. . "\u601D\u97CB\u8328\u51B0\u5DDD\uFF08\u82F1\u8A9E\uFF1AThwaites Glacier\uFF09\u662F\u5357\u6975\u6D32\u7684\u51B0\u5DDD\uFF0C\u4F4D\u65BC\u746A\u9E97\u4F2F\u5FB7\u5730\u7684\u6C83\u723E\u683C\u6797\u6D77\u5CB8\uFF0C\u6700\u7D42\u6CE8\u5165\u963F\u8499\u68EE\u6D77\uFF0C\u4EE5\u5A01\u65AF\u5EB7\u8F9B\u5927\u5B78\u9EA5\u8FEA\u905C\u5206\u6821\u7684\u5730\u8CEA\u5B78\u5BB6\u547D\u540D\uFF0C\u73FE\u6642\u7531\u5357\u6975\u689D\u7D04\u9AD4\u7CFB\u7BA1\u7406\u3002\u898F\u6A21\u5B8F\u5927\uFF0C\u800C\u5728\u5168\u7403\u6696\u5316\u5E95\u4E0B\uFF0C\u88AB\u8A8D\u70BA\u53EF\u80FD\u5C0D\u6D77\u5E73\u9762\u4E0A\u5347\u5E36\u4F86\u91CD\u5927\u5F71\u97FF\uFF0C\u6545\u53C8\u88AB\u7A31\u70BA\u672B\u65E5\u51B0\u5DDD \uFF08\u82F1\u8A9E\uFF1ADoomsday Glacier\uFF09\u3002"@zh . . . . "Gletser Thwaites, terkadang disebut sebagai Gletser Kiamat, adalah sebuah gletser Antarktika besar tak lazim yang mengambang di , bagian dari Laut Amundsen, timur , di dari Tanah Marie Byrd. Kecepatan permukaan tersebut mencapai 2 kilometer (1,2 mil) per tahun di dekat . Pada 1967, menamai gletser tersebut dari Fredrik T. Thwaites (1883\u20131961), seorang pakar geologi glasial, pakar geomorfologi dan di Universitas Wisconsin\u2013Madison. Sejarawan adalah ayahnya."@in . . . "\u041B\u044C\u043E\u0434\u043E\u0432\u0438\u043A \u0422\u0432\u0435\u0439\u0442\u0441\u0430"@uk . . "\u30B9\u30A6\u30A7\u30A4\u30C4\u6C37\u6CB3"@ja . . "\u041B\u044C\u043E\u0434\u043E\u0432\u0438\u043A \u0422\u0432\u0435\u0439\u0442\u0441\u0430 \u0430\u0431\u043E \u043B\u044C\u043E\u0434\u043E\u0432\u0438\u043A \u0421\u0443\u0434\u043D\u043E\u0433\u043E \u0434\u043D\u044F \u2014 \u0430\u043D\u0442\u0430\u0440\u043A\u0442\u0438\u0447\u043D\u0438\u0439 \u043B\u044C\u043E\u0434\u043E\u0432\u0438\u043A, \u0449\u043E \u0432\u043F\u0430\u0434\u0430\u0454 \u0434\u043E , \u0430\u043A\u0432\u0430\u0442\u043E\u0440\u0456\u044F \u043C\u043E\u0440\u044F \u0410\u043C\u0443\u043D\u0434\u0441\u0435\u043D\u0430, \u043D\u0430 \u0441\u0445\u0456\u0434 \u0432\u0456\u0434 \u0433\u043E\u0440\u0438 \u041C\u0435\u0440\u0444\u0456, \u043D\u0430 \u0437\u0435\u043C\u043B\u0456 \u041C\u0430\u0440\u0456 \u0411\u0435\u0440\u0434."@uk . . "Por Thwaites entende-se tanto o glaciar/geleira propriamente dito como a l\u00EDngua de gelo com o mesmo nome. Ambos foram baptizado em homenagem a Fredrik T. Thwaites, ge\u00F3logo e professor em\u00E9rito da Universidade de Wisconsin-Madison."@pt . . "Der Thwaites-Gletscher (inoffiziell auch englisch Doomsday Glacier \u201AGletscher des J\u00FCngsten Gerichts, Weltuntergangsgletscher\u2018) ist ein gro\u00DFer Gletscher im westantarktischen Marie-Byrd-Land. 2010 wies er eine Ausdehnung von rund 192.000 km\u00B2 auf \u2013 eine Fl\u00E4che mehr als doppelt so gro\u00DF wie \u00D6sterreich bzw. in etwa so gro\u00DF wie Florida."