{"id":201884,"date":"2026-03-26T19:28:08","date_gmt":"2026-03-26T18:28:08","guid":{"rendered":"https:\/\/helloproject.es\/vigilancia\/como-se-forman-los-tsunamis-los-satelites-podrian-explicar-el-origen-de-estas-olas-gigantes\/"},"modified":"2026-03-26T19:28:08","modified_gmt":"2026-03-26T18:28:08","slug":"como-se-forman-los-tsunamis-los-satelites-podrian-explicar-el-origen-de-estas-olas-gigantes","status":"publish","type":"post","link":"https:\/\/helloproject.es\/vigilancia\/como-se-forman-los-tsunamis-los-satelites-podrian-explicar-el-origen-de-estas-olas-gigantes\/","title":{"rendered":"\u00bfC\u00f3mo se forman los tsunamis? Los sat\u00e9lites podr\u00edan explicar el origen de estas olas gigantes"},"content":{"rendered":"

Estas olas monstruosas pueden recorrer miles de kil\u00f3metros, atravesar cuencas oce\u00e1nicas enteras o devastar las costas; y pese a ello, todav\u00eda se desconocen las causas exactas de su formaci\u00f3n. Un estudio, publicado en Science, revela que los sat\u00e9lites podr\u00edan ser \u00fatiles para investigar dichos fen\u00f3menos extremos.\u00a0<\/p>\n

Los investigadores creen que los sat\u00e9lites podr\u00edan ser una herramienta complementaria que delimite el origen de los terremotos, sus riesgos y din\u00e1micas<\/p>\n

De hecho, uno de ellos recab\u00f3 informaci\u00f3n del tsunami de Kamchatka de 2025 poco despu\u00e9s de su g\u00e9nesis y proporcion\u00f3 mediciones en alta resoluci\u00f3n de la superficie del mar con una precisi\u00f3n de cent\u00edmetros.\u00a0<\/p>\n

Aunque la monitorizaci\u00f3n mediante sensores del fondo marino y medidores costeros ayud\u00f3 a captar parte del evento, los sistemas se vieron limitados por la cobertura y la atenuaci\u00f3n de las ondas de corta longitud. Por ello, los investigadores creen que los sat\u00e9lites podr\u00edan ser una herramienta complementaria que delimite el origen de los terremotos, sus riesgos y la din\u00e1mica de las zonas de subducci\u00f3n.<\/p>\n


\n \"En
\n <\/a><\/p>\n

<\/a><\/p>\n

En el Mediterr\u00e1neo hubo tsunamis y podr\u00edan volver a producirse<\/h3>\n

<\/p>\n


\n SINC
\n <\/a> <\/p>\n

<\/a><\/p>\n

Sat\u00e9lites: grandes aliados\u00a0<\/h2>\n

Para saberlo, un equipo internacional liderado por la Universidad de San Diego (EE UU) analiz\u00f3 los datos del sat\u00e9lite SWOT de la NASA que sobrevol\u00f3 la regi\u00f3n por casualidad\u00a070 minutos despu\u00e9s de que empezara el evento.\u00a0<\/p>\n

Observaron que el sat\u00e9lite captur\u00f3 el campo de ondas completo y contemplaron la curvatura, direcci\u00f3n y longitud de las olas de este fen\u00f3meno catastr\u00f3fico.<\/p>\n

El sat\u00e9lite SWOT de la NASA sobrevol\u00f3 la regi\u00f3n por casualidad\u00a070 minutos\u00a0despu\u00e9s de que empezara el evento<\/p>\n

Asimismo, los an\u00e1lisis de sensibilidad revelaron que el tsunami se gener\u00f3 a unos 10 kil\u00f3metros de la zona de subducci\u00f3n, una informaci\u00f3n valiosa que no puede obtenerse mediante las\u00a0t\u00e9cnicas tradicionales.\u00a0<\/p>\n

Estos hallazgos constituyen la primera evidencia espacial en alta resoluci\u00f3n sobre el origen de un tsunami, y evidencian que estos aparatos pueden ayudar a la investigaci\u00f3n sobre la din\u00e1mica de grandes fen\u00f3menos provocados por terremotos de subducci\u00f3n en el oc\u00e9ano, unos de los eventos naturales m\u00e1s peligrosos.<\/p>\n

Referencia:\u00a0<\/p>\n

Sepulveda. et al. SWOT detects dispersive tsunami tied to a near-trench source in the 2025 Kamchatka earthquake. Science<\/a>\u00a02026<\/p>","protected":false},"excerpt":{"rendered":"

Estas olas monstruosas pueden recorrer miles de kil\u00f3metros, atravesar cuencas oce\u00e1nicas enteras o devastar las costas; y pese a ello, todav\u00eda se desconocen las causas exactas de su formaci\u00f3n. Un estudio, publicado en Science, revela que los sat\u00e9lites podr\u00edan ser \u00fatiles para investigar dichos fen\u00f3menos extremos.\u00a0 Los investigadores creen que los sat\u00e9lites podr\u00edan ser una […]<\/p>\n","protected":false},"author":5,"featured_media":0,"comment_status":"","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","ast-disable-related-posts":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"footnotes":""},"categories":[5],"tags":[],"class_list":["post-201884","post","type-post","status-publish","format-standard","hentry","category-noticias"],"yoast_head":"\n\u00bfC\u00f3mo se forman los tsunamis? 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