{"id":4363,"date":"2025-01-17T16:42:49","date_gmt":"2025-01-17T16:42:49","guid":{"rendered":"https:\/\/www.andex-rhp.org\/?p=4363"},"modified":"2025-01-17T16:42:50","modified_gmt":"2025-01-17T16:42:50","slug":"estacionalidad-de-los-tornados-en-el-centro-sur-de-chile","status":"publish","type":"post","link":"https:\/\/www.andex-rhp.org\/?p=4363","title":{"rendered":"Estacionalidad de los tornados en el centro-sur de Chile"},"content":{"rendered":"\n<p><strong>Por Roberto Rondanelli*\/<\/strong><\/p>\n\n\n\n<p>En Caballero-Mor\u00e1n y Rondanelli\u00a0<a href=\"https:\/\/paperpile.com\/c\/C7tVAU\/8Q59\/?noauthor=1\" target=\"_blank\" rel=\"noreferrer noopener\">(2025)<\/a><sup>1<\/sup>\u00a0estudiamos la estacionalidad de los tornados en Chile Centro-Sur. Tempranamente en el estudio de los tornados, nos llam\u00f3 la atenci\u00f3n el hecho que los tornados parecen ocurrir mayormente\u00a0 desde mediados de Mayo a mediados de Junio con mucha regularidad, a lo largo de las observaciones de tornados disponibles desde el a\u00f1o 1554\u00a0<a href=\"https:\/\/doi.org\/10.6084\/m9.figshare.25119566.v3\" target=\"_blank\" rel=\"noreferrer noopener\">(Bast\u00edas-Curivil et al. 2024)<\/a><sup>2<\/sup>. Es as\u00ed como muchos casos de tornados hist\u00f3ricos en Chile, como el de Concepci\u00f3n en 1934, San Carlos en 1981, Villarrica 2011 y el reciente enjambre de tornados de 2019 en que los tornados de Concepci\u00f3n y Los \u00c1ngeles fueron los m\u00e1s recordados, ocurrieron en esa ventana de tiempo de cerca de 4 semanas que podr\u00edamos denominar la \u201ctemporada de tornados\u201d en el Sur de Chile. <\/p>\n\n\n\n<p>En b\u00fasqueda de una explicaci\u00f3n a este comportamiento es que se calcul\u00f3 primordialmente el par\u00e1metro generador de vorticidad o VGP (por sus siglas en Ingl\u00e9s) que combina el efecto del cizalle en el primer kil\u00f3metro sobre la superficie y la energ\u00eda potencial convectiva disponible (CAPE) de la columna atmosf\u00e9rica. Este \u00edndice a diferencia de otros, est\u00e1 \u00edntimamente relacionado a la f\u00edsica de la formaci\u00f3n de tormentas supercelulares pues escala proporcionalmente al t\u00e9rmino de inclinaci\u00f3n en la ecuaci\u00f3n de vorticidad \u2014y de ah\u00ed su nombre de \u201cgenerador de vorticidad\u201d\u2014. Usando datos de CAPE y cizalle calculados con rean\u00e1lisis ERA-5 durante un periodo desde 1959 a 2021 se pudo reproducir con mucha fidelidad el comportamiento de las observaciones, encontr\u00e1ndose un ciclo estacional en este par\u00e1metro con valores m\u00e1ximos durante la 1era quincena de Junio (CAPE tiene un m\u00e1ximo a fines de Mayo y el cizalle por otro lado a fines de Junio en la zona de mayor frecuencia de tornados).\u00a0<\/p>\n\n\n\n<blockquote class=\"wp-block-quote is-layout-flow wp-block-quote-is-layout-flow\">\n<p>Una observaci\u00f3n muy curiosa es que en \u00e1reas del Sur de Chile en donde los tornados no han sido observados, los valores de VGP, cizalle y otros par\u00e1metros como la helicidad relativa a la tormenta, muestran valores suficientemente altos y que son indicativos de la posibilidad de tornados con una estacionalidad m\u00e1s \u201cplana\u201d respecto de la encontrada en la zona centro-sur de Chile. <\/p>\n<\/blockquote>\n\n\n\n<p>Nuestro an\u00e1lisis otorga confianza al uso del par\u00e1metro de generaci\u00f3n de vorticidad como un \u201cproxy\u201d de la formaci\u00f3n de tormentas severas y torn\u00e1dicas en Chile centro-sur de Chile y abre la posibilidad de encontrar estas tormentas torn\u00e1dicas en zonas mayormente despobladas de la zona austral de Sudam\u00e9rica.