Puget Sound Convergence Zone Puget Sound Convergence Zone 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
Port Washington Narrows Port Washington Narrows The Port Washington Narrows is a tidal strait located in Bremerton, Washington, United States. The northwest entrance is marked on the west side by Rocky Point, and the southeast entrance is located at Point Turner on the west side and Point Herron on the east side. It is located between downtown Bremerton and the Manette Peninsula. It is through this channel that Dyes Inlet drains into Sinclair Inlet and into Puget Sound. Tidal currents attain velocities in excess of 4 knots at times. The Narrows divide the city of Bremerton into east and west portions, which are