Storm surges during IANOS Medicane

Author:

Androulidakis Yannis1,Makris Christos1,Mallios Zissis1,Pytharoulis Ioannis2,Baltikas Vassilis1,Krestenitis Yannis1

Affiliation:

1. Aristotle University of Thessaloniki Faculty of Engineering: Aristoteleio Panepistemio Thessalonikes Polytechnike Schole

2. Aristotle University of Thessaloniki School of Sciences: Aristoteleio Panepistemio Thessalonikes Schole Thetikon Epistemon

Abstract

Abstract The IANOS Medicane was one the most severe storms that have formed in the Mediterranean Sea with Category 2 Hurricane characteristics. The storm induced a significant increase of sea level elevation along its pathway and caused the occurrence of storm surges at the central Ionian Sea with consequent impacts on coastal regions of the Ionian islands and western Greece. A multi-platform approach, based on hydrodynamic ocean simulations, nested to meteorological and coastal flooding simulations, is used in combination with field and satellite observations to describe the marine weather conditions, the storm surge characteristics, and the coastal inundation processes due to the impact of IANOS Medicane in September 2020. Both wind and atmospheric pressure patterns affected the storm surge variability over the Ionian Sea. The direct intrusion of the Medicane from the central Mediterranean Sea towards the Ionian Sea formed storm surges over several coastal areas, even before the storm's landfall, due to the accompanying onshore currents. Storm surges in the order of 30 cm generated extensive flooding over lowland coastal areas, as confirmed by both satellite (Normalized Difference Water Index: NDWI) and numerical (coastal inundation modeling) data. Satellite-derived and simulated estimations showed that, in specific coastal regions, the run-up of seawater extended up to 200 m inland, depending on the hydraulic connectivity between the lowland areas, which determined the inundation extents during the storm surge.

Publisher

Research Square Platform LLC

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