{"id":606,"date":"2022-09-01T11:47:24","date_gmt":"2022-09-01T11:47:24","guid":{"rendered":"https:\/\/theclimatebook.org\/notas-finales\/segunda-parte-como-esta-cambiando-nuestro-planeta\/2-23-el-permafrost\/"},"modified":"2022-11-01T13:01:18","modified_gmt":"2022-11-01T13:01:18","slug":"2-23-el-permafrost","status":"publish","type":"page","link":"https:\/\/theclimatebook.org\/es\/notas-finales\/segunda-parte-como-esta-cambiando-nuestro-planeta\/2-23-el-permafrost\/","title":{"rendered":"2.23 El permafrost"},"content":{"rendered":"<div class=\"notes\">\n<p class=\"author\"><a href=\"\/contributors#\u00f6rjan-gustafsson\" rel=\"author\">\u00d6rjan Gustafsson<\/a><\/p>\n<p class=\"date\">Todas las fuentes en l\u00ednea se consultaron el <time datetime=\"2022-03-01\">1 de marzo de 2022<\/time><\/p>\n<ol start=\"114\">\n<li>\n<p>\n<q>del 75 por ciento de los hidratos del planeta situados a baja profundidad<\/q> Shakhova, N., et al., <cite>\u2018Understanding the permafrost\u2013hydrate system and associated methane releases in the east Siberian Arctic shelf\u2019<\/cite>, <span class=\"book\">Geosciences<\/span>, 9 (6), 2019: art\u00edculo 251, <a href=\"https:\/\/doi.org\/10.3390\/geosciences9060251\" target=\"_blank\" rel=\"noopener\">https:\/\/doi.org\/10.3390\/geosciences9060251<\/a>.\n<\/p>\n<\/li>\n<li>\n<p>\n<q>diez veces m\u00e1s r\u00e1pido en la meseta del T\u00edbet<\/q> Gao, T., et al., <cite>\u2018Accelerating permafrost collapse on the eastern Tibetan Plateau\u2019<\/cite>, <span class=\"book\">Environmental Research Letters<\/span>, 16 (5), 2021: art\u00edculo 054023, <a href=\"https:\/\/doi.org\/10.1088\/1748-9326\/abf7f0\" target=\"_blank\" rel=\"noopener\">https:\/\/doi.org\/10.1088\/1748-9326\/abf7f0https:\/\/doi.org\/10.1088\/1748-9326\/abf7f0<\/a>.\n<\/p>\n<p>\n<q>calentado unos 10\u00b0C debido al agua de mar suprayacente<\/q> Shakhova, N., et al., <cite>\u2018Current rates and mechanisms of subsea permafrost degradation in the east Siberian Arctic shelf\u2019<\/cite>, <span class=\"book\">Nature Communications<\/span>, 8, 2017: art\u00edculo 15872, <a href=\"https:\/\/doi.org\/10.1038\/ncomms15872\" target=\"_blank\" rel=\"noopener\">https:\/\/doi.org\/10.1038\/ncomms15872<\/a>.\n<\/p>\n<\/li>\n<li>\n<p>\n<q>tambi\u00e9n hemos sido testigos del burbujeo de metano<\/q> Shakhova, N., et al., <cite>\u2018Extensive methane venting to the atmosphere from sediments of the east Siberian Arctic shelf\u2019<\/cite>, <span class=\"book\">Science<\/span>, 327 (5970), 2010: 1246\u201350, <a href=\"https:\/\/doi.org\/10.1126\/science.1182221\" target=\"_blank\" rel=\"noopener\">https:\/\/doi.org\/10.1126\/science.1182221<\/a>; Steinbach, J., et al., <cite>\u2018Source apportionment of methane escaping the subsea permafrost system in the outer Eurasian Arctic shelf\u2019<\/cite>, <span class=\"book\">Proceedings of the National Academy of Sciences<\/span>, 118 (10), 2021: art\u00edculo e2019672118, <a href=\"https:\/\/doi.org\/10.1073\/pnas.2019672118\" target=\"_blank\" rel=\"noopener\">https:\/\/doi.org\/10.1073\/pnas.2019672118<\/a>.\n<\/p>\n<\/li>\n<\/ol>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>\u00d6rjan Gustafsson Todas las fuentes en l\u00ednea se consultaron el 1 de marzo de 2022 del 75 por ciento de los hidratos del planeta situados a baja profundidad Shakhova, N., et al., \u2018Understanding the permafrost\u2013hydrate system and associated methane releases in the east Siberian Arctic shelf\u2019, Geosciences, 9 (6), 2019: art\u00edculo 251, https:\/\/doi.org\/10.3390\/geosciences9060251. diez veces&hellip;<\/p>\n","protected":false},"author":5,"featured_media":0,"parent":588,"menu_order":23,"comment_status":"closed","ping_status":"closed","template":"page-essay.php","meta":{"footnotes":""},"class_list":["post-606","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/theclimatebook.org\/es\/wp-json\/wp\/v2\/pages\/606","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/theclimatebook.org\/es\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/theclimatebook.org\/es\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/theclimatebook.org\/es\/wp-json\/wp\/v2\/users\/5"}],"replies":[{"embeddable":true,"href":"https:\/\/theclimatebook.org\/es\/wp-json\/wp\/v2\/comments?post=606"}],"version-history":[{"count":0,"href":"https:\/\/theclimatebook.org\/es\/wp-json\/wp\/v2\/pages\/606\/revisions"}],"up":[{"embeddable":true,"href":"https:\/\/theclimatebook.org\/es\/wp-json\/wp\/v2\/pages\/588"}],"wp:attachment":[{"href":"https:\/\/theclimatebook.org\/es\/wp-json\/wp\/v2\/media?parent=606"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}