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. More model information for the winds around SeaTac can be found on the SeaTac Wind Page .





Hover over or click station to get METAR and TAF (if available)

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


718
FTUS46 KSEW 152332
TAFSEA
TAF
KSEA 152332Z 1600/1706 31012G20KT P6SM VCTS BKN035CB
PROB30 1600/1603 5SM -TSRA BKN040CB
FM160300 18005KT P6SM VCSH BKN027 OVC050
FM161000 19005KT P6SM BKN025 BKN050
FM161900 22006KT P6SM BKN050
FM162300 22008KT P6SM BKN100=
 
 

717
FTUS46 KSEW 152332
TAFBFI
TAF
KBFI 152332Z 1600/1624 35010G18KT P6SM VCTS BKN040CB
PROB30 1600/1603 5SM -TSRA BKN040CB
FM160300 18003KT P6SM VCSH BKN025 OVC050
FM161200 16005KT P6SM OVC025
FM161800 18005KT P6SM BKN050=
 
 
   

772
FTUS46 KSEW 152332
TAFPAE
TAF
KPAE 152332Z 1600/1624 34006KT P6SM VCTS BKN007 BKN040CB
PROB30 1600/1603 4SM -TSRA OVC040CB
FM160300 30005KT P6SM VCSH SCT025 BKN045
FM160800 20005KT P6SM OVC050
FM161100 19006KT P6SM BKN007 OVC015
FM161700 21005KT P6SM BKN025
FM162000 23007KT P6SM BKN050=