The Nevelsk tsunami on August 2, 2007: Instrumental data and numerical modeling

Dynamics of interaction between solitary and rogue wave of the space-time fractional Broer–Kaup models arising in shallow water of harbor and coastal zone

“…The researchers can compare their experimental/numerical results with our exact results like Ref. [1,2], and civil engineer's may convey to predict disaster situations of harbor regions by taking preventive initiatives with help of our results. The future prospect of the fractional models holds strong.…”

“…Any researcher can compare their experimental/numerical results with our exact solutions to require actual investigation like Ref. [1,2].…”

“…Tsunamis type massive waves create dissipated energy that travels through water medium and when the depth of the ocean decreases, the wave height increase to higher. The velocity of tsunami waves depends on ocean intensity instead of the gap from the source of the wave [2]. It is, therefore, an important event whose study will contribute to better understanding of coastal hazards from seismic waves.…”

The depth effect of earthquakes on tsunami heights in the Sea of Okhotsk

“…If the focal depth had been shallow, for example 60 km, the tsunami would have been effective and the wave height would have reached several meters, mainly along the east of Sakhalin Island and the west of the Kamchatka Peninsula. The analysis of the 2013 Sea of Okhotsk tsunami event given in this study, along with previous studies (Kim and Rabinovich, 1990;Lobkovsky et al, , 2009Zaitsev et al, 2008;Baranov et al, 2013), indicates the importance of a special study on tsunami hazard assessment in the Sea of Okhotsk. The tsunami source was calculated from the elastic dislocation theory using the algorithm of Okada (1985).…”