\u00a0<\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><img fetchpriority=\"high\" decoding=\"async\" width=\"821\" height=\"1024\" src=\"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2025\/01\/unnamed-2-821x1024.png\" alt=\"Imagen Infrarroja del sat\u00e9lite GOES-16 durante el d\u00eda 30 de Mayo de 2019.\" class=\"wp-image-4365\" srcset=\"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2025\/01\/unnamed-2-821x1024.png 821w, https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2025\/01\/unnamed-2-241x300.png 241w, https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2025\/01\/unnamed-2-768x957.png 768w, https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2025\/01\/unnamed-2.png 1022w\" sizes=\"(max-width: 821px) 100vw, 821px\" \/><figcaption class=\"wp-element-caption\">Imagen Infrarroja del sat\u00e9lite GOES-16 durante el d\u00eda 30 de Mayo de 2019. <\/figcaption><\/figure>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p>*Departament of Geophysics, Universidad de Chile, Santiago, Chile. Center for Climate and Resilience Research, Santiago, Chile.<\/p>\n\n\n\n<hr class=\"wp-block-separator has-alpha-channel-opacity\"\/>\n\n\n\n<p><sup>1<\/sup> Caballero\u2010Mor\u00e1n, V., and Rondanelli, R. (2025). Tornado Seasonality in Central\u2010Southern Chile. Geophysical Research Letters 52, e2024GL110900.\u00a0<a href=\"https:\/\/doi.org\/10.1029\/2024GL110900\" target=\"_blank\" rel=\"noreferrer noopener\">https:\/\/doi.org\/10.1029\/2024GL110900<\/a><br><sup>2<\/sup> Bast\u00edas-Curivil, Cristian; Rondanelli, Roberto; Vicencio, Jose; Matus, Felipe; Caballero, Victoria; Munoz, Francisca; et al. (2024). Tornadoes and Waterspouts in Chile \/ Tornados y Trombas en Chile. figshare. Dataset. <a href=\"https:\/\/doi.org\/10.6084\/m9.figshare.25119566.v3\">https:\/\/doi.org\/10.6084\/m9.figshare.25119566.v3<\/a><\/p>\n\n\n\n<p><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Por Roberto Rondanelli*\/ En Caballero-Mor\u00e1n y Rondanelli\u00a0(2025)1\u00a0estudiamos la estacionalidad de los tornados en Chile Centro-Sur. Tempranamente en el estudio de los tornados, nos llam\u00f3 la atenci\u00f3n el hecho que los tornados parecen ocurrir mayormente\u00a0 desde mediados de Mayo a mediados de Junio con mucha regularidad, a lo largo de las observaciones de tornados disponibles desde [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"ocean_post_layout":"","ocean_both_sidebars_style":"","ocean_both_sidebars_content_width":0,"ocean_both_sidebars_sidebars_width":0,"ocean_sidebar":"","ocean_second_sidebar":"","ocean_disable_margins":"enable","ocean_add_body_class":"","ocean_shortcode_before_top_bar":"","ocean_shortcode_after_top_bar":"","ocean_shortcode_before_header":"","ocean_shortcode_after_header":"","ocean_has_shortcode":"","ocean_shortcode_after_title":"","ocean_shortcode_before_footer_widgets":"","ocean_shortcode_after_footer_widgets":"","ocean_shortcode_before_footer_bottom":"","ocean_shortcode_after_footer_bottom":"","ocean_display_top_bar":"default","ocean_display_header":"default","ocean_header_style":"","ocean_center_header_left_menu":"","ocean_custom_header_template":"","ocean_custom_logo":0,"ocean_custom_retina_logo":0,"ocean_custom_logo_max_width":0,"ocean_custom_logo_tablet_max_width":0,"ocean_custom_logo_mobile_max_width":0,"ocean_custom_logo_max_height":0,"ocean_custom_logo_tablet_max_height":0,"ocean_custom_logo_mobile_max_height":0,"ocean_header_custom_menu":"","ocean_menu_typo_font_family":"","ocean_menu_typo_font_subset":"","ocean_menu_typo_font_size":0,"ocean_menu_typo_font_size_tablet":0,"ocean_menu_typo_font_size_mobile":0,"ocean_menu_typo_font_size_unit":"px","ocean_menu_typo_font_weight":"","ocean_menu_typo_font_weight_tablet":"","ocean_menu_typo_font_weight_mobile":"","ocean_menu_typo_transform":"","ocean_menu_typo_transform_tablet":"","ocean_menu_typo_transform_mobile":"","ocean_menu_typo_line_height":0,"ocean_menu_typo_line_height_tablet":0,"ocean_menu_typo_line_height_mobile":0,"ocean_menu_typo_line_height_unit":"","ocean_menu_typo_spacing":0,"ocean_menu_typo_spacing_tablet":0,"ocean_menu_typo_spacing_mobile":0,"ocean_menu_typo_spacing_unit":"","ocean_menu_link_color":"","ocean_menu_link_color_hover":"","ocean_menu_link_color_active":"","ocean_menu_link_background":"","ocean_menu_link_hover_background":"","ocean_menu_link_active_background":"","ocean_menu_social_links_bg":"","ocean_menu_social_hover_links_bg":"","ocean_menu_social_links_color":"","ocean_menu_social_hover_links_color":"","ocean_disable_title":"default","ocean_disable_heading":"default","ocean_post_title":"","ocean_post_subheading":"","ocean_post_title_style":"","ocean_post_title_background_color":"","ocean_post_title_background":0,"ocean_post_title_bg_image_position":"","ocean_post_title_bg_image_attachment":"","ocean_post_title_bg_image_repeat":"","ocean_post_title_bg_image_size":"","ocean_post_title_height":0,"ocean_post_title_bg_overlay":0.5,"ocean_post_title_bg_overlay_color":"","ocean_disable_breadcrumbs":"default","ocean_breadcrumbs_color":"","ocean_breadcrumbs_separator_color":"","ocean_breadcrumbs_links_color":"","ocean_breadcrumbs_links_hover_color":"","ocean_display_footer_widgets":"default","ocean_display_footer_bottom":"default","ocean_custom_footer_template":"","ocean_post_oembed":"","ocean_post_self_hosted_media":"","ocean_post_video_embed":"","ocean_link_format":"","ocean_link_format_target":"self","ocean_quote_format":"","ocean_quote_format_link":"post","ocean_gallery_link_images":"on","ocean_gallery_id":[],"footnotes":""},"categories":[16],"tags":[37,87,88,86],"class_list":["post-4363","post","type-post","status-publish","format-standard","hentry","category-lecturas","tag-chile","tag-estacionalidad","tag-tormentas","tag-tornados","entry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v26.8 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Estacionalidad de los tornados en el centro-sur de Chile - Programa Hidroclim\u00e1tico Regional para los Andes<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.andex-rhp.org\/?p=4363\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Estacionalidad de los tornados en el centro-sur de Chile - Programa Hidroclim\u00e1tico Regional para los Andes\" \/>\n<meta property=\"og:description\" content=\"Por Roberto Rondanelli*\/ En Caballero-Mor\u00e1n y Rondanelli\u00a0(2025)1\u00a0estudiamos la estacionalidad de los tornados en Chile Centro-Sur. Tempranamente en el estudio de los tornados, nos llam\u00f3 la atenci\u00f3n el hecho que los tornados parecen ocurrir mayormente\u00a0 desde mediados de Mayo a mediados de Junio con mucha regularidad, a lo largo de las observaciones de tornados disponibles desde [&hellip;]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/www.andex-rhp.org\/?p=4363\" \/>\n<meta property=\"og:site_name\" content=\"Programa Hidroclim\u00e1tico Regional para los Andes\" \/>\n<meta property=\"article:published_time\" content=\"2025-01-17T16:42:49+00:00\" \/>\n<meta property=\"article:modified_time\" content=\"2025-01-17T16:42:50+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2025\/01\/unnamed-2.png\" \/>\n\t<meta property=\"og:image:width\" content=\"1022\" \/>\n\t<meta property=\"og:image:height\" content=\"1274\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/png\" \/>\n<meta name=\"author\" content=\"andex\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Written