Future changes in atmospheric rivers and their implications for winter flooding in Britain

[thumbnail of Article]
Preview
Text (Article) - Published Version
· Available under License Creative Commons Attribution.
· Please see our End User Agreement before downloading.
| Preview
Available under license: Creative Commons Attribution
[thumbnail of Lavers13ERLsup.pdf]
Preview
Text - Supplemental Material
· Please see our End User Agreement before downloading.
| Preview

Please see our End User Agreement.

It is advisable to refer to the publisher's version if you intend to cite from this work. See Guidance on citing.

Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

Lavers, D. A., Allan, R. P. orcid id iconORCID: https://orcid.org/0000-0003-0264-9447, Villarini, G., Lloyd-Hughes, B., Brayshaw, D. J. orcid id iconORCID: https://orcid.org/0000-0002-3927-4362 and Wade, A. J. orcid id iconORCID: https://orcid.org/0000-0002-5296-8350 (2013) Future changes in atmospheric rivers and their implications for winter flooding in Britain. Environmental Research Letters, 8 (3). 034010. ISSN 1748-9326 doi: 10.1088/1748-9326/8/3/034010

Abstract/Summary

Within the warm conveyor belt of extra-tropical cyclones, atmospheric rivers (ARs) are the key synoptic features which deliver the majority of poleward water vapour transport, and are associated with episodes of heavy and prolonged rainfall. ARs are responsible for many of the largest winter floods in the mid-latitudes resulting in major socioeconomic losses; for example, the loss from United Kingdom (UK) flooding in summer/winter 2012 is estimated to be about $1.6 billion in damages. Given the well-established link between ARs and peak river flows for the present day, assessing how ARs could respond under future climate projections is of importance in gauging future impacts from flooding. We show that North Atlantic ARs are projected to become stronger and more numerous in the future scenarios of multiple simulations from five state-of-the-art global climate models (GCMs) in the fifth Climate Model Intercomparison Project (CMIP5). The increased water vapour transport in projected ARs implies a greater risk of higher rainfall totals and therefore larger winter floods in Britain, with increased AR frequency leading to more flood episodes. In the high emissions scenario (RCP8.5) for 2074–2099 there is an approximate doubling of AR frequency in the five GCMs. Our results suggest that the projected change in ARs is predominantly a thermodynamic response to warming resulting from anthropogenic radiative forcing.

Altmetric Badge

Item Type Article
URI https://reading-clone.eprints-hosting.org/id/eprint/33434
Identification Number/DOI 10.1088/1748-9326/8/3/034010
Refereed Yes
Divisions Interdisciplinary Research Centres (IDRCs) > Walker Institute
Science > School of Archaeology, Geography and Environmental Science > Department of Geography and Environmental Science
Science > School of Mathematical, Physical and Computational Sciences > NCAS
Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
Publisher Institute of Physics
Download/View statistics View download statistics for this item

Downloads

Downloads per month over past year

University Staff: Request a correction | Centaur Editors: Update this record

Search Google Scholar