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The February 13, 1979, windstorm was a natural phenomenon that took place in Pacific Canada and the United States. During the early morning, 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 particularly intense pressure gradient across the Kitsap Peninsula region.

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  • The February 13, 1979, windstorm was a natural phenomenon that took place in Pacific Canada and the United States. During the early morning, 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 particularly intense pressure gradient across the Kitsap Peninsula region. (en)
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  • 5501 (xsd:integer)
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  • Priscilla Long (en)
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  • 2003-08-05 (xsd:date)
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  • 0001-02-13 (xsd:gMonthDay)
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  • The February 13, 1979, windstorm was a natural phenomenon that took place in Pacific Canada and the United States. During the early morning, 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 particularly intense pressure gradient across the Kitsap Peninsula region. (en)
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  • February 13, 1979 windstorm (en)
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