The Zone of Convergence of Puget Sound is a weather phenomenon in the area of Puget Sound in the American state of Washington. It is formed when enormous drafts separate on the level from the Olympic Mountains before converging on the level of Puget Sound. This convergence in general takes place in the north of Seattle and Everett and causes phenomena of ascents and Convection which forms a fine band of precipitations. Precipitations on the mount Glacier Peak located at the east of Puget Sound in the Chaîne of the Cascades rise thus between 3560 and 4570 mm of water.

External bonds

• What the zone of convergence of Puget Sound?
• Investigation on the zone of convergence of Puget Sound
• Snowfalls in the mountainous chain of the Cascades