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Sources of 21St Century Regional Sea Level Rise Along the Coast of North-west Europe : Volume 10, Issue 6 (17/12/2013)

By Howard, T.

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Book Id: WPLBN0004020742
Format Type: PDF Article :
File Size: Pages 27
Reproduction Date: 2015

Title: Sources of 21St Century Regional Sea Level Rise Along the Coast of North-west Europe : Volume 10, Issue 6 (17/12/2013)  
Author: Howard, T.
Volume: Vol. 10, Issue 6
Language: English
Subject: Science, Ocean, Science
Collections: Periodicals: Journal and Magazine Collection (Contemporary), Copernicus GmbH
Historic
Publication Date:
2013
Publisher: Copernicus Gmbh, Göttingen, Germany
Member Page: Copernicus Publications

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Lowe, J. A., Ridley, J., Howard, T., Pardaens, A. K., W. L. Hurkman, R. T., Bamber, J. L.,...Vaughan, D. (2013). Sources of 21St Century Regional Sea Level Rise Along the Coast of North-west Europe : Volume 10, Issue 6 (17/12/2013). Retrieved from http://www.ebooklibrary.org/


Description
Description: Met Office Hadley Centre, FitzRoy Road, Exeter, EX1 3PB, UK. Changes in both global and regional mean sea level, and changes in the magnitude of extreme flood heights, are the result of a combination of several distinct contributions most, but not all, of which are associated with climate change. These contributions include effects in the solid earth, gravity field, changes in ocean mass due to ice-loss from ice sheets and glaciers, thermal expansion, alterations in ocean circulation driven by climate change and changing freshwater fluxes, and the intensity of surge tides. Due to the diverse range of models required to simulate these systems, the contributions to sea-level change have usually been discussed in isolation rather than as a fully-coupled system. Focusing on the coastline of Northwest Europe, we consider all these processes and their relative impact on 21st century regional mean sea levels and extreme flood height. As far as possible our projections of change are derived from process-based models forced by the A1B emissions scenario to provide a self-consistent comparison of the contributions. We address uncertainty by considering both a mid-range and an illustrative high-end combination of the different components.

For our mid-range ice-loss scenario we find that thermal expansion of seawater is the dominant contributor to change in sea level by 2100. However, the projected contribution to extreme sea level, due to changes in storminess alone, is significant and in places is comparable to the global mean contribution of thermal expansion. For example, under the A1B emissions scenario, by 2100, change in storminess contributes around 15 cm to the increase in projected height of the 50 yr storm surge on the west coast of the Jutland Peninsula, compared with a contribution of around 22 cm due to thermal expansion. An illustrative combination of our high-end projections suggests increases in the 50 yr return level of 86 cm at Sheerness, 95 cm at Roscoff, 106 cm at Esbjerg, and 67 cm at Bergen. The notable regional differences between these locations arise from differences in rate of vertical land movement and changes in storminess.


Summary
Sources of 21st century regional sea level rise along the coast of North-West Europe

Excerpt
Araujo, I. B. and Pugh, D. T.: Sea levels at Newlyn 1915–2005: analysis of trends for future flooding risks, J. Coastal Res., 24, 203–212, doi:10.2112/06-0785.1, 2008.; Coles, S.: An introduction to statistical modeling of extreme values, Springer, 208 pp., 2001.; Brown, S., Boorman, P., McDonald, R., and Murphy, J.: Use and interpretation of surface wind projections from the 11-member Met Office Regional Climate Model ensemble, UKCP09 Technical Note. Met Office Hadley Centre, Exeter, UK, available at: http://ukclimateprojections.defra.gov.uk (last access: 12 December 2013), 2009.; Church, J. A., Clark, P. U., Cazenave, A., Gregory, J. M., Jevrejeva, S., Levermann, A., Merrifield, M. A., Milne, G. A., Nerem, R. S., Nunn, P. D., Payne, A. J., Pfeffer, W. T., Stammer, D., and Unnikrishnan, A. S.: Sea level change, in: Climate Change 2013: The Physical Science Basis Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, edited by: Stocker, T. F., Qin, D., Plattner, G.-K., Tignor, M., Allen, S. K., Boschung, J., Nauels, A., Xia, Y., Bex, V., and Midgley, P. M., Cambridge University Press, Cambridge, UK and New York, NY, USA, in press, 2013.; Lempérière, F.: The role of dams in the XXI century: achieving a sustainable development target, International Journal on Hydropower and Dams, 13, 99–108, 2006.; Debernard, J. B. and Roed, L. P.: Future wind, wave and storm surge climate in the Northern Seas: a revisit, Tellus A, 60, 427–438, doi:10.1111/j.1600-0870.2008.00312.x, 2008.; de Winter, R. C., Sterl, A., and Ruessink, B. G.: Wind extremes in the North Sea Basin under climate change: An ensemble study of 12 CMIP5 GCMs, J. Geophys. Res.-Atmos., 118, 1601–1612, doi:10.1002/jgrd.50147, 2013.; Flather, R. A., Smith, J. A., Richards, J. D., Bell, C., and Blackman, D. L.: Direct estimates of extreme storm surge elevations from a 40 yr numerical model simulations and from observations, The Global Atmosphere and Ocean System, 6, 165–176, 1998.; Gaslikova, L., Grabemann, I., and Groll, N.: Changes in North Sea storm surge conditions for four transient future climate realizations, Nat. Hazards, 66, 1501–1518, doi:10.1007/s11069-012-0279-1, 2013.; Giesen, R. H. and Oerlemans, J.: Climate-model induced differences in the 21st century global and regional glacier contributions to sea-level rise, Clim. Dynam., 41, 1–18, 2013.; Goelzer, H., Huybrechts, P., Fürst, J. J., Nick, F. M., Andersen, M. L., Edwards, T. L., Fettweis, X., Payne, A. J., and Shannon, S. R.: Sensitivity of Greenland ice sheet projections to model formulations, J. Glaciol., 59, 733–749, 2013.; Haigh, I., Nicholls, R., and Wells, N.: Assessing changes in extreme sea levels: application to the English Channel, 1900–2006, Cont. Shelf. Res., 30, 1042–1055, doi:10.1016/j.csr.2010.02.002, 2010.; Howard, T., Lowe, J., and Horsburgh, K.: Interpreting century-scale changes in Southern North Sea storm surge climate derived from coupled model simulations, J. Climate, 23, 6234–6247, doi:10.1175/2010jcli3520.1, 2010.; Howard, T., Ridley, J., Pardaens, A. K., Hurkmans, R. T. W. L., Payne, A. J., Giesen, R. H., Lowe, J. A., Bamber, J. L., Edwards, T. L., and Oerlemans, J.: The land-ice contribution to 21st century dynamic sea level rise, Ocean Sci. Discuss., submitted, 2013.; Jenkins, G. J., Perry, M. C., and Prior, M. J.: The climate of the UK and recent trends. Met Office Hadley Centre, Exeter, UK, available at:

 

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