High-magnitude flooding across Britain since AD 1750

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 fl...

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Published in:Hydrology and Earth System Sciences
Main Authors: N. Macdonald, H. Sangster
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2017
Subjects:
T
G
Online Access:https://doi.org/10.5194/hess-21-1631-2017
https://doaj.org/article/2c6d716b42dc4f709d068babad44b66e
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spelling ftdoajarticles:oai:doaj.org/article:2c6d716b42dc4f709d068babad44b66e 2023-05-15T17:33:00+02:00 High-magnitude flooding across Britain since AD 1750 N. Macdonald H. Sangster 2017-03-01T00:00:00Z https://doi.org/10.5194/hess-21-1631-2017 https://doaj.org/article/2c6d716b42dc4f709d068babad44b66e EN eng Copernicus Publications http://www.hydrol-earth-syst-sci.net/21/1631/2017/hess-21-1631-2017.pdf https://doaj.org/toc/1027-5606 https://doaj.org/toc/1607-7938 1027-5606 1607-7938 doi:10.5194/hess-21-1631-2017 https://doaj.org/article/2c6d716b42dc4f709d068babad44b66e Hydrology and Earth System Sciences, Vol 21, Iss 3, Pp 1631-1650 (2017) Technology T Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 article 2017 ftdoajarticles https://doi.org/10.5194/hess-21-1631-2017 2022-12-31T05:48:17Z 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. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Directory of Open Access Journals: DOAJ Articles Hydrology and Earth System Sciences 21 3 1631 1650
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Technology
T
Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
spellingShingle Technology
T
Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
N. Macdonald
H. Sangster
High-magnitude flooding across Britain since AD 1750
topic_facet Technology
T
Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
description 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.
format Article in Journal/Newspaper
author N. Macdonald
H. Sangster
author_facet N. Macdonald
H. Sangster
author_sort N. Macdonald
title High-magnitude flooding across Britain since AD 1750
title_short High-magnitude flooding across Britain since AD 1750
title_full High-magnitude flooding across Britain since AD 1750
title_fullStr High-magnitude flooding across Britain since AD 1750
title_full_unstemmed High-magnitude flooding across Britain since AD 1750
title_sort high-magnitude flooding across britain since ad 1750
publisher Copernicus Publications
publishDate 2017
url https://doi.org/10.5194/hess-21-1631-2017
https://doaj.org/article/2c6d716b42dc4f709d068babad44b66e
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Hydrology and Earth System Sciences, Vol 21, Iss 3, Pp 1631-1650 (2017)
op_relation http://www.hydrol-earth-syst-sci.net/21/1631/2017/hess-21-1631-2017.pdf
https://doaj.org/toc/1027-5606
https://doaj.org/toc/1607-7938
1027-5606
1607-7938
doi:10.5194/hess-21-1631-2017
https://doaj.org/article/2c6d716b42dc4f709d068babad44b66e
op_doi https://doi.org/10.5194/hess-21-1631-2017
container_title Hydrology and Earth System Sciences
container_volume 21
container_issue 3
container_start_page 1631
op_container_end_page 1650
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