@de . "Ghiacciaio Thwaites"@it . . "28328"^^ . . "Der Thwaites-Gletscher (inoffiziell auch englisch Doomsday Glacier \u201AGletscher des J\u00FCngsten Gerichts, Weltuntergangsgletscher\u2018) ist ein gro\u00DFer Gletscher im westantarktischen Marie-Byrd-Land. 2010 wies er eine Ausdehnung von rund 192.000 km\u00B2 auf \u2013 eine Fl\u00E4che mehr als doppelt so gro\u00DF wie \u00D6sterreich bzw. in etwa so gro\u00DF wie Florida."@de . . . . . . . "La Glacera de Thwaites \u00E9s una gran glacera a la Terra de Marie Byrd de la Ant\u00E0rtida Occidental. L'any 2010, tenia una extensi\u00F3 d'aproximadament 192.000 km\u00B2 \u2013 igual que Florida o el doble d'Austria."@ca . . . . . . . "Por Thwaites entende-se tanto o glaciar/geleira propriamente dito como a l\u00EDngua de gelo com o mesmo nome. Ambos foram baptizado em homenagem a Fredrik T. Thwaites, ge\u00F3logo e professor em\u00E9rito da Universidade de Wisconsin-Madison."@pt . . "Glacera de Thwaite"@ca . "Thwaitesgletsjer"@nl . . . . . . . "De Thwaitesgletsjer is een uitzonderlijk brede en snelle gletsjer in Marie Byrdland, Antarctica, die vanuit de West-Antarctische ijskap uitmondt in de , een onderdeel van de Amundsenzee. De oppervlaktesnelheid bedraagt meer dan 2 km/jaar nabij de contactlijn (grounding line) met het zeewater. De gletsjer werd door het ACAN vernoemd naar geoloog Fredrik T. Thwaites. De Thwaitesgletsjer wordt nauwkeurig geobserveerd vanwege zijn bijdrage tot de stijging van de zeespiegel."@nl . "Thwaites Glacier"@en . "La Glacera de Thwaites \u00E9s una gran glacera a la Terra de Marie Byrd de la Ant\u00E0rtida Occidental. L'any 2010, tenia una extensi\u00F3 d'aproximadament 192.000 km\u00B2 \u2013 igual que Florida o el doble d'Austria."@ca . . "El glaciar Thwaites es un gran glaciar de la Ant\u00E1rtida. Desemboca en el mar de Amundsen a unos 30 kil\u00F3metros al este del monte Murphy, en la tierra de Marie Byrd.\u200B Se encuentra en el sector ant\u00E1rtico que no es reclamado por ning\u00FAn pa\u00EDs.\u200B Fue cartografiado por el Servicio Geol\u00F3gico de los Estados Unidos a partir de trabajos en el \u00E1rea y fotograf\u00EDas realizadas por la Armada de los Estados Unidos entre 1959 y 1966. Fue nombrado por el Comit\u00E9 Consultivo sobre Nomenclatura Ant\u00E1rtica, en honor a Fredrik T. Thwaites, ge\u00F3logo glacial, geomorf\u00F3logo y profesor em\u00E9rito de la Universidad de Wisconsin-Madison.\u200B Sus velocidades de superficie exceden los 2 km por a\u00F1o cerca de su l\u00EDnea de tierra, y su hielo que fluye m\u00E1s r\u00E1pido se centra entre 50 y 100 km al este del Monte Murphy.\u200B Un estudio de la Universidad de Washington, utilizando mediciones satelitales y modelos de computadora, determin\u00F3 que el glaciar se derrite gradualmente, lo que puede llevar a un colapso irreversible en los pr\u00F3ximos 200 a 1000 a\u00F1os.\u200B\u200B\u200B\u200B\u200B De acuerdo a los expertos del Centro Espacial Goddard, esto significa que el glaciar est\u00E1 contribuyendo al 4% del aumento del nivel del mar en todo el planeta, hasta un metro y medio m\u00E1s que en la actualidad.