Please use this identifier to cite or link to this item:
Toward the predictability of meteotsunamis in the Balearic Sea using regional nested atmosphere and ocean models
|Toward the predictability of meteotsunamis in the Balearic Sea using regional nested atmosphere and ocean models
|Renault, Lionel; Vizoso, Guillermo; Jansà Clar, Agustí ; Wilkin, John; Tintoré Subirana, Joaquín
|Meteotsunamis; Oceanic waves; Atmospheric model
|American Geophysical Union
|Geophysical Research Letters. 2011, 38(10), p. 1-7
|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.
|This work has been partially funded by COOL (CTM2006‐12072/MAR), ECOOP (CTM2007‐31006E) and SOCIB Modeling Facility whose support is gratefully acknowledged.
|Appears in Collections:
|Artículos científicos 2010-2014
Items in Arcimis are protected by Creative Commons License, unless otherwise indicated.