Mass Movement-Induced Tsunami Hazard on Perialpine Lake Lucerne (Switzerland): Scenarios and Numerical Experiments

Previous studies of the sediments of Lake Lucerne have shown that massive subaqueous mass movements affecting unconsolidated sediments on lateral slopes are a common process in this lake, and, in view of historical reports describing damaging waves on the lake, it was suggested that tsunamis generated by mass movements represent a considerable natural hazard on the lakeshores. Newly performed numerical simulations combining two-dimensional, depth-averaged models for mass-movement propagation and for tsunami generation, propagation and inunda- tion reproduce a number of reported tsunami effects. Four analysed mass-movement scenarios—three based on documented slope failures involving volumes of 5.5 to 20.8 9 106 m3—show peak wave heights of several metres and maximum runup of 6 to [10 m in the directly affected basins, while effects in neighbouring basins are less drastic. The tsunamis cause large-scale inundation over distances of several hundred metres on flat alluvial plains close to the mass-movement source areas. Basins at the ends of the lake experience regular water-level oscillations with characteristic periods of several minutes. The vulnerability of potentially affected areas has increased dramatically since the times of the damaging historical events, recommending a thorough evaluation of the hazard.

Reconstructing 4000 years of mass movement and tsunami history in a deep peri-Alpine lake (Lake Geneva, France-Switzerland)

The study of mass movements in lake sediments provides insights into past natural hazards at historic and prehistoric timescales. Sediments from the deep basin of Lake Geneva reveal a succession of six large-scale (volumes of 22 × 106 to 250 × 106 m3) mass-transport deposits, associated with five mass-movement events within 2600 years (4000 cal bp to 563 ad). The mass-transport deposits result from: (i) lateral slope failures (mass-transport deposit B at 3895 ± 225 cal bp and mass-transport deposits A and C at 3683 ± 128 cal bp); and (ii) Rhône delta collapses (mass-transport deposits D to G dated at 2650 ± 150 cal bp, 2185 ± 85 cal bp, 1920 ± 120 cal bp and 563 ad, respectively). Mass-transport deposits A and C were most probably triggered by an earthquake, whereas the Rhône delta collapses were likely to be due to sediment overload with a rockfall as the external trigger (mass-transport deposit G, the Tauredunum event in 563 ad known from historical records), an earthquake (mass-transport deposit E) or unknown external triggers (mass-transport deposits D and F). Independent of their origin and trigger mechanisms, numerical simulations show that all of these recorded mass-transport deposits are large enough to have generated at least metre-scale tsunamis during mass movement initiation. Since the Tauredunum event in 563 ad, two small-scale (volumes of 1 to 2 × 106 m3) mass-transport deposits (H and I) are present in the seismic record, both of which are associated with small lateral slope failures. Mass-transport deposits H and I might be related to earthquakes in Lausanne/Geneva (possibly) 1322 ad and Aigle 1584 ad, respectively. The sedimentary record of the deep basin of Lake Geneva, in combination with the historical record, show that during the past 3695 years, at least six tsunamis were generated by mass movements, indicating that the tsunami hazard in the Lake Geneva region should not be neglected, although such events are not frequent with a recurrence time of 0·0016 yr−1.

Maximum intensity projection of cranial computed tomography data for dental identification

Dental radiographs play the major role in the identification of victims in mass casualties besides DNA. Under circumstances such as those caused by the recent tsunami in Asia, it is nearly impossible to document the entire dentition using conventional x-rays as it would be too time consuming. Multislice computed tomography can be used to scan the dentition of a deceased within minutes, and the postprocessing software allows visualization of the data adapted to every possible antemortem x-ray for identification. We introduce the maximum intensity projection of cranial computed tomography data for the purpose of dental identification exemplarily in a case of a burned corpse. As transportable CT scanners already exist, these could be used to support the disaster victim identification teams in the field.

Fukushima und die Folgen. Medienberichterstattung, Öffentliche Meinung, Politische Konsequenzen

Am 11. März 2011 ereignete sich vor der japanischen Küste ein schweres Erdbeben. Es löste einen gewaltigen Tsunami aus, der an der Ostküste Japans schwere Schäden hervorrief und fast 20.000 Menschen das Leben kostete. Im Atomkraftwerk Fukushima verursachte der Tsunami eine Reaktorkatastrophe, in deren Folge insbesondere in Deutschland eine heftige Diskussion über die Atomenergie entflammte, die schließlich zum deutschen Atomausstieg führte. Die Reaktorkatastrophe erfuhr international eine große öffentliche (Medien-) Aufmerksamkeit und rief auch die kommunikationswissenschaftliche Forschung auf den Plan. Ergebnisse dieser Forschungen, die an verschiedenen Stellen unabhängig voneinander durchgeführt wurden, sind in diesem Band versammelt. In insgesamt 13 Beiträgen werden die medialen und öffentlichen Reaktionen auf das Unglück empirisch analysiert. Die Beiträge befassen sich zum einen mit der Darstellung der Atomenergie in historischer Vergleichsperspektive, wobei die Reaktorkatastrophe in Tschernobyl als Referenzpunkt für Fukushima diente. In weiteren Beiträgen wird die Dynamik der Berichterstattung in Deutschland fokussiert. Fünf Beiträge betrachten die Reaktionen der Medien in internationaler Vergleichsperspektive und weitere vier untersuchen die Reaktionen der Bevölkerung auf die Ereignisse in Fukushima. Die Beiträge beruhen überwiegend auf quantitativen Inhaltsanalysen und Befragungen, aber es wurden auch qualitative Methoden sowie automatisierten Verfahren der Textanalyse verwendet. Zudem wurden in mehreren Studien verschiedene Formen der Datenerhebung kombiniert. Durch die Zusammenführung der unterschiedlichen Perspektiven wird eine differenzierte Einschätzung der medialen und gesellschaftlichen Konsequenzen des Extremereignisses möglich. Die Umrisse eines Forschungsprogramms für die Nachhaltigkeits-, Energie- und Umweltkommunikation werden sichtbar.