This paper examines flood frequencies in three coastal sectors of Britain and analyses the associated storm tracks and their principal pathways. The results indicate that the east coast of Britain has suffered most floods over the last 200 years. The frequencies of flood incidents in the south and southwest coast of Britain have increased, particularly during the 20th century, whereas on the west coast flood frequencies have declined. Three distinctive pathways of storm track are identified, related to flood incidents in each coastal sector. A southern pathway in a corridor along the 55° N parallel is associated with flood incidents recorded on the south and southwest coast, whilst storms that are associated with floods on the west coast concentrate along the 60° N parallel. The relationship between the frequencies of floods and climatic variations needs to be explored further. However, the development of coastal settlements has certainly increased vulnerability, and hence the risk of flood disasters.
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Allott & Lomax Consulting Engineers: 1979, Study of Morecambe Sea Defences, unpublished report to Lancaster City Council.
Briffa, K. R., Jones, P. D. and Kelly, P.M.: 1990, Principal component analysis of the Lamb catalogue of daily weather types: Part 2, seasonal frequencies and update to 1987, International Journal of Climatology 10, 549–563.
César, C.: 1991, Five hundred years of hurricanes in the Caribbean: Their relationship with global climatic variations, GeoJournal 23(4), 301–310.
Coker, A. M., Thompson, P. M., Smith, D. I. and Penning-Rowsell, E. C.: 1989, The impacts of climate change on coastal zone management in Britain: A preliminary analysis, The Publications of the Academy of Finland 9/89, Conference on Climate and Water 2, pp. 148–160.
Cracknell, E. B.: 1959, Canvey Island: The History of a Marshland Community, Department of English Local History Occasional Paper, No. 12, Leicester University Press.
Deser, C. and Blackmon, M. L.: 1993, Surface climate variations over the North Atlantic ocean during winter: 1900–1989, Journal of Climate 6, 1743–1753.
Emmanuel, K. A.: 1987, The dependence of hurricane intensity on climate, Nature 326, 483–485.
Fu, C., Diaz, H. F., Dong, D., and Fletcher, J. O.: 1999, Changes in atmospheric circulation over Northern Hemisphere oceans associated with the rapid warming of the 1920s, International Journal of Climatology 19, 581–606.
Golding, B.: 1981, The meteorological input to surge and wave prediction, in D. H. Peregrine (ed.), Floods Due to High Winds and Tides, Academic Press, London, pp. 1–8.
Hewitt, K. ed.: 1983, Interpretation of Calamity from Viewpoint of Human Ecology, Allen and Unwin, Boston.
Hickey, K. R.: 1998, Documentary Records of Coastal Storms in Scotland, unpublished PhD dissertation, Coventry University.
Hurrell, J. W.: 1995, Decadal trends in the North Atlantic Oscillation: Regional temperature and precipitation, Science 169, 676–679.
Hydraulics Research Station: 1976, Lune Foreshore, Morecambe Bay: Wave Statistics, unpublished report No. EX754.
Jones, M.: 1992, When the Sea Came by: The Story of a Flooded Coast, The Workers' Educational Association, North Wales, pp.102.
Jones, P. D. and Bradley, R. S.: 1992, Climatic variations over the last 500 years, in R. S. Bradley and P. D. Jones (eds.), Climate since A.D. 1500, Routledge, London, pp. 649–665.
Knox, J. L. and Hay, J. E.: 1985, Blocking signatures in the northern hemisphere: Frequency distribution and interpretation, International Journal of Climatology 5, 1–16.
Kushnir, Y.: 1994, Interdecadal variations in North Atlantic sea surface temperature and associated atmospheric conditions, Journal of Climate 7, 141–157.
Lamb, H. H.: 1985, The Little Ice Age period and the great storms within it, in M. J. Tooley and G. M. Sheail (eds), The Climatic Scene, George Allen and Unwin, London, pp. 104–131.
Lamb, H. H.: 1991, Historical Storms of the North Sea, British Isles and Northwest Europe, Cambridge University Press, Cambridge.
Parker, D. E., Horton, E. B. and Alexander, L. V.: 2000, Global and regional climate in 1999, Weather 55, 188–199.
Raper, S. C. B.: 1993, Observational data on the relationships between climatic change and the frequency and magnitude of severe tropical storms, in R. A. Warrick, E. M. Barrow and T. M. L. Wigley (eds) Climate and Sea-Level Change: Observations, Projections and Implications, Cambridge University Press, Cambridge, pp. 192–212.
Reading, A. J.: 1990, Caribbean tropical storm activity over the past four centuries, International Journal of Climatology 10, 365–376.
Rogers, J. C.: 1985. Atmospheric circulation changes associated with the warming over the northern North Atlantic in the 1920s, Journal of Climatology and Applied Meteorology 24, 1303–1310.
Spalding, J. V.: 1954, A general survey of the damage done and action taken, Conference on the North Sea Floods of 31 January–1 February 1953, The Institute of Civil Engineers, London, pp. 3–15.
Steers, J. A.: 1971, The East Coast floods: 31 January–1 February 1953, in J. A. Steers (ed.), Applied Coastal Geomorphology, Macmillan, London, pp. 198–223.
Subbaramayya, I. and Mohana Rao, S. R.: 1984, Frequency of Bay of Bengal cyclones in the postmonsoon season, Monthly Weather Review 112, 1640–1642.
Tooley, M. J.: 1992, Sea-level changes and the impacts on coastal lowlands, Journal of the Society of Fellows 7(1), 36–45.
Tooley, M. J., Zong, Y. and Innes, J. B.: 1997, Holocene storm surge signatures, in N. G. Jablonski (ed.), The Changing Face of East Asia During the Tertiary and Quaternary, Centre of Asian Studies, Hong Kong, pp. 138–149.
Townsend, J.: 1981, Storm surges and their forecasting. in D. H. Peregrine (ed.), Floods Due to High Winds and Tides, Academic Press, London, pp. 1–8.
Wendland, W. M.: 1977, Tropical storm frequencies related to sea surface temperatures, Journal of Applied Meteorology 16, 477–481.
White, G. F.: 1974, Natural Hazards: Local, National, Global, Oxford University Press, Oxford.
Wilby, R. L., O'Hare, G. and Barnsley, N.: 1997, The North Atlantic Oscillation and British Isles climate variability, 1865–1996, Weather 52, 266–276.
Zong, Y.: 1993, Flandrian Sea-Level Changes and Impacts of Projected Sea-level Rise on the Coastal Lowlands of Morecambe Bay and the Thames Estuary, U.K., unpublished PhD thesis, University of Durham, U.K.
Zong, Y. and Tooley, M. J.: 1995, The Incursion of Marine Sediment Inland During Severe Storms, Contract report to the National Radiological Protection Board, p. 175.
Zong, Y. and Tooley, M. J.: 1999, Evidence of mid-Holocene storm-surge deposits from Morecambe Bay, northwest England: A biostratigraphical approach, Quaternary International 55, 43–50.
Zong, Y., Tooley, M. J. and Donohgue, N. M. D.: 1995, Geographical information systems and sea flooding risk assessment in the Thames lowlands, Journal of the Society of Fellows 9(2), 3–18.
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Zong, Y., Tooley, M.J. A Historical Record of Coastal Floods in Britain: Frequencies and Associated Storm Tracks. Natural Hazards 29, 13–36 (2003). https://doi.org/10.1023/A:1022942801531
- coastal flood
- storm track
- historical records