by\" \/>\n\t<meta name=\"twitter:data1\" content=\"andex\" \/>\n\t<meta name=\"twitter:label2\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data2\" content=\"3 minutes\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\/\/schema.org\",\"@graph\":[{\"@type\":\"Article\",\"@id\":\"https:\/\/www.andex-rhp.org\/?p=4363#article\",\"isPartOf\":{\"@id\":\"https:\/\/www.andex-rhp.org\/?p=4363\"},\"author\":{\"name\":\"andex\",\"@id\":\"https:\/\/www.andex-rhp.org\/#\/schema\/person\/502e4f38fe30f00d8b101cd988a956fb\"},\"headline\":\"Estacionalidad de los tornados en el centro-sur de Chile\",\"datePublished\":\"2025-01-17T16:42:49+00:00\",\"dateModified\":\"2025-01-17T16:42:50+00:00\",\"mainEntityOfPage\":{\"@id\":\"https:\/\/www.andex-rhp.org\/?p=4363\"},\"wordCount\":517,\"commentCount\":0,\"publisher\":{\"@id\":\"https:\/\/www.andex-rhp.org\/#organization\"},\"image\":{\"@id\":\"https:\/\/www.andex-rhp.org\/?p=4363#primaryimage\"},\"thumbnailUrl\":\"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2025\/01\/unnamed-2-821x1024.png\",\"keywords\":[\"Chile\",\"Estacionalidad\",\"Tormentas\",\"Tornados\"],\"articleSection\":[\"Lecturas\"],\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"CommentAction\",\"name\":\"Comment\",\"target\":[\"https:\/\/www.andex-rhp.org\/?p=4363#respond\"]}]},{\"@type\":\"WebPage\",\"@id\":\"https:\/\/www.andex-rhp.org\/?p=4363\",\"url\":\"https:\/\/www.andex-rhp.org\/?p=4363\",\"name\":\"Estacionalidad de los tornados en el centro-sur de Chile - Programa Hidroclim\u00e1tico Regional para los Andes\",\"isPartOf\":{\"@id\":\"https:\/\/www.andex-rhp.org\/#website\"},\"primaryImageOfPage\":{\"@id\":\"https:\/\/www.andex-rhp.org\/?p=4363#primaryimage\"},\"image\":{\"@id\":\"https:\/\/www.andex-rhp.org\/?p=4363#primaryimage\"},\"thumbnailUrl\":\"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2025\/01\/unnamed-2-821x1024.png\",\"datePublished\":\"2025-01-17T16:42:49+00:00\",\"dateModified\":\"2025-01-17T16:42:50+00:00\",\"breadcrumb\":{\"@id\":\"https:\/\/www.andex-rhp.org\/?p=4363#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\/\/www.andex-rhp.org\/?p=4363\"]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"https:\/\/www.andex-rhp.org\/?p=4363#primaryimage\",\"url\":\"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2025\/01\/unnamed-2.png\",\"contentUrl\":\"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2025\/01\/unnamed-2.png\",\"width\":1022,\"height\":1274,\"caption\":\"Imagen Infrarroja del sat\u00e9lite GOES-16 durante el d\u00eda 30 de Mayo de 2019.\"},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\/\/www.andex-rhp.org\/?p=4363#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"https:\/\/www.andex-rhp.org\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"Estacionalidad de los tornados en el centro-sur de Chile\"}]},{\"@type\":\"WebSite\",\"@id\":\"https:\/\/www.andex-rhp.org\/#website\",\"url\":\"https:\/\/www.andex-rhp.org\/\",\"name\":\"Programa Hidroclim\u00e1tico Regional para los Andes\",\"description\":\"ANDEX\",\"publisher\":{\"@id\":\"https:\/\/www.andex-rhp.org\/#organization\"},\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"https:\/\/www.andex-rhp.org\/?s={search_term_string}\"},\"query-input\":{\"@type\":\"PropertyValueSpecification\",\"valueRequired\":true,\"valueName\":\"search_term_string\"}}],\"inLanguage\":\"en-US\"},{\"@type\":\"Organization\",\"@id\":\"https:\/\/www.andex-rhp.org\/#organization\",\"name\":\"Programa Hidroclim\u00e1tico Regional para los