Modeling Submarine Landslide-Generated Waves in Lake Ohrid, Macedonia/Albania
- 1.6k Downloads
We study potential tsunami hazards associated with submarine landslides in Lake Ohrid, Macedonia/Albania. The transboundary Lake Ohrid located on the Balkan Peninsula shared by Macedonia and Albania is considered to be the oldest- continuously existing lake in Europe (2–5 Ma), though the age and the origin are not completely unraveled to date. Previous studies by means of hydroacoustic methods have shown that the western margin of Lake Ohrid has a long history of mass wasting. Based on seismic data, slide deposits are found in different stratigraphic levels as well as on the lake floor where they have affected a large area. This study is focused on the well-studied Udenisht Slide Complex covering an area of 27 km2 within the southwestern part of Lake Ohrid. The Udenisht slide is by far the largest mass movement with an average thickness of 30–40 m and an estimated volume of about 0.11 km3. It is therefore well within the limits of submarine landslides that are known to be capable of triggering tsunamis. Using numerical modeling, the propagation of a landslide-generated tsunami with an initial wave height of more than 5 m has been calculated. Run-up heights estimated for coastal communities around the lake are moderate in the north (2–3 m) can reach up to 10 m directly at the site where the slide initiated. This study is a first generation of landslide tsunami hazard assessment for Lake Ohrid and further detailed modeling is recommended for the region.
KeywordsLake Ohrid Submarine landslide Tsunami Numerical modeling
We thank the reviewers Hendrik Vogel and Ahmet C. Yalciner as well as the editor Carl B. Harbitz for their comments and suggestions that improved the manuscript. The TUNAMI-N2 code used is this paper is originally authored by Professors Fumihiku Imamura and Nobou Shuto at the Tohoku University in Japan. TUNAMI-N2 is copyrighted to Professors Ahmet C. Yalciner, Fumihiku Imamura and Costas E. Synolakis. We acknowledge them for developing and making available the code to scientists around the world. We also would like to thank Sascha Brune for his constructive cooperation regarding landslide tsunami modeling. We also thank C. Berndt for valuable comments.
- Harbitz C, Løvholt F, Pedersen G, Masson D (2006) Mechanisms of tsunami generation by submarine landslides: a short review. Nor J Geol 86:255–264Google Scholar
- Imamura F, Yalciner AC, Ozyurt G (2006) Tsunami modelling manual. UNESCO IOC international training course on Tsunami Numerical ModellingGoogle Scholar
- Lindhorst K (2012) Neotectonic and sedimentary evolution of Lake Ohrid (Albania/Macedonia): acquisition and interpretation of new hydro-acoustic and seismic data. Unpublished PhD thesis, Christian-Albrechts-Universität zu Kiel, KielGoogle Scholar
- Lindhorst K, Vogel H, Krastel S, Wagner B, Hilgers A, Zander A, Schwenk T, Wessels M, Daut G (2010) Stratigraphic analysis of lake level fluctuations in Lake Ohrid: an integration of high resolution hydro-acoustic data and sediment cores. Biogeosciences 7:3531–3548. doi: 10.5194/bgd-7-3651-2010 CrossRefGoogle Scholar
- Lynett P, Liu PL-F (2005) A numerical study of the run-up generated by three-dimensional landslides. J Geophys Res 110(C3):C03006Google Scholar
- Ward SN, Day S (2007) Tsunami balls: a granular approach to tsunami runup and inundation. Commun Comput Phys 3(1):222–249Google Scholar
- Yeh HH-J, Liu PL, Synolakis C (1996) Long-wave runup models: Friday Harbor, USA, 12–17 September 1995. World Scientific, SingaporeGoogle Scholar