{"id":4735,"date":"2023-01-26T08:47:52","date_gmt":"2023-01-26T08:47:52","guid":{"rendered":"https:\/\/proespacio.tedae.org\/?p=4735"},"modified":"2023-12-20T13:15:12","modified_gmt":"2023-12-20T13:15:12","slug":"regiones-polares","status":"publish","type":"post","link":"https:\/\/proespacio.tedae.org\/en\/regiones-polares\/","title":{"rendered":"Polar Regions"},"content":{"rendered":"<div data-elementor-type=\"wp-post\" data-elementor-id=\"4735\" class=\"elementor elementor-4735\" data-elementor-post-type=\"post\">\n\t\t\t\t\t\t<section class=\"has-el-gap el-gap-default elementor-section elementor-top-section elementor-element elementor-element-edfcdfb elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"edfcdfb\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-no\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-f88156f\" data-id=\"f88156f\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-1e0a991 elementor-widget elementor-widget-text-editor\" data-id=\"1e0a991\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\tPolar Regions are of paramount importance in the balance of global climate. Due to its geographic isolation, difficult access and large surface, Earth Observation satellites are particularly well-suited to study and monitor its environmental parameters. Among these parameters, the changes in the depth and area of polar ice are crucial to understand the phenomena associated with climate change, given its influence in Earth\u2019s temperature regulation, ocean currents and sea level fluctuations.\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-df2a8e7 elementor-widget elementor-widget-text-editor\" data-id=\"df2a8e7\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\tThe efforts to comply with international agreements to limit the rise of global temperature are essential in maintaining the conditions in the Poles, and therefore, to control the effects of climate change.\nIn line with this, the progressive restoration of the ozone layer shows what agreements like these can accomplish when implemented at a global scale. ESA has been monitoring the ozone layer for over twenty years, and current forecasts point to its complete recovery in the next few decades, ending in the recovery of the Polar Regions by 2060.\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-6963b69 elementor-widget elementor-widget-text-editor\" data-id=\"6963b69\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p><strong>About the image<\/strong><\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-9d783fb elementor-widget elementor-widget-text-editor\" data-id=\"9d783fb\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\tOzone Hole over the Southern Pole (2021)\nThe map is centered on the Antarctic region. Areas in yellow, orange and red\nrepresent high ozone values, while areas in green and blue show low values\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-f1d24e7 elementor-widget elementor-widget-spacer\" data-id=\"f1d24e7\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<div class=\"elementor-spacer\">\n\t\t\t<div class=\"elementor-spacer-inner\"><\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-03339eb elementor-widget elementor-widget-text-editor\" data-id=\"03339eb\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<h5><strong>Antarctic ice speed<\/strong><\/h5>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-b2ffce1 elementor-widget elementor-widget-text-editor\" data-id=\"b2ffce1\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<figure class=\"wp-block-image alignwide size-large\" style=\"margin-top: 0px; margin-bottom: 0px;\"><img decoding=\"async\" data-recalc-dims=\"1\" class=\"wp-image-651\" src=\"https:\/\/i0.wp.com\/proespacio.tedae.org\/wp-content\/uploads\/2023\/01\/instantes-regiones-polares-v2.jpg?w=788&#038;ssl=1\" alt=\"Instantes\" \/><figcaption>Credits: ESA\/MEaSUREs version 2, 1996\u20132016 (multimission data), NASA, NSIDC\/BAS<\/figcaption><\/figure>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-565b177 elementor-widget elementor-widget-text-editor\" data-id=\"565b177\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p><strong>About the image<\/strong><\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-4d4d4dc elementor-widget elementor-widget-text-editor\" data-id=\"4d4d4dc\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\tThe image shows the different glacier flow speeds toward the ocean between 1996 and 2016. Recent research shows that glaciers in the Getz region (inside the black rectangle) are accelerating their flow toward the sea.