Andes\",\"url\":\"https:\/\/www.andex-rhp.org\/\",\"logo\":{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"https:\/\/www.andex-rhp.org\/#\/schema\/logo\/image\/\",\"url\":\"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2024\/04\/cropped-cropped-logo_ANDEX_color_trans1.png\",\"contentUrl\":\"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2024\/04\/cropped-cropped-logo_ANDEX_color_trans1.png\",\"width\":555,\"height\":444,\"caption\":\"Programa Hidroclim\u00e1tico Regional para los Andes\"},\"image\":{\"@id\":\"https:\/\/www.andex-rhp.org\/#\/schema\/logo\/image\/\"}},{\"@type\":\"Person\",\"@id\":\"https:\/\/www.andex-rhp.org\/#\/schema\/person\/502e4f38fe30f00d8b101cd988a956fb\",\"name\":\"andex\",\"image\":{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"https:\/\/www.andex-rhp.org\/#\/schema\/person\/image\/\",\"url\":\"https:\/\/secure.gravatar.com\/avatar\/23494ed4720f39176481de38bcdec2a13011e1321adeb3faa91d0e623a2a8587?s=96&d=mm&r=g\",\"contentUrl\":\"https:\/\/secure.gravatar.com\/avatar\/23494ed4720f39176481de38bcdec2a13011e1321adeb3faa91d0e623a2a8587?s=96&d=mm&r=g\",\"caption\":\"andex\"},\"url\":\"https:\/\/www.andex-rhp.org\/?author=2\"}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"Estacionalidad de los tornados en el centro-sur de Chile - Programa Hidroclim\u00e1tico Regional para los Andes","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/www.andex-rhp.org\/?p=4363","og_locale":"en_US","og_type":"article","og_title":"Estacionalidad de los tornados en el centro-sur de Chile - Programa Hidroclim\u00e1tico Regional para los Andes","og_description":"Por Roberto Rondanelli*\/ En Caballero-Mor\u00e1n y Rondanelli\u00a0(2025)1\u00a0estudiamos la estacionalidad de los tornados en Chile Centro-Sur. Tempranamente en el estudio de los tornados, nos llam\u00f3 la atenci\u00f3n el hecho que los tornados parecen ocurrir mayormente\u00a0 desde mediados de Mayo a mediados de Junio con mucha regularidad, a lo largo de las observaciones de tornados disponibles desde [&hellip;]","og_url":"https:\/\/www.andex-rhp.org\/?p=4363","og_site_name":"Programa Hidroclim\u00e1tico Regional para los Andes","article_published_time":"2025-01-17T16:42:49+00:00","article_modified_time":"2025-01-17T16:42:50+00:00","og_image":[{"width":1022,"height":1274,"url":"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2025\/01\/unnamed-2.png","type":"image\/png"}],"author":"andex","twitter_card":"summary_large_image","twitter_misc":{"Written by":"andex","Est. reading time":"3 minutes"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"Article","@id":"https:\/\/www.andex-rhp.org\/?p=4363#article","isPartOf":{"@id":"https:\/\/www.andex-rhp.org\/?p=4363"},"author":{"name":"andex","@id":"https:\/\/www.andex-rhp.org\/#\/schema\/person\/502e4f38fe30f00d8b101cd988a956fb"},"headline":"Estacionalidad de los tornados en el centro-sur de Chile","datePublished":"2025-01-17T16:42:49+00:00","dateModified":"2025-01-17T16:42:50+00:00","mainEntityOfPage":{"@id":"https:\/\/www.andex-rhp.org\/?p=4363"},"wordCount":517,"commentCount":0,"publisher":{"@id":"https:\/\/www.andex-rhp.org\/#organization"},"image":{"@id":"https:\/\/www.andex-rhp.org\/?p=4363#primaryimage"},"thumbnailUrl":"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2025\/01\/unnamed-2-821x1024.png","keywords":["Chile","Estacionalidad","Tormentas","Tornados"],"articleSection":["Lecturas"],"inLanguage":"en-US","potentialAction":[{"@type":"CommentAction","name":"Comment","target":["https:\/\/www.andex-rhp.org\/?p=4363#respond"]}]},{"@type":"WebPage","@id":"https:\/\/www.andex-rhp.org\/?p=4363","url":"https:\/\/www.andex-rhp.org\/?p=4363","name":"Estacionalidad de los tornados en el centro-sur de Chile - Programa Hidroclim\u00e1tico Regional para los