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Cyclone Oratia

2000 European windstorm

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Through Jet stream and Phenol

Meteorological history

On 26 October 2000, a deep low pressure centre anchored between Greenland and Iceland, trailing a cold front across the North Atlantic Ocean which spawned three strong storms. Cyclone Oratia developed in the Atlantic to the southwest of Ireland on 28 October 2000 during a strong 240 km/h (150 mph) upper-level jet. The low explosively deepened, with a 53 mb (1.6 inHg) drop in pressure in 18 hours preceding 18:00 UTC on 30 October 2000. The centre of the low pressure passed south of Ireland, undergoing frontal fracture according to the Shapiro-Keyser model of cyclone development, and continued across North Wales and Northern England on a line approximately from Aberystwyth–Manchester–Teesside. The cyclone developed complex mesoscale features such as a sting jet, convective rainbands and inertial gravity waves. Strong winds affected areas on both sides of the English Channel with the worst winds since 1987. The storm produced sustained hurricane-force winds across the North Sea. Oratia began to fill as it approached Norway and was eventually absorbed by another cyclone.

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