\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-14c4a20 elementor-widget elementor-widget-spacer\" data-id=\"14c4a20\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<div class=\"elementor-spacer\">\n\t\t\t<div class=\"elementor-spacer-inner\"><\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-9d0f0d0 elementor-widget elementor-widget-text-editor\" data-id=\"9d0f0d0\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<h5><strong>Permafrost cover in the Northern Hemisphere<\/strong><\/h5>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-b6bdbbe elementor-widget elementor-widget-text-editor\" data-id=\"b6bdbbe\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<figure class=\"wp-block-image alignwide size-large\" style=\"margin-top: 0px; margin-bottom: 0px;\"><img decoding=\"async\" data-recalc-dims=\"1\" class=\"wp-image-651\" src=\"https:\/\/i0.wp.com\/proespacio.tedae.org\/wp-content\/uploads\/2023\/01\/instantes-regiones-polares-v3.jpg?w=788&#038;ssl=1\" alt=\"Instantes\" \/><figcaption>Credit: Permafrost CCI, Obu et al, 2019 via the CEDA archive<\/figcaption><\/figure>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-688ec67 elementor-widget elementor-widget-text-editor\" data-id=\"688ec67\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p><strong>About the image<\/strong><\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-f0445b2 elementor-widget elementor-widget-text-editor\" data-id=\"f0445b2\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\tThe maps generated by the ESA\u2019s Climate Change Initiative offer new information about the melting of permafrost in the northern hemisphere. The image shows the permafrost cover in 2003 compared with 2017.\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-5f48807 elementor-widget elementor-widget-spacer\" data-id=\"5f48807\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"spacer.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<div class=\"elementor-spacer\">\n\t\t\t<div class=\"elementor-spacer-inner\"><\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-750c8a2 elementor-widget elementor-widget-text-editor\" data-id=\"750c8a2\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<h5><strong>Ice in the Arctic Ocean \u201catlantifies\u201d<\/strong><\/h5>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-3625dbb elementor-widget elementor-widget-text-editor\" data-id=\"3625dbb\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<figure class=\"wp-block-image alignwide size-large\" style=\"margin-top: 0px; margin-bottom: 0px;\"><img decoding=\"async\" data-recalc-dims=\"1\" class=\"wp-image-651\" src=\"https:\/\/i0.wp.com\/proespacio.tedae.org\/wp-content\/uploads\/2023\/01\/instantes-regiones-polares-v4.jpg?w=788&#038;ssl=1\" alt=\"Instantes\" \/><figcaption>Credits: ESA\/AWI<\/figcaption><\/figure>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-9ef98d3 elementor-widget elementor-widget-text-editor\" data-id=\"9ef98d3\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p><strong>About the image<\/strong><\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t<div class=\"elementor-element elementor-element-eafa7f5 elementor-widget elementor-widget-text-editor\" data-id=\"eafa7f5\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\tA combined analysis of data from Cryosat and SMOS allows us to compare the width of sea ice in April 2021 with the average for the same month in the years 2011-2020.\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>","protected":false},"excerpt":{"rendered":"<p>Las Regiones Polares tienen una relevancia esencial en el equilibrio del clima global. Debido a sus caracter\u00edsticas de islamiento geogr\u00e1fico, la dificultad de acceso y su gran superficie, los sat\u00e9lites de Observaci\u00f3n de la Tierra son particularmente adecuados para el estudio y la monitorizaci\u00f3n de sus par\u00e1metros medioambientales. Entre estos par\u00e1metros la evoluci\u00f3n del grosor<\/p>","protected":false},"author":1,"featured_media":4741,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_jetpack_memberships_contains_paid_content":false,"footnotes":""},"categories":[32],"tags":[125,43,128,122],"class_list":{"0":"post-4735","1":"post","2":"type-post","3":"status-publish","4":"format-standard","5":"has-post-thumbnail","7":"category-instantes","8":"tag-header-no51","9":"tag-instantes","10":"tag-instantes-no51","11":"tag-no51"},"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.1.1 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Regiones Polares - PROESPACIO<\/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:\/\/proespacio.tedae.org\/en\/regiones-polares\/\" \/>\n<meta property=\"og:locale\" content=\"en_GB\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Regiones Polares - PROESPACIO\" \/>\n<meta property=\"og:description\" content=\"Las Regiones Polares tienen una relevancia esencial en el equilibrio del clima global. Debido a sus caracter\u00edsticas de islamiento geogr\u00e1fico, la dificultad de acceso y su gran superficie, los sat\u00e9lites de Observaci\u00f3n de la Tierra son particularmente adecuados para el estudio y la monitorizaci\u00f3n de sus par\u00e1metros medioambientales. 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