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- W2089486047 abstract "The 1883 Krakatau tsunami provides an important clue for solving the mechanisms of the eruption of Krakatau. First, sea waves of volcanic origin are basically classified. The travel times of the crest of the largest tsunami in the 1883 Krakatau eruption are recalculated taking the wave heights and the sea depths along the path into consideration. As a special case of sea waves, air waves coupled with those of the sea are examined and the necessary conditions of their generation are discussed: the sea depths must be around 5 km, the sea wave paths require long stretches of sea, and the magnitudes of volcanic explosions must be large to produce the air-sea waves. The information collected suggests that the tsunamis registered at Batavia (Jakarta) were not air sea-waves. Some results of the recent reflection survey of the subbottom materials and a supplemental gravity survey in the Krakatau area are introduced to provide further evidence for explosive mechanisms. The origin times of the onset and the crest of the tsunami and the air wave, both registered at Batavia, are calculated from their travel times. Adopting these origin times, the author reconstructs a scenario of the tsunami. In order to generate a tsunami, as long as about 60 km wave length, successive developments of surges and water domes seem to be necessary." @default.
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- W2089486047 date "1987-12-01" @default.
- W2089486047 modified "2023-10-18" @default.
- W2089486047 title "A scenario of the 1883 Krakatau tsunami" @default.
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- W2089486047 doi "https://doi.org/10.1016/0377-0273(87)90097-7" @default.
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