300 17007KT P6SM -RA OVC035
FM220200 16009KT 6SM -RA BR OVC024
FM220700 16008KT 6SM -RA BR OVC017=
 
 

674
FTUS46 KSEW 211124
TAFBFI
TAF
KBFI 211124Z 2112/2212 VRB03KT P6SM OVC090
FM211800 14005KT P6SM OVC050
FM212300 15006KT P6SM -RA OVC040
FM220200 15006KT 6SM -RA BR OVC027
FM220700 15008KT 6SM -RA BR OVC020=
 
 
   

615
FTUS46 KSEW 211124
TAFPAE
TAF
KPAE 211124Z 2112/2212 12004KT P6SM OVC070
FM212000 13007KT P6SM -RA OVC035
FM212200 13010KT 6SM -RA BR OVC025
FM220100 13010KT 6SM -RA BR OVC020
FM220600 16014G21KT 6SM -RA BR OVC022=