1 / 12

Climate change and North Sea storm surge extremes - an ensemble study (PRUDENCE)

Climate change and North Sea storm surge extremes - an ensemble study (PRUDENCE). Katja Woth & Hans von Storch Institute for Coastal Research GKSS Research Center Geesthacht, Germany. Institute for Coastal Research GKSS, Germany. Assessing ongoing change of coastal climate.

tanek
Télécharger la présentation

Climate change and North Sea storm surge extremes - an ensemble study (PRUDENCE)

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Climate change and North Sea storm surge extremes - an ensemble study (PRUDENCE) Katja Woth & Hans von Storch Institute for Coastal Research GKSS Research Center Geesthacht, Germany

  2. Institute for Coastal ResearchGKSS, Germany • Assessing ongoing change of coastal climate. • Deriving scenarios of plausible, possible futures of coastal climates. • Special emphasis on wind-related aspects, i.e., wind force, storm surges and ocean waves. • Special emphasis on North Sea and Baltic Sea. • Participant in HIPOCAS, PRUDENCE and ENSEMBLES.

  3. NCEP Globale Reanalysen ( 210 km x 210 km )1958 - 2002 BAW - TELEMAC 2DWasserstand und barotrope Strömung 21.02.1993 12 UTC REMO Windgeschwindigkeit und Richtung 21.02.1993 12 UTC HIPOCAS:Für Rekonstruktionen verwendete Modellkette Gebiet hier: Nordsee und östlicher Nordatlantik WAM sig. Wellenhöhe und Richtung 21.02.1993 12 UTC Auflösung etwa 50 x 50 km Auflösung zwischen etwa 100 m und 5km Auflösung etwa 5 x 5 km

  4. Climate risk assessments done with these models • Reconstruction of past and ongoing state and change • PCPnP futures(PCPnP = plausible, consistent, possible but not necessarily probable = scenarios)

  5. Comparison of wind speed statistics with in-situ data: RCM is skillful in describing marine wind statistics Not assimilated into NCEP (Ionic Sea)

  6. External Forcing – Future Scenarios

  7. EU-Project PRUDENCE (Prediction of Regional scenarios and Uncertainties for Defining EuropeaN Climate change risks and Effects) GCM RCMs • RegionalClimate Models: • CLM- REMO- HIRHAM- RCAO Global Climate Model (HadAM3) IPCC A2 SRES Scenario(1961-1990 / 2071-2100) today today Storm SurgeModel forthe North Sea: - TRIM 3D Impact model Impact scenarios scenario scenario global local scale

  8. A2 - CTL: changes in 99 % - iles of wind speed (6 hourly, DJF): west wind sector selected(247.5 to 292.5 deg) HIRHAM RCAO REMO5 CLM

  9. Projections for the future / surge meteorological forcing: HIRHAM / RCA Differencesin inter-annual percentiles of surge/ A2 - CTL: RCA Differences in inter-annual percentiles of surge/ A2 - CTL: HIRHAM

  10. Mean change of winter 95%ile surge levels Near coastal model cells

  11. According to scenario A2 and the specific set of GCM / RCMs, water level may rise in extreme situations by as much as 40 cm + 30 cm = 70 cm along the German North Sea coast. IPCC, 2001 SREs emission scenarios: Impact on global sea level

  12. Conclusions • Dynamical models have been demonstrated to be a useful tool to describe the statistics, and changes thereof, of wind-related phenomena in coastal seas – wind force, storm surge, coastal currents and ocean waves. • An ensemble of regionalizations, derived from one global A2 scenario, results in rather similar changes of regional wind over the North sea and the associated change of surge levels. • Along the German North Sea coast, water levels may rise by up to 70 cm - of which 40 cm are due to mean sea level rise and 30 cm to different storm patterns.

More Related