Storm Event

Severity ? 2

Source

On the 24th of October, a small low-pressure over the Bay of Biscay produced strong north-easterly winds over the south coast of the UK (Boza, 2018). No particular high sea level was recorded, which includes the possibility of waves.

Pathway

No known sources of information.

Receptor and Consequence

In Hythe properties were flooded one foot deep and in Wallington Shore, houses had several inches of water (Ruocco et al., 2011).

Summary Table

Loss of life *
Residential property In Hythe properties were flooded one foot deep and in Wallington Shore, houses had several inches of water
Evacuation & Rescue *
   
Cost *
Ports *
Transport *
Energy *
Public services *
Water & wastewater *
Livestock *
Agricultural land *
   
Coastal erosion *
Natural environment *
Cultural heritage *
Coastal defences *

*No known sources of information available

References

  1. Boza, X. (2018). The Reconstruction and Analysis of Historical Coastal Flood Events from 1800’s in the Solent. UK. Southampton MSc Dissertation.
  2. Ruocco, A. Nicholls, R. J., Haigh, I. D., and Wadey, M. (2011). ‘Reconstructing Coastal Flood Occurrence Combining Sea Level and Media Sources: A case study of the Solent UK since 1935’. Natural Hazards, 59(3): 1773-1796. Available at: http://link.springer.com/10.1007/s11069-011-9868-7 (Accessed: 27 March 2015).