{"id":1591,"date":"2023-09-08T06:26:31","date_gmt":"2023-09-08T06:26:31","guid":{"rendered":"https:\/\/sarai.igme.es\/?p=1591"},"modified":"2023-09-08T06:49:46","modified_gmt":"2023-09-08T06:49:46","slug":"articulo-analysis-sar-emergency-volcanic-crisis-la-palma","status":"publish","type":"post","link":"https:\/\/sarai.igme.es\/index.php\/articulo-analysis-sar-emergency-volcanic-crisis-la-palma\/","title":{"rendered":"Publicaci\u00f3n del art\u00edculo \u201cAnalysis of SAR-derived products to support emergency management during volcanic crisis: La Palma case study\u201d en el marco de SARAI"},"content":{"rendered":"\n<p>El art\u00edculo \u201cAnalysis of SAR-derived products to support emergency management during volcanic crisis: La Palma case study\u201d, donde se reconoce el trabajo en el marco del proyecto SARAI, ha sido recientemente publicado en la prestigiosa revista Remote Sensing of Environment. El trabajo recopila las labores llevadas a cabo durante la Erupci\u00f3n del volc\u00e1n de Tajogaite (La Palma) en 2021 desde el laboratorio de Interferometr\u00eda Radar del IGME-CSIC. En el art\u00edculo se describen los diferentes resultados obtenidos para analizar la evoluci\u00f3n morfol\u00f3gica del cono, los desplazamientos superficiales regionales y los cambios en las coladas.<\/p>\n\n\n\n<p>El estudio compara los resultados obtenidos empleando im\u00e1genes SAR procedentes de 4 constelaciones de sat\u00e9lites (Sentinel-1, COSMO-SkyMed, PAZ-TerraSAR y Capella) para explorar su operatividad durante la emergencia y las posibilidades durante futuros eventos. Tambi\u00e9n se muestra como los datos SAR de alta resoluci\u00f3n espacial y temporal son capaces de detectar cambios en la estructura del cono y el avance de las nuevas coladas de lava sobre las de d\u00edas anteriores, aportando informaci\u00f3n que facilite la gesti\u00f3n de la emergencia. Para obtener informaci\u00f3n m\u00e1s detallada y datos de la investigaci\u00f3n, puedes acceder al art\u00edculo completo de acceso abierto utilizando el enlace proporcionado:<\/p>\n\n\n\n<p><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0034425723002195\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0034425723002195<\/a><\/p>\n\n\n\n<div style=\"height:50px\" aria-hidden=\"true\" class=\"wp-block-spacer\"><\/div>\n\n\n\n<figure class=\"wp-block-image aligncenter size-large\"><img decoding=\"async\" width=\"949\" height=\"1024\" src=\"https:\/\/sarai.igme.es\/wp-content\/uploads\/articulo-sarai-crisis-volcanica-La_Palma-949x1024.png\" alt=\"Figura en la que se muestran mediante patrones geom\u00e9tricos en diferentes momentos de la erupci\u00f3n, los movimientos detectados en el cono volc\u00e1nico y alrededores.\" class=\"wp-image-1592\" srcset=\"https:\/\/sarai.igme.es\/wp-content\/uploads\/articulo-sarai-crisis-volcanica-La_Palma-949x1024.png 949w, https:\/\/sarai.igme.es\/wp-content\/uploads\/articulo-sarai-crisis-volcanica-La_Palma-278x300.png 278w, https:\/\/sarai.igme.es\/wp-content\/uploads\/articulo-sarai-crisis-volcanica-La_Palma-139x150.png 139w, https:\/\/sarai.igme.es\/wp-content\/uploads\/articulo-sarai-crisis-volcanica-La_Palma-768x829.png 768w, https:\/\/sarai.igme.es\/wp-content\/uploads\/articulo-sarai-crisis-volcanica-La_Palma-1423x1536.png 1423w, https:\/\/sarai.igme.es\/wp-content\/uploads\/articulo-sarai-crisis-volcanica-La_Palma-1898x2048.png 1898w, https:\/\/sarai.igme.es\/wp-content\/uploads\/articulo-sarai-crisis-volcanica-La_Palma-463x500.png 463w, https:\/\/sarai.igme.es\/wp-content\/uploads\/articulo-sarai-crisis-volcanica-La_Palma.png 1899w\" sizes=\"(max-width: 949px) 100vw, 949px\" \/><\/figure>\n\n\n\n<p class=\"has-small-font-size\">En la figura se muestra la evoluci\u00f3n de la morfolog\u00eda del cono utilizando PAZ Stripmap (resoluci\u00f3n de 3 m) en geometr\u00eda ascendente. Las caracter\u00edsticas rojas proporcionan una interpretaci\u00f3n geomorfol\u00f3gica del \u00e1rea del cono (l\u00ednea), los respiraderos (tri\u00e1ngulos), los acantilados del cr\u00e1ter (l\u00ednea perpendicular) y los flujos de lava (flechas). Las flechas negras indican las direcciones de vuelo y observaci\u00f3n del sat\u00e9lite. a) 27\/09\/2021, b) 30\/10\/2021, c) 21\/11\/2021, d) 24\/12\/2021. (Para la interpretaci\u00f3n de las referencias al color en la leyenda de esta figura, se remite al lector a la versi\u00f3n web de este art\u00edculo).<\/p>\n","protected":false},"excerpt":{"rendered":"<p>En este art\u00edculo se describen los diferentes resultados obtenidos para analizar la evoluci\u00f3n morfol\u00f3gica del cono, los desplazamientos superficiales regionales y los cambios en las coladas en el volc\u00e1n de La Palma durante la \u00faltima crisis volc\u00e1nica.<\/p>\n","protected":false},"author":1,"featured_media":1592,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_uag_custom_page_level_css":"","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":"set","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 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este art\u00edculo se describen los diferentes resultados obtenidos para analizar la evoluci\u00f3n morfol\u00f3gica del cono, los desplazamientos superficiales regionales y los cambios en las coladas en el volc\u00e1n de La Palma durante la \u00faltima crisis volc\u00e1nica.","_links":{"self":[{"href":"https:\/\/sarai.igme.es\/index.php\/wp-json\/wp\/v2\/posts\/1591","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/sarai.igme.es\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/sarai.igme.es\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/sarai.igme.es\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/sarai.igme.es\/index.php\/wp-json\/wp\/v2\/comments?post=1591"}],"version-history":[{"count":3,"href":"https:\/\/sarai.igme.es\/index.php\/wp-json\/wp\/v2\/posts\/1591\/revisions"}],"predecessor-version":[{"id":1603,"href":"https:\/\/sarai.igme.es\/index.php\/wp-json\/wp\/v2\/posts\/1591\/revisions\/1603"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/sarai.igme.es\/index.php\/wp-json\/wp\/v2\/media\/1592"}],"wp:attachment":[{"href":"https:\/\/sarai.igme.es\/index.php\/wp-json\/wp\/v2\/media?parent=1591"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/sarai.igme.es\/index.php\/wp-json\/wp\/v2\/categories?post=1591"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/sarai.igme.es\/index.php\/wp-json\/wp\/v2\/tags?post=1591"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}