South Valley Surprise of 2002
| Type | Extratropical storm |
|---|---|
| Formed | February 7, 2002 |
| Dissipated | February 7, 2002 |
| Lowest pressure | 994 hPa |
| Maximum snowfall or ice accretion | 88 mph in Bandon, Oregon |
| Damage | $22.1 million (2002 USD) |
| Areas affected | British Columbia, Washington, Oregon, Northern California, Nevada, Idaho, and Western Montana |
The South Valley Surprise of 2002 was a Pacific Northwest windstorm that affected the U.S. states of Oregon, Washington, California, Nevada, and Idaho on February 7, 2002.
Overview
The storm underwent rapid cyclogenesis just before travelling inland. The circulation was so small in area that the isobars were compacted tightly, thanks to a strong ridge of high pressure to the south, resulting in sustained winds of 50 mph with gusts above 70 mph. The South Valley Surprise was second only to the Columbus Day Storm in terms of wind speed for the southern Willamette Valley.[1] The "surprise" was how rapidly the storm organized and matured, and its unanticipated strength. Thus, the public had no idea of the impending storm. The storm was able to tap into the jet stream and aim it towards the surface the phenomenon known as "Jet stream enhancement", which usually occurs in the unstable air found in a cold front in a mid latitude cyclone. The result was extensive damage to structures both directly and indirectly from falling trees and debris.[1]
See also
References
- 1 2 Wolf Read. "February 7, 2002 South Valley Surprise". Retrieved September 2012. Check date values in:
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