Mathematics – Logic
Scientific paper
May 2011
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011georl..3810601r&link_type=abstract
Geophysical Research Letters, Volume 38, Issue 10, CiteID L10601
Mathematics
Logic
1
Atmospheric Processes: Mesoscale Meteorology, Oceanography: General: Numerical Modeling (0545, 0560, 1952), Oceanography: General: Ocean Predictability And Prediction (3238, 4315), Oceanography: Physical: Air/Sea Interactions (0312, 3339), Oceanography: Physical: Tsunamis And Storm Surges (4302, 4304)
Scientific paper
Meteotsunamis are oceanic waves that possess tsunami-like characteristics but are meteorological in origin. In the western Mediterranean, travelling atmospheric pressure oscillations generate these long oceanic surface waves that can become amplified and produce strong seiche oscillations inside harbors. We analyze a June 2006 meteotsunami event in Ciutadella harbor (Menorca Island, Spain), studying numerically the phenomenon during its full life cycle, from the early atmospheric stages to the atmosphere-ocean resonant phase and the final highly amplified harbor oscillation. The Weather Research Forecast (WRF) atmospheric model adequately reproduces the development of a convective nucleus and also reproduces the induced atmospheric pressure oscillations moving at a speed of 27 m/s. The oceanic response is studied using the Regional Ocean Modeling System (ROMS), forced by the WRF pressure field. It shows an inverse barometer wave front in the open ocean progressively amplified through resonant interactions in the different shelf and coastal regions. The predictive capability of this new WRF/ROMS modeling approach is then discussed.
Jansá Agustin
Renault Lionel
Tintore Joaquin
Vizoso Guillermo
Wilkin John
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