About: Puget Sound Convergence Zone

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The Puget Sound Convergence Zone (PSCZ) is a meteorological phenomenon that occurs over Puget Sound in the U.S. state of Washington. It is formed when the large-scale air flow splits around the Olympic Mountains and then converges over Puget Sound. This convergence zone generally occurs between north Seattle and Everett and can cause updrafts and convection, which leads to a narrow band of precipitation. The National Weather Service publishes special reports, forecasts, and graphical analyses for the PSCZ region.

Attributes	Values
rdf:type	disease
rdfs:label	Zone de Convergence de Puget Sound (fr) Puget Sound Convergence Zone (en)
rdfs:comment	La Zone de Convergence de Puget Sound est un effet local de la circulation atmosphérique dans la région de Puget Sound dans l'État américain de Washington. Il se forme lorsque le vent océanique se sépare en deux pour contourner les montagnes Olympiques avant de converger de l'autre côté dans le détroit. Cette convergence a lieu en général aux environs de la banlieue nord de Seattle à Everett et cause des phénomènes d'ascendance et de convection atmosphérique donnant de mince bandes de précipitations. La pluviométrie sur le pic Glacier, situé à l'est de Puget Sound dans la chaîne des Cascades, s'élève ainsi entre 3 560 et 4 570 mm d'eau. (fr) The Puget Sound Convergence Zone (PSCZ) is a meteorological phenomenon that occurs over Puget Sound in the U.S. state of Washington. It is formed when the large-scale air flow splits around the Olympic Mountains and then converges over Puget Sound. This convergence zone generally occurs between north Seattle and Everett and can cause updrafts and convection, which leads to a narrow band of precipitation. The National Weather Service publishes special reports, forecasts, and graphical analyses for the PSCZ region. (en)
dct:subject	Natural history of Washington (state) Mesoscale meteorology Atmospheric circulation
Wikipage page ID	5150399 (xsd:integer)
Wikipage revision ID	994665134 (xsd:integer)
Link from a Wikipage to another Wikipage	Cascade Range Puget Sound Roosevelt High School (Seattle) Enhanced Fujita scale Mountlake Terrace Bellingham, Washington United States dollar University District, Seattle University of Washington Updraft Victoria, British Columbia Convergence zone Glacier Peak Convection 2018 Port Orchard tornado Natural history of Washington (state) Lynnwood Shoreline, Washington Snohomish County, Washington Strait of Georgia Strait of Juan de Fuca Mesoscale meteorology Washington (U.S. state) Atmospheric circulation Edmonds, Washington Everett, Washington Northgate, Seattle Green Lake (Seattle) Atmospheric river King County, Washington Port Orchard, Washington Olympic Mountains Seattle San Juan Islands Rain shadow Meteorological Bothell Woodinville Precipitation (meteorology) Lake Forest Park U-District
sameAs	Puget Sound Convergence Zone Puget Sound Convergence Zone Puget Sound Convergence Zone Puget Sound Convergence Zone
dbp:wikiPageUsesTemplate	dbt:Convert dbt:Main dbt:Reflist
has abstract	The Puget Sound Convergence Zone (PSCZ) is a meteorological phenomenon that occurs over Puget Sound in the U.S. state of Washington. It is formed when the large-scale air flow splits around the Olympic Mountains and then converges over Puget Sound. This convergence zone generally occurs between north Seattle and Everett and can cause updrafts and convection, which leads to a narrow band of precipitation. A second, weaker convergence zone can occur between approximately Victoria, British Columbia, and Bellingham, Washington, over the San Juan Islands, as a result of southwesterly air blowing from the Strait of Juan de Fuca meeting northerly air moving southward down the Strait of Georgia. The National Weather Service publishes special reports, forecasts, and graphical analyses for the PSCZ region. (en) La Zone de Convergence de Puget Sound est un effet local de la circulation atmosphérique dans la région de Puget Sound dans l'État américain de Washington. Il se forme lorsque le vent océanique se sépare en deux pour contourner les montagnes Olympiques avant de converger de l'autre côté dans le détroit. Cette convergence a lieu en général aux environs de la banlieue nord de Seattle à Everett et cause des phénomènes d'ascendance et de convection atmosphérique donnant de mince bandes de précipitations. La pluviométrie sur le pic Glacier, situé à l'est de Puget Sound dans la chaîne des Cascades, s'élève ainsi entre 3 560 et 4 570 mm d'eau. (fr)
gold:hypernym	Phenomenon
prov:wasDerivedFrom	wikipedia-en:Puget_Sound_Convergence_Zone?oldid=994665134&ns=0
page length (characters) of wiki page	5958 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:Puget_Sound_Convergence_Zone
is Link from a Wikipage to another Wikipage of	Convergence zone Monroe, Washington Mukilteo, Washington Snohomish County, Washington Climate of Seattle Everett, Washington Chehalis Gap Kenmore, Washington Brown Willy effect PSCZ
is Wikipage redirect of	PSCZ
is foaf:primaryTopic of	wikipedia-en:Puget_Sound_Convergence_Zone

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