\u200B"@es . . . . "\u041B\u044C\u043E\u0434\u043E\u0432\u0438\u043A \u0422\u0432\u0435\u0439\u0442\u0441\u0430 \u0430\u0431\u043E \u043B\u044C\u043E\u0434\u043E\u0432\u0438\u043A \u0421\u0443\u0434\u043D\u043E\u0433\u043E \u0434\u043D\u044F \u2014 \u0430\u043D\u0442\u0430\u0440\u043A\u0442\u0438\u0447\u043D\u0438\u0439 \u043B\u044C\u043E\u0434\u043E\u0432\u0438\u043A, \u0449\u043E \u0432\u043F\u0430\u0434\u0430\u0454 \u0434\u043E , \u0430\u043A\u0432\u0430\u0442\u043E\u0440\u0456\u044F \u043C\u043E\u0440\u044F \u0410\u043C\u0443\u043D\u0434\u0441\u0435\u043D\u0430, \u043D\u0430 \u0441\u0445\u0456\u0434 \u0432\u0456\u0434 \u0433\u043E\u0440\u0438 \u041C\u0435\u0440\u0444\u0456, \u043D\u0430 \u0437\u0435\u043C\u043B\u0456 \u041C\u0430\u0440\u0456 \u0411\u0435\u0440\u0434."@uk . "Thwaites Glacier"@en . . . . . . "Gletser Thwaites, terkadang disebut sebagai Gletser Kiamat, adalah sebuah gletser Antarktika besar tak lazim yang mengambang di , bagian dari Laut Amundsen, timur , di dari Tanah Marie Byrd. Kecepatan permukaan tersebut mencapai 2 kilometer (1,2 mil) per tahun di dekat . Pada 1967, menamai gletser tersebut dari Fredrik T. Thwaites (1883\u20131961), seorang pakar geologi glasial, pakar geomorfologi dan di Universitas Wisconsin\u2013Madison. Sejarawan adalah ayahnya."@in . . . . . "\u041B\u0435\u0434\u043D\u0438\u043A \u0422\u0443\u044D\u0439\u0442\u0441\u0430, \u0442\u0430\u043A\u0436\u0435 \u0438\u0437\u0432\u0435\u0441\u0442\u043D\u044B\u0439 \u043A\u0430\u043A \u00AB\u043B\u0435\u0434\u043D\u0438\u043A \u0441\u0443\u0434\u043D\u043E\u0433\u043E \u0434\u043D\u044F\u00BB (\u0430\u043D\u0433\u043B. Doomsday Glacier) \u2014 \u043B\u0435\u0434\u043D\u0438\u043A \u0432 \u0417\u0430\u043F\u0430\u0434\u043D\u043E\u0439 \u0410\u043D\u0442\u0430\u0440\u043A\u0442\u0438\u0434\u0435, \u0438\u0437\u0432\u0435\u0441\u0442\u043D\u044B\u0439 \u0441\u0432\u043E\u0438\u043C \u0431\u044B\u0441\u0442\u0440\u044B\u043C \u0434\u0432\u0438\u0436\u0435\u043D\u0438\u0435\u043C \u0438 \u0443\u0433\u0440\u043E\u0437\u043E\u0439 \u0443\u0432\u0435\u043B\u0438\u0447\u0435\u043D\u0438\u044F \u0443\u0440\u043E\u0432\u043D\u044F \u043C\u0438\u0440\u043E\u0432\u043E\u0433\u043E \u043E\u043A\u0435\u0430\u043D\u0430. \u0412 \u043F\u043E\u043F\u0435\u0440\u0435\u0447\u043D\u0438\u043A\u0435 \u0432\u044B\u0432\u043E\u0434\u043D\u0430\u044F \u0447\u0430\u0441\u0442\u044C \u043B\u0435\u0434\u043D\u0438\u043A\u0430 \u043F\u0440\u043E\u0441\u0442\u0438\u0440\u0430\u0435\u0442\u0441\u044F \u043D\u0430 120 \u043A\u043C \u0432\u0434\u043E\u043B\u044C \u043F\u043E\u0431\u0435\u0440\u0435\u0436\u044C\u044F, \u0447\u0442\u043E \u044F\u0432\u043B\u044F\u0435\u0442\u0441\u044F \u0440\u0435\u043A\u043E\u0440\u0434\u043D\u044B\u043C \u043F\u043E\u043A\u0430\u0437\u0430\u0442\u0435\u043B\u0435\u043C \u0441\u0440\u0435\u0434\u0438 \u0432\u0441\u0435\u0445 \u0434\u0440\u0443\u0433\u0438\u0445 \u043B\u0435\u0434\u043D\u0438\u043A\u043E\u0432. \u0412\u043F\u0430\u0434\u0430\u0435\u0442 \u0432 \u0437\u0430\u043B\u0438\u0432 \u041F\u0430\u0439\u043D-\u0410\u0439\u043B\u0435\u043D\u0434 \u043C\u043E\u0440\u044F \u0410\u043C\u0443\u043D\u0434\u0441\u0435\u043D\u0430, \u043A \u0432\u043E\u0441\u0442\u043E\u043A\u0443 \u043E\u0442 \u043F\u043E\u0442\u0443\u0445\u0448\u0435\u0433\u043E \u0432\u0443\u043B\u043A\u0430\u043D\u0430 \u041C\u0435\u0440\u0444\u0438. \u0421\u043A\u043E\u0440\u043E\u0441\u0442\u044C \u0434\u0432\u0438\u0436\u0435\u043D\u0438\u044F \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u043E\u0441\u0442\u0438 \u043B\u0435\u0434\u043D\u0438\u043A\u0430 \u0431\u043E\u043B\u0435\u0435 2 \u043A\u043C/\u0433\u043E\u0434. \u041D\u0430\u0437\u0432\u0430\u043D \u0432 \u0447\u0435\u0441\u0442\u044C \u0443\u0447\u0451\u043D\u043E\u0433\u043E-\u0433\u043B\u044F\u0446\u0438\u043E\u043B\u043E\u0433\u0430 \u0424\u0440\u0435\u0434\u0440\u0438\u043A\u0430 \u0422. \u0422\u0443\u044D\u0439\u0442\u0441\u0430 (Fredrik T. Thwaites, 1883\u20141961)."@ru . . . "20"^^ . "Le glacier Thwaites est un glacier d'Antarctique situ\u00E9 dans la Terre Marie Byrd. Il forme une barri\u00E8re de glace aliment\u00E9e par un courant glaciaire permettant \u00E0 une partie des glaces de l'inlandsis Ouest-Antarctique de s'\u00E9vacuer du plateau de Antarctique occidental vers la mer d'Amundsen. Il est surveill\u00E9 depuis des d\u00E9cennies par les glaciologues en raison de ses dimensions et de son r\u00F4le majeur dans le bilan hydrique de cette partie du continent : l'acc\u00E9l\u00E9ration de sa vitesse d'\u00E9coulement constat\u00E9e depuis le d\u00E9but des ann\u00E9es 2000 pourrait amener \u00E0 sa dislocation totale et rapide et au d\u00E9versement d'importantes quantit\u00E9s de glaces dans l'oc\u00E9an mondial, contribuant ainsi significativement \u00E0 l'\u00E9l\u00E9vation du niveau de la mer ; il est ainsi surnomm\u00E9 \u00AB glacier de l'apocalypse \u00BB par certains m\u00E9dia"@fr . . "Le glacier Thwaites est un glacier d'Antarctique situ\u00E9 dans la Terre Marie Byrd. Il forme une barri\u00E8re de glace aliment\u00E9e par un courant glaciaire permettant \u00E0 une partie des glaces de l'inlandsis Ouest-Antarctique de s'\u00E9vacuer du plateau de Antarctique occidental vers la mer d'Amundsen. Il est surveill\u00E9 depuis des d\u00E9cennies par les glaciologues en raison de ses dimensions et de son r\u00F4le majeur dans le bilan hydrique de cette partie du continent : l'acc\u00E9l\u00E9ration de sa vitesse d'\u00E9coulement constat\u00E9e depuis le d\u00E9but des ann\u00E9es 2000 pourrait amener \u00E0 sa dislocation totale et rapide et au d\u00E9versement d'importantes quantit\u00E9s de glaces dans l'oc\u00E9an mondial, contribuant ainsi significativement \u00E0 l'\u00E9l\u00E9vation du niveau de la mer ; il est ainsi surnomm\u00E9 \u00AB glacier de l'apocalypse \u00BB par certains m\u00E9dias."