{"id":64462,"date":"2026-10-23T11:23:04","date_gmt":"2026-10-23T11:23:04","guid":{"rendered":"https:\/\/cp.snarskis.lt\/index.php\/2026\/10\/23\/mokslininkai-pervertino-thwaiteso-ledyno-stabiluma-iki-2100-metu-juros-lygis-gali-kilti-sparciau\/"},"modified":"2026-10-23T11:23:04","modified_gmt":"2026-10-23T11:23:04","slug":"mokslininkai-pervertino-thwaiteso-ledyno-stabiluma-iki-2100-metu-juros-lygis-gali-kilti-sparciau","status":"publish","type":"post","link":"https:\/\/cp.snarskis.lt\/index.php\/2026\/10\/23\/mokslininkai-pervertino-thwaiteso-ledyno-stabiluma-iki-2100-metu-juros-lygis-gali-kilti-sparciau\/","title":{"rendered":"Mokslininkai pervertino Thwaiteso ledyno stabilum\u0105: iki 2100 met\u0173 j\u016bros lygis gali kilti spar\u010diau"},"content":{"rendered":"<p>Vakar\u0173 Antarktidoje esantis Thwaiteso ledynas, da\u017enai vadinamas lemtingu klimato rizikos ta\u0161ku, gali tirpti ir trauktis grei\u010diau, nei buvo manyta iki \u0161iol. Nauji modeliavimai rodo, kad jau \u0161iame \u0161imtmetyje jo ind\u0117lis \u012f pasaulin\u012f j\u016bros lygio kilim\u0105 gali b\u016bti ma\u017edaug dvigubai didesnis, palyginti su ankstesniais vertinimais.<\/p>\n<p>Thwaiteso ledynas yra mil\u017eini\u0161ka ledo mas\u0117, savo plotu prilyginama didel\u0117ms valstyb\u0117ms ar regionams. Vien jo visi\u0161kas suirimas ilgainiui gal\u0117t\u0173 reik\u0161mingai prisid\u0117ti prie j\u016bros lygio kilimo, o svarbiausia rizika slypi tame, kad jis gali paleisti grandinin\u0119 reakcij\u0105 Vakar\u0173 Antarktidos ledo skydyne.<\/p>\n<p class=\"article__like-h2\">Kod\u0117l prognoz\u0117s blog\u0117ja<\/p>\n<p>Ledyn\u0173 elgsena priklauso ne tik nuo oro temperat\u016bros, bet ir nuo to, kas vyksta ties riba, kur ledas remiasi \u012f sausum\u0105 ir pereina \u012f pl\u016bduriuojant\u012f ledo \u0161elf\u0105. Naujesni skai\u010diavimai pabr\u0117\u017eia, kad \u0161i riba n\u0117ra siaura linija, o keli\u0173 kilometr\u0173 plo\u010dio pereinamoji zona, kurioje procesai gali b\u016bti gerokai dinami\u0161kesni.<\/p>\n<p>\u0160iose zonose santykinai \u0161iltesnis vandenyno vanduo gali lengviau patekti po ledu ir j\u012f ardyti i\u0161 apa\u010dios. Be to, potvyni\u0173 ir atosl\u016bgi\u0173 ciklai gali periodi\u0161kai pakelti ledo pakra\u0161\u010dius, ma\u017eindami sukibim\u0105 su dugnu ir didindami nestabilum\u0105.<\/p>\n<p class=\"article__like-h2\">Kas gali \u012fvykti iki 2100 met\u0173<\/p>\n<p>Tyr\u0117jai atkreipia d\u0117mes\u012f, kad Thwaiteso ledyno stabilum\u0105 \u0161iuo metu dar gali palaikyti povandenin\u0117s reljefo strukt\u016bros, veikian\u010dios tarsi \u201eatrama\u201c. Ta\u010diau jei \u0161iltesnis vanduo ir toliau skverbsis \u012f pereinam\u0105sias zonas, ledynas gali silpninti ry\u0161\u012f su \u0161ia atrama ir tapti jautresnis staigiems poky\u010diams.