During the early morning of February 13, 1979, an intense wave cyclone moved across southern Vancouver Island, British Columbia. South of the low center, a strong atmospheric pressure gradient was carried across Washington, with associated high winds. With a cold airflow moving toward the northeast interacting with the high terrain of the Olympic Mountains, a lee low developed east of the Olympics. The mesoscale low caused a particualrly intense pressure gradient to develop across the Kitsap Peninsula region. As reported by the crew of the Hood Canal Bridge, average winds exceeded 80 mph out of the south, with gusts into the triple digits. The pressure of wind and wave on the generally east-west oriented bridge stressed the structure enough to cause catastrophic failure. It is suspected that a severe list in the bridge exposed pontoon access hatches to the waves, which subsequently tore the covers loose and allowed water to enter the flotation devices, causing sections to sink. It took nearly three years and over $140 million U.S. to rebuild the lost bridge.
Most of these peak gusts are from official stations.
February13, 1979Windstorm Overview During the early morning of February13, 1979, an intense wave cyclone moved across southern Vancouver Island, British Columbia.
It was decided to use a large rubber dam between each of the two pontoons as they were attached, clean the concrete surfaces of all marine growth, epoxy, and tension them with a number of cables welded to a variety of attachment points.
Washington State Route 104 is a highway in the state of Washington, U.S.A. It extends from Discovery Bay in the northwest to Lake Forest Park in the southeast.
The Hood Canal Bridge suffered catastrophic failure during the February13, 1979Windstorm.
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