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During the storm, height of the water surface from the deepest point of each cross section ranged from 0.35 to 1.57 m and surface velocity ranged from 0.35 to 4.15 m/s.
However, more recently, Yoshida et al. (2009) have shown that the number of lightning flashes per second per convective cloud is approximately proportional to the fifth power of the cold-cloud depth (the height from the melting level to the storm height) and this relationship is not regional dependent.
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We characterise the spatial dependence of storm peak significant wave height using three models motivated by max-stable processes for locations in the northern North Sea.
For storm peak significant wave height events, the approach uses quantile regression to estimate a suitable extremal threshold, a Poisson process model for the rate of occurrence of threshold exceedances, and a generalised Pareto model for size of threshold exceedances.
We evaluate the new approach in application to marginal extreme value modelling of storm peak significant wave heights in two ocean basins, accommodating spatial and directional covariate effects.
Extreme hindcast storm peak significant wave heights (HS) for 816 locations throughout the North Sea are modelled, using the four parameter Poisson point process model of Wadsworth et al. (2010), incorporating measurement scale variability via a Box Cox transformation.
These measurements peaked in Cedar Key, where a station documented a storm surge height of 4.08 feet; the same station recorded a storm tide height of 6.26 feet.
At the storm's height, tornadoes popped up faster than they could be tallied.
At the storm's height, snow fell at a rate of 2 3 inches (50 75 mm) per hour in some areas.
Two fishing boats with 45 aboard were lost at sea after issuing distress calls at the storm's height, officials told La Prensa.
Wales battled winds of 89mph (143kph) at the storm's height on Saturday.
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