Journal metrics

Journal metrics

  • IF value: 2.281 IF 2.281
  • IF 5-year value: 2.693 IF 5-year 2.693
  • CiteScore value: 2.43 CiteScore 2.43
  • SNIP value: 1.193 SNIP 1.193
  • SJR value: 0.965 SJR 0.965
  • IPP value: 2.31 IPP 2.31
  • h5-index value: 40 h5-index 40
  • Scimago H index value: 73 Scimago H index 73
Nat. Hazards Earth Syst. Sci., 16, 1999-2007, 2016
https://doi.org/10.5194/nhess-16-1999-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
29 Aug 2016
The 21st century decline in damaging European windstorms
Laura C. Dawkins1, David B. Stephenson1, Julia F. Lockwood2, and Paul E. Maisey2 1College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, UK
2Met Office Hadley Centre, Exeter, UK
Abstract. A decline in damaging European windstorms has led to a reduction in insured losses in the 21st century. This decline is explored by identifying a damaging windstorm characteristic and investigating how and why this characteristic has changed in recent years. This novel exploration is based on 6103 high-resolution model-generated historical footprints (1979–2014), representing the whole European domain.

The footprint of a windstorm is defined as the maximum wind gust speed to occur at a set of spatial locations over the duration of the storm. The area of the footprint exceeding 20 ms−1 over land, A20, is shown to be a good predictor of windstorm damage. This damaging characteristic has decreased in the 21st century, due to a statistically significant decrease in the relative frequency of windstorms exceeding 20 ms−1 in north-western Europe, although an increase is observed in southern Europe. This is explained by a decrease in the quantiles of the footprint wind gust speed distribution above approximately 18 ms−1 at locations in this region. In addition, an increased variability in the number of windstorm events is observed in the 21st century.

Much of the change in A20 is explained by the North Atlantic Oscillation (NAO). The correlation between winter total A20 and winter-averaged mean sea-level pressure resembles the NAO pattern, shifted eastwards over Europe, and a strong positive relationship (correlation of 0.715) exists between winter total A20 and winter-averaged NAO. The shifted correlation pattern, however, suggests that other modes of variability may also play a role in the variation in windstorm losses.


Citation: Dawkins, L. C., Stephenson, D. B., Lockwood, J. F., and Maisey, P. E.: The 21st century decline in damaging European windstorms, Nat. Hazards Earth Syst. Sci., 16, 1999-2007, https://doi.org/10.5194/nhess-16-1999-2016, 2016.
Publications Copernicus
Download
Short summary
A decline in damaging European windstorms has led to a reduction in insured losses in the 21st century. This decline is explored through understanding how and why a damaging windstorm characteristic has changed in recent years. For individual windstorm events, the area of damaging winds is shown to have reduced due to a significant decrease in extreme winds in north-western Europe. This decline is largely related to changes in a large-scale atmospheric circulation pattern in the North Atlantic.
A decline in damaging European windstorms has led to a reduction in insured losses in the 21st...
Share