Abstract

Abstract. The last decade has witnessed severe flooding across much of the globe, but have these floods really been exceptional? Globally, relatively few instrumental river flow series extend beyond 50 years, with short records presenting significant challenges in determining flood risk from high-magnitude floods. A perceived increase in extreme floods in recent years has decreased public confidence in conventional flood risk estimates; the results affect society (insurance costs), individuals (personal vulnerability) and companies (e.g. water resource managers). Here, we show how historical records from Britain have improved understanding of high-magnitude floods, by examining past spatial and temporal variability. The findings identify that whilst recent floods are notable, several comparable periods of increased flooding are identifiable historically, with periods of greater frequency (flood-rich periods). Statistically significant relationships between the British flood index, the Atlantic Meridional Oscillation and the North Atlantic Oscillation Index are identified. The use of historical records identifies that the largest floods often transcend single catchments affecting regions and that the current flood-rich period is not unprecedented.

Highlights

  • One of the greatest challenges presently facing river basin managers is the dearth of reliable long-term data on the frequency and severity of extreme floods, with an average gauged record length of ∼ 40 years in the UK (Marsh and Lees, 2003)

  • The apparent increase in flooding witnessed over the last decade appears in consideration to the long-term flood record not to be unprecedented; whilst the period since 2000 has been considered as flood-rich, the period 1970–2000 is “flood poor”, which may partly explain why recent floods are often perceived as extreme events

  • The principal findings of this work are that of the strong correlations between flood-rich/flood-poor phases and solar magnetic activity, Atlantic Meridional Oscillation (AMO) and North Atlantic Oscillation Index (NAOI), indicating a clear driver for flooding patterns across Britain

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Summary

Introduction

One of the greatest challenges presently facing river basin managers is the dearth of reliable long-term data on the frequency and severity of extreme floods, with an average gauged record length of ∼ 40 years in the UK (Marsh and Lees, 2003). Historical accounts represent a precious resource when considering the frequency and risks associated with high-magnitude low-frequency floods (Williams and Archer, 2002). Historical flood records are found in a variety of forms, directly or indirectly chronicling historic floods (Brázdil et al, 2005); sources include documentary

Series construction
Catchment characteristics
River Tweed
River Tyne
River Eden
River Dee
River Severn
3.10 River Thames
3.12 River Exe
Series composition
Spatial and temporal flood variability
Flood drivers
Findings
Summary
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