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Observing meteotsunamis (“Marrobbio”) on the southwestern coast of Sicily

Author

Listed:
  • Petra Zemunik

    (Institute of Oceanography and Fisheries)

  • Angelo Bonanno

    (Istituto per lo studio degli impatti Antropici e Sostenibilità in ambiente marino, Consiglio Nazionale delle Ricerche, UOS di Capo Granitola)

  • Salvatore Mazzola

    (Istituto per lo studio degli impatti Antropici e Sostenibilità in ambiente marino, Consiglio Nazionale delle Ricerche, UOS di Capo Granitola)

  • Giovanni Giacalone

    (Istituto per lo studio degli impatti Antropici e Sostenibilità in ambiente marino, Consiglio Nazionale delle Ricerche, UOS di Capo Granitola)

  • Ignazio Fontana

    (Istituto per lo studio degli impatti Antropici e Sostenibilità in ambiente marino, Consiglio Nazionale delle Ricerche, UOS di Capo Granitola)

  • Simona Genovese

    (Istituto per lo studio degli impatti Antropici e Sostenibilità in ambiente marino, Consiglio Nazionale delle Ricerche, UOS di Capo Granitola)

  • Gualtiero Basilone

    (Istituto per lo studio degli impatti Antropici e Sostenibilità in ambiente marino, Consiglio Nazionale delle Ricerche, UOS di Capo Granitola)

  • Julio Candela

    (Centro de Investigación Científica y de Educación Superior de Ensenada (CICESE))

  • Jadranka Šepić

    (Institute of Oceanography and Fisheries
    University of Split)

  • Ivica Vilibić

    (Institute of Oceanography and Fisheries)

  • Salvatore Aronica

    (Istituto per lo studio degli impatti Antropici e Sostenibilità in ambiente marino, Consiglio Nazionale delle Ricerche, UOS di Capo Granitola)

Abstract

The paper presents sea level and air pressure observations acquired during the 2007 experiment carried out along the southwestern coast of Sicily. The experiment aimed to quantify the atmospheric and oceanic conditions related with the phenomenon of marrobbio, a kind of meteotsunami that is frequently observed in the Strait of Sicily. Sea level data measured at surrounding tide gauges, radio-sounding atmospheric profiles and ERA5 reanalysis data conjoined the analysis. Rapid air pressure and sea level oscillations were measured simultaneously during marrobbio events, while the atmospheric disturbances were estimated to propagate mostly towards east-northeast with a predominant speed of 19–24 m/s. The observed propagation direction and speed were found conducive for generation of long ocean waves through Proudman resonance over a wide outer shelf, although a complex bathymetry in front of affected area may strongly modify the generation. The atmospheric patterns were favourable for wave ducting mechanism during most of the observed marrobbio events. A need for establishing long-term high-frequency observations at marrobbio hot spots, as well to apply high-resolution atmospheric and oceanic models for proper quantification of meteotsunamis, is emphasized.

Suggested Citation

  • Petra Zemunik & Angelo Bonanno & Salvatore Mazzola & Giovanni Giacalone & Ignazio Fontana & Simona Genovese & Gualtiero Basilone & Julio Candela & Jadranka Šepić & Ivica Vilibić & Salvatore Aronica, 2021. "Observing meteotsunamis (“Marrobbio”) on the southwestern coast of Sicily," Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 106(2), pages 1337-1363, March.
  • Handle: RePEc:spr:nathaz:v:106:y:2021:i:2:d:10.1007_s11069-020-04303-2
    DOI: 10.1007/s11069-020-04303-2
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    References listed on IDEAS

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