Andes","isPartOf":{"@id":"https:\/\/www.andex-rhp.org\/#website"},"primaryImageOfPage":{"@id":"https:\/\/www.andex-rhp.org\/?p=4363#primaryimage"},"image":{"@id":"https:\/\/www.andex-rhp.org\/?p=4363#primaryimage"},"thumbnailUrl":"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2025\/01\/unnamed-2-821x1024.png","datePublished":"2025-01-17T16:42:49+00:00","dateModified":"2025-01-17T16:42:50+00:00","breadcrumb":{"@id":"https:\/\/www.andex-rhp.org\/?p=4363#breadcrumb"},"inLanguage":"en-US","potentialAction":[{"@type":"ReadAction","target":["https:\/\/www.andex-rhp.org\/?p=4363"]}]},{"@type":"ImageObject","inLanguage":"en-US","@id":"https:\/\/www.andex-rhp.org\/?p=4363#primaryimage","url":"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2025\/01\/unnamed-2.png","contentUrl":"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2025\/01\/unnamed-2.png","width":1022,"height":1274,"caption":"Imagen Infrarroja del sat\u00e9lite GOES-16 durante el d\u00eda 30 de Mayo de 2019."},{"@type":"BreadcrumbList","@id":"https:\/\/www.andex-rhp.org\/?p=4363#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Home","item":"https:\/\/www.andex-rhp.org\/"},{"@type":"ListItem","position":2,"name":"Estacionalidad de los tornados en el centro-sur de Chile"}]},{"@type":"WebSite","@id":"https:\/\/www.andex-rhp.org\/#website","url":"https:\/\/www.andex-rhp.org\/","name":"Programa Hidroclim\u00e1tico Regional para los Andes","description":"ANDEX","publisher":{"@id":"https:\/\/www.andex-rhp.org\/#organization"},"potentialAction":[{"@type":"SearchAction","target":{"@type":"EntryPoint","urlTemplate":"https:\/\/www.andex-rhp.org\/?s={search_term_string}"},"query-input":{"@type":"PropertyValueSpecification","valueRequired":true,"valueName":"search_term_string"}}],"inLanguage":"en-US"},{"@type":"Organization","@id":"https:\/\/www.andex-rhp.org\/#organization","name":"Programa Hidroclim\u00e1tico Regional para los Andes","url":"https:\/\/www.andex-rhp.org\/","logo":{"@type":"ImageObject","inLanguage":"en-US","@id":"https:\/\/www.andex-rhp.org\/#\/schema\/logo\/image\/","url":"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2024\/04\/cropped-cropped-logo_ANDEX_color_trans1.png","contentUrl":"https:\/\/www.andex-rhp.org\/wp-content\/uploads\/2024\/04\/cropped-cropped-logo_ANDEX_color_trans1.png","width":555,"height":444,"caption":"Programa Hidroclim\u00e1tico Regional para los Andes"},"image":{"@id":"https:\/\/www.andex-rhp.org\/#\/schema\/logo\/image\/"}},{"@type":"Person","@id":"https:\/\/www.andex-rhp.org\/#\/schema\/person\/502e4f38fe30f00d8b101cd988a956fb","name":"andex","image":{"@type":"ImageObject","inLanguage":"en-US","@id":"https:\/\/www.andex-rhp.org\/#\/schema\/person\/image\/","url":"https:\/\/secure.gravatar.com\/avatar\/23494ed4720f39176481de38bcdec2a13011e1321adeb3faa91d0e623a2a8587?s=96&d=mm&r=g","contentUrl":"https:\/\/secure.gravatar.com\/avatar\/23494ed4720f39176481de38bcdec2a13011e1321adeb3faa91d0e623a2a8587?s=96&d=mm&r=g","caption":"andex"},"url":"https:\/\/www.andex-rhp.org\/?author=2"}]}},"_links":{"self":[{"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=\/wp\/v2\/posts\/4363","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=4363"}],"version-history":[{"count":3,"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=\/wp\/v2\/posts\/4363\/revisions"}],"predecessor-version":[{"id":4367,"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=\/wp\/v2\/posts\/4363\/revisions\/4367"}],"wp:attachment":[{"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=4363"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=4363"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.andex-rhp.org\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=4363"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}