Factores que influyen en la forma de la cola de un tsunami.
保存先:
| 著者: | |
|---|---|
| フォーマット: | artículo original |
| 状態: | Versión publicada |
| 出版日付: | 2009 |
| その他の書誌記述: | The propagation speed of a tsunami depends on the depth of the ocean in which it propagates. As the tsunami crosses the abyssal plain, it suffers modifications in its form due to change in the depths of the ocean bottom. When the tsunami is reflected on coasts, islands or bathymetric discontinuities, the reflected wave is added to the original form of the tsunami. In this work it is identified how several factors affect the wave-form of a tsunami during its propagation through abyssal plains, by numerical simulations of a tsunami´s propagation from Alaska to Hawai. |
| 国: | Portal de Revistas UNA |
| 機関: | Universidad Nacional de Costa Rica |
| Repositorio: | Portal de Revistas UNA |
| 言語: | Español |
| OAI Identifier: | oai:www.revistas.una.ac.cr:article/6741 |
| オンライン･アクセス: | https://www.revistas.una.ac.cr/index.php/uniciencia/article/view/6741 |
| キーワード: | Tsunami propagation tsunami wave-form tsunami reflections Pacific Ocean abyssal plain’s bathymetry. Propagación de tsunamis forma de onda de un tsunami reflexiones de tsunamis Océano Pacífico batimetría de las planicies abisales. |