4.6 Article

The impact of climate change on storm surges over Irish waters

Journal

OCEAN MODELLING
Volume 25, Issue 1-2, Pages 83-94

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.ocemod.2008.06.009

Keywords

ROMS; Storm surge; Regional atmosphere model; Extreme surge

Funding

  1. Environmental Protection Agency (under the National Development Plan)
  2. Met Eireann, Sustainable Energy Ireland
  3. Higher Education Authority
  4. CosmoGrid
  5. Programme for Research in Third Level Institutions (PRTLI)
  6. Irish Higher Education
  7. National Development Plan
  8. European Regional Development Fund
  9. CNES
  10. British Oceanographic Data Center

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The Regional Ocean Model System (ROMS) of Rutgers University is used to investigate the influence of anthropogenic climate change on storm surges over Irish waters, particularly on the extreme values. Two experiments were performed to confirm the validity of the approach in the current climate: the first focused on hindcasting the surge generated by a storm in early 2002 while the second provided surge statistics by running the model for the period 1990-2002; in both cases ROMS was driven with ERA-40 forcing fields. The results show that the model is capable of simulating both specific surge events and surge climate statistics with reasonable accuracy (order of 10 cm). Model outputs were also compared spatially against satellite altimetry data, corrected for long wavelength errors, from 1993 to 2001. The ROMS model consistently reproduces the sea level changes in the Irish Sea, and over the waters to the south and west of Ireland. For the investigation of the impact of the climate change on storm surges, the same configuration of ROMS was driven by atmospheric forcing fields downscaled from ECHAM5/OM1 data for the past (1961-1990) and future (2031-2060; SIZES A1B greenhouse gas scenario); the clownscaled data were produced using the Rossby Centre Regional Atmosphere model (RCA3). The results show an increase in storm surge events around Irish coastal areas in the future projection, except along the south Irish coast; there is also a significant increase in the height of the extreme surges along the west and east coasts, with most of the extreme surges occurring in wintertime. (c) 2008 Elsevier Ltd. All rights reserved.

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