Abstract

Two hazardous typhoons, Lionrock (August 2016) and Jebi (September 2018), destructively affected the coast of Japan and produced extreme sea level variations. The results of field surveys in the impacted regions showed that multiple deaths and extensive floods were caused by the combined effect of low-frequency sea level raise (storm surges) and intensive high-frequency (HF) tsunami-like waves (meteotsunamis). The data from ten tide gauges for the 2016 event and eight gauges for the 2018 event were used to examine the properties of the observed sea levels, to estimate the relative contribution of the two sea level components and to evaluate their statistical characteristics (maximum wave heights, amplitudes and periods of individual components, etc.). For the 2016 event, we found that the surge heights were from 12 to 35 cm and that the mean contribution of surges into the total observed sea level heights was ~ 39%; the meteotsunami amplitudes were from 22 to 92 cm, and they contributed 61% of the total height. For the 2018 event, storm surges were significantly stronger, from 46 to 170 cm, while HF amplitudes were from 38 to 130 cm; their relative inputs were 67% and 33%, respectively. Combined, they formed total flood heights of up to 120 cm (2016 event) and 288 cm (2018 event). Previously, the contribution of storm seiches (meteotsunamis) in coastal floods had been underestimated, but results of the present study demonstrate that they can play the principal role. What is even more important, they produce devastating currents: according to our estimates, current speeds were up to 3 knots (1.5 m/s) during the Lionrock event and more than 5 knots (2.6 m/s) during Jebi; these strong currents appear to be the main reason for the resulting damage of coastal infrastructure. The most important characteristic of the recorded meteotsunamis is their trough-to-crest maximum height. During the 2016 event, these heights at three stations were > 1 m: 171 cm at Erimo, 109 cm at Hachijojima and 102 cm at Ayukawa. The 2018 event was stronger; maximum meteotsunami wave heights were 257 cm at Gobo, 138 cm at Kushimoto, 137 cm at Kumano and 128 cm at Murotomisaki. The 2018 Gobo height of 257 cm is much larger than historical non-seismic seiche maxima for the Pacific coast of Japan (140–169 cm) estimated by Nakano and Unoki (1962) for the period of 1930–1956.

Highlights

  • Meteorological tsunamis are strong tsunami-like ocean waves generated by atmospheric processes

  • The field surveys in the impacted regions showed that the multiple deaths and extensive floods in these regions were caused by the combined effect of low-frequency sea level rise and intensive high-frequency tsunami-like seiches

  • We used the data from ten coastal tide gauges for the 2016 event and eight tide gauges for the 2018 event to examine the properties of the sea level oscillations in the affected regions, to estimate the relative contribution of these two sea level components and to evaluate their statistical characteristics

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Summary

Introduction

Meteorological tsunamis (meteotsunamis) are strong tsunami-like ocean waves generated by atmospheric processes. Typhoons are usually associated with a number of hazards in a cascading order, including severe storm waves, wind-blown debris, storm surges, extreme seiches, intensive rainfall, landslides and debris flows (cf Heidarzadeh et al 2018, 2020b). Severe typhoons are characterized by very low air pressure and are frequently accompanied by sustained hurricane onshore winds These two factors cause powerful surges on the oceanic coasts of Japan. The primary focuses of their studies were field surveys of the affected territories and numerical modelling of generated storm surges The results of their studies showed that multiple deaths and extensive coastal floods were partly caused by intensive high-frequency tsunami-like waves observed at several sites. The typhoon caused intense floods in coastal regions associated with extreme rainfalls, storm surges and seiches

Description of the event on the east coast of Japan
The combined effect of storm surges and meteotsunamis
Observed sea level oscillations
Time–frequency analysis
Description of the event on the south‐east coast of Japan
Discussion and perspectives
Findings
Conclusions
Compliance with ethical standards
Full Text
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