2018 Port Orchard tornado
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Kitsap County, Washington
- 120–130 miles per hour (190–210 km/h)[1]
| EF2 tornado | |
|---|---|
 EF2 damage to a dry storage facility in Port Orchard, Washington following the tornado. | |
| Formed | December 18, 2018, 1:50 p.m. PST (UTC−08:00) Kitsap County, Washington |
| Duration | 5 minutes |
| Dissipated | December 18, 2018, 1:55 p.m. |
| Highest winds |
|
| Max. rating1 | EF2 tornado |
| Fatalities | 0 fatalities, 0 injuries[2] |
| Damage | $1.81 million (2018 USD)[3] |
| Areas affected | Kitsap County, Washington |
| 1Most severe tornado damage; see Enhanced Fujita scale Part of the tornado outbreaks of 2018 | |
The 2018 Port Orchard tornado was a rare strong tornado that struck the city of Port Orchard, Washington on December 18, 2018.[4] The National Weather Service office in Seattle rated the tornado EF2 following an on-site survey of the storm damage the day after the event.[5] There were no fatalities or major injuries reported.[1][2] This was the first tornado to have touched down in Western Washington since an EF0 tornado in 2017 near Monroe.[6] Damage was most pronounced near the South Kitsap Regional Park.[4]
The tornado was the largest recorded in Kitsap County, and the 12th recorded F2/EF2 tornado to touch down in Washington since 1950. Washington state averages 2.5 tornadoes annually, but only 0.1 tornadoes in the month of December; the majority of these are rated EF0.[4][7]
The tornado was part of an atmospheric river event pointed straight at the Pacific Northwest causing $18 million (2018 USD) of damage between December 10 and December 25. This system caused flooding, severe erosion, and widespread power outages. Washington Governor Jay Inslee sought funding from the Federal Emergency Management Agency for damages caused during the prolonged stormy period, including for the Port Orchard tornado.[3]
There was not a tornado warning issued for the storm that produced the tornado.[8] The Storm Prediction Center placed the Kitsap Peninsula and nearby Olympic Peninsula under a risk for general thunderstorms for the day, but did not note a chance of severe thunderstorms for the region.[9]
The storm was a product of the Olympic Mountain velocity shear zone, a meteorological phenomenon that occurs when an incoming onshore flow in usually in the wake of a cold front from the Pacific Ocean is forced around the Olympic Mountains and adds the needed low-level wind shear that can enhance rotating storms moving through the area. Velocity scans show that this storm had mesoscale rotation to about 10,000 feet and rotation could be seen by the Langley Radar on Camano Island Doppler weather radar imagery.[8]