Information about Extra-Tropical Storm Stephanie
2014-02-11 (IPMA)
During the evening february 8 and february 9, 2014, a low pressure system crossed the North Atlantic between the East Coast of the USA and the Azores Island, deepening 29 hPa in 24h (between 081200UTC and 091200UTC) and reached the West Cost of Iberian Península with 981 hPa, at 18UTC february 9. This Low was baptized as Stephanie by University of Berlin (Fig. 1).
This low caused heavy precipitation, special in west regions of mainland Portugal, and strong westerly wind during the afternoon and evening february 9, with very strong gusts, reaching 134 km/h in Cabo da Roca.
During the night February 9, the low move to Biscay Gulf, and the wind became northwest and gradually decreased its intensity, but with gusts up to about 80 to 90 km/h, until the evening morning, february 10.
Instituto Hidrográfico (IH) buoys, in Leixões and Sines, in the west portuguese coast, recordeds waves with 8 metres of significant wave high (SWH) 12.5 metres of maximum wave hight (Hmax) in Leixões and 17 metres in Sines, and 10 s of wave mean period (Fig. 2).
The numerical models and operational forecast from IPMA (Fig. 3) agreed with the observations the Instituto Hidrográfico (IH) buoys.
The 17metres Hmax value observed in Sines, can be defined as a “freak (or rogue) wave”, as these value is more than two times the SWH values being an extreme phenomenon, with a probability below 1%.
This situation is very similar to the one occurred in the January 6, associated to Christina Storm. However in that case, the waves were formed in Christina´s Atlantic path, producing waves with similar significant high to the Stephanie but with higher wavelength and periods, therefore more energetic.
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