<\/p>\n<p>Pagal naujus vertinimus, iki 2100 met\u0173 Thwaiteso ind\u0117lis \u012f vidutin\u012f pasaulin\u012f j\u016bros lygio kilim\u0105 gali siekti apie 30 milimetr\u0173, su ma\u017edaug 6 milimetr\u0173 paklaida. Tai yra ma\u017edaug dvigubai daugiau, nei rod\u0117 dalis ankstesni\u0173 skai\u010diavim\u0173, o svarbiausia tai, kad \u0161is procesas didina ir platesn\u0117s Vakar\u0173 Antarktidos destabilizacijos rizik\u0105.<\/p>\n<p class=\"article__like-h2\">K\u0105 tai rei\u0161kia pakran\u010di\u0173 miestams<\/p>\n<p>Nors keli centimetrai i\u0161 pirmo \u017evilgsnio gali atrodyti nedaug, pasauliniu mastu net ir toks papildomas j\u016bros lygio kilimas rei\u0161kia da\u017enesnius pakran\u010di\u0173 potvynius, spartesn\u0119 krant\u0173 erozij\u0105 ir didesn\u012f s\u016bri\u0173 vanden\u0173 prasiskverbim\u0105 \u012f g\u0117lo vandens i\u0161teklius. Did\u017eiausi\u0105 poveik\u012f paprastai pajunta \u017eemose pakrant\u0117se esantys miestai, salos ir deltos.<\/p>\n<p>Mokslininkai pabr\u0117\u017eia, kad ledo skydyn\u0173 reakcija n\u0117ra momentin\u0117, ta\u010diau kai kurie poky\u010diai gali tapti sunkiai sustabdomi. \u0160iltnamio efekt\u0105 sukelian\u010di\u0173 duj\u0173 emisij\u0173 ma\u017einimas, pasak j\u0173, vis dar gali sul\u0117tinti proces\u0173 temp\u0105 ir suma\u017einti ilgalaik\u0119 rizik\u0105.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Nauji tyrimai rodo, kad Thwaiteso ledynas Vakar\u0173 Antarktidoje gali kelti didesn\u0119 gr\u0117sm\u0119: iki 2100 met\u0173 j\u016bros lygis gali kilti spar\u010diau.<\/p>\n","protected":false},"author":0,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[7],"tags":[4540,101,22190,673,4806,47564,11925],"miestas":[],"class_list":["post-64462","post","type-post","status-publish","format-standard","hentry","category-technologijos","tag-antarktida","tag-ekologija","tag-juros-lygio-kilimas","tag-klimato-kaita","tag-ledynu-tirpimas","tag-thwaiteso-ledynas","tag-vandenynai"],"acf":[],"_links":{"self":[{"href":"https:\/\/cp.snarskis.lt\/index.php\/wp-json\/wp\/v2\/posts\/64462","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/cp.snarskis.lt\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/cp.snarskis.lt\/index.php\/wp-json\/wp\/v2\/types\/post"}],"replies":[{"embeddable":true,"href":"https:\/\/cp.snarskis.lt\/index.php\/wp-json\/wp\/v2\/comments?post=64462"}],"version-history":[{"count":0,"href":"https:\/\/cp.snarskis.lt\/index.php\/wp-json\/wp\/v2\/posts\/64462\/revisions"}],"wp:attachment":[{"href":"https:\/\/cp.snarskis.lt\/index.php\/wp-json\/wp\/v2\/media?parent=64462"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cp.snarskis.lt\/index.php\/wp-json\/wp\/v2\/categories?post=64462"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cp.snarskis.lt\/index.php\/wp-json\/wp\/v2\/tags?post=64462"},{"taxonomy":"miestas","embeddable":true,"href":"https:\/\/cp.snarskis.lt\/index.php\/wp-json\/wp\/v2\/miestas?post=64462"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}