@fr . . . "Visiting the most vulnerable place on Earth: the 'doomsday glacier'"@en . "Below sea level"@en . . . . . "Walgreen Coast, Marie Byrd Land, Antarctic"@en . . . . . . . . . "POINT(-106.75 -75.5)"^^ . . . "Thwaites Glacier"@sv . "Il ghiacciaio Thwaites (75\u00B030\u2032S 106\u00B045\u2032W\uFEFF / \uFEFF75.5\u00B0S 106.75\u00B0W) \u00E8 un ampio ed inusualmente vasto ghiacciaio dell'Antartide che fluisce nella baia Pine Island, parte del Mare di Amundsen, ad est del , sulla costa di Walgreen della Terra di Marie Byrd. Le velocit\u00E0 della sua superficie superano i 2 km/anno nei pressi della sua linea di galleggiamento, e il ghiaccio che fluisce con maggiore velocit\u00E0 al suolo si centra tra i 50 e i 100 km ad est del monte Murphy. Venne denominato dall'ACAN in onore di Fredrik T. Thwaites, un geologo glaciale, geomorfologo e professore emerito all'University of Wisconsin\u2013Madison. Il ghiacciaio Thwaites defluisce nel mare di Amundsen nell'Antartide occidentale e viene attentamente monitorato per il pericolo potenziale che potrebbe rappresentare, dato che se scivola"@it . "De Thwaitesgletsjer is een uitzonderlijk brede en snelle gletsjer in Marie Byrdland, Antarctica, die vanuit de West-Antarctische ijskap uitmondt in de , een onderdeel van de Amundsenzee. De oppervlaktesnelheid bedraagt meer dan 2 km/jaar nabij de contactlijn (grounding line) met het zeewater. De gletsjer werd door het ACAN vernoemd naar geoloog Fredrik T. Thwaites. De Thwaitesgletsjer wordt nauwkeurig geobserveerd vanwege zijn bijdrage tot de stijging van de zeespiegel. Het volume van de gletsjer wordt geschat op 483 \u00B1 6 x 103 km\u00B3 ijs, waarvan ongeveer 258 \u00B1 6 103 km\u00B3 boven zeeniveau. Zou de gletsjer volledig afsmelten, dan komt dit overeen met een zeespiegelstijging van ongeveer 65 cm."@nl . "1123703998"^^ . . "Thwaits Glacier.jpg"@en . . . "Glaciar Thwaites"@es . "2815865"^^ . . . . . . . "\u30B9\u30A6\u30A7\u30A4\u30C4\u6C37\u6CB3\uFF08\u30B9\u30A6\u30A7\u30A4\u30C4\u3072\u3087\u3046\u304C\u3001\u82F1\u8A9E: Thwaites Glacier\uFF09\u306F\u3001\u5357\u6975\u306E\u4ED8\u8FD1\u306B\u3042\u308B\u6C37\u6CB3\u3067\u3042\u308B\u3002\u79FB\u52D5\u901F\u5EA6\u304C\u5927\u304D\u3044\u6C37\u6CB3\u3067\u3042\u308A\u3001\u79FB\u52D5\u901F\u5EA6\u306F 2 km/year \u4EE5\u4E0A\u3067\u3042\u308B\u3002 \u3053\u306E\u6C37\u6CB3\u306F\u878D\u89E3\u304C\u9032\u884C\u3057\u3066\u304A\u308A\u3001\u5730\u7403\u6E29\u6696\u5316\u306B\u3088\u308B\u6D77\u9762\u4E0A\u6607\u306B\u5F71\u97FF\u3092\u4E0E\u3048\u308B\u304A\u305D\u308C\u304C\u5927\u304D\u3044\u3002"@ja . . "\u041B\u0435\u0434\u043D\u0438\u043A \u0422\u0443\u044D\u0439\u0442\u0441\u0430, \u0442\u0430\u043A\u0436\u0435 \u0438\u0437\u0432\u0435\u0441\u0442\u043D\u044B\u0439 \u043A\u0430\u043A \u00AB\u043B\u0435\u0434\u043D\u0438\u043A \u0441\u0443\u0434\u043D\u043E\u0433\u043E \u0434\u043D\u044F\u00BB (\u0430\u043D\u0433\u043B. Doomsday Glacier) \u2014 \u043B\u0435\u0434\u043D\u0438\u043A \u0432 \u0417\u0430\u043F\u0430\u0434\u043D\u043E\u0439 \u0410\u043D\u0442\u0430\u0440\u043A\u0442\u0438\u0434\u0435, \u0438\u0437\u0432\u0435\u0441\u0442\u043D\u044B\u0439 \u0441\u0432\u043E\u0438\u043C \u0431\u044B\u0441\u0442\u0440\u044B\u043C \u0434\u0432\u0438\u0436\u0435\u043D\u0438\u0435\u043C \u0438 \u0443\u0433\u0440\u043E\u0437\u043E\u0439 \u0443\u0432\u0435\u043B\u0438\u0447\u0435\u043D\u0438\u044F \u0443\u0440\u043E\u0432\u043D\u044F \u043C\u0438\u0440\u043E\u0432\u043E\u0433\u043E \u043E\u043A\u0435\u0430\u043D\u0430. \u0412 \u043F\u043E\u043F\u0435\u0440\u0435\u0447\u043D\u0438\u043A\u0435 \u0432\u044B\u0432\u043E\u0434\u043D\u0430\u044F \u0447\u0430\u0441\u0442\u044C \u043B\u0435\u0434\u043D\u0438\u043A\u0430 \u043F\u0440\u043E\u0441\u0442\u0438\u0440\u0430\u0435\u0442\u0441\u044F \u043D\u0430 120 \u043A\u043C \u0432\u0434\u043E\u043B\u044C \u043F\u043E\u0431\u0435\u0440\u0435\u0436\u044C\u044F, \u0447\u0442\u043E \u044F\u0432\u043B\u044F\u0435\u0442\u0441\u044F \u0440\u0435\u043A\u043E\u0440\u0434\u043D\u044B\u043C \u043F\u043E\u043A\u0430\u0437\u0430\u0442\u0435\u043B\u0435\u043C \u0441\u0440\u0435\u0434\u0438 \u0432\u0441\u0435\u0445 \u0434\u0440\u0443\u0433\u0438\u0445 \u043B\u0435\u0434\u043D\u0438\u043A\u043E\u0432. \u0412\u043F\u0430\u0434\u0430\u0435\u0442 \u0432 \u0437\u0430\u043B\u0438\u0432 \u041F\u0430\u0439\u043D-\u0410\u0439\u043B\u0435\u043D\u0434 \u043C\u043E\u0440\u044F \u0410\u043C\u0443\u043D\u0434\u0441\u0435\u043D\u0430, \u043A \u0432\u043E\u0441\u0442\u043E\u043A\u0443 \u043E\u0442 \u043F\u043E\u0442\u0443\u0445\u0448\u0435\u0433\u043E \u0432\u0443\u043B\u043A\u0430\u043D\u0430 \u041C\u0435\u0440\u0444\u0438. \u0421\u043A\u043E\u0440\u043E\u0441\u0442\u044C \u0434\u0432\u0438\u0436\u0435\u043D\u0438\u044F \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u043E\u0441\u0442\u0438 \u043B\u0435\u0434\u043D\u0438\u043A\u0430 \u0431\u043E\u043B\u0435\u0435 2 \u043A\u043C/\u0433\u043E\u0434. \u041D\u0430\u0437\u0432\u0430\u043D \u0432 \u0447\u0435\u0441\u0442\u044C \u0443\u0447\u0451\u043D\u043E\u0433\u043E-\u0433\u043B\u044F\u0446\u0438\u043E\u043B\u043E\u0433\u0430 \u0424\u0440\u0435\u0434\u0440\u0438\u043A\u0430 \u0422. \u0422\u0443\u044D\u0439\u0442\u0441\u0430 (Fredrik T. Thwaites, 1883\u20141961). \u0412\u043C\u0435\u0441\u0442\u0435 \u0441 \u043B\u0435\u0434\u043D\u0438\u043A\u043E\u043C , \u043B\u0435\u0434\u043D\u0438\u043A \u0422\u0443\u044D\u0439\u0442\u0441\u0430 \u0431\u044B\u043B \u043E\u043F\u0438\u0441\u0430\u043D \u043A\u0430\u043A \u0447\u0430\u0441\u0442\u044C \u00AB\u0441\u043B\u0430\u0431\u043E\u0433\u043E \u043F\u043E\u0434\u0431\u0440\u044E\u0448\u044C\u044F\u00BB . \u0412 \u0441\u043B\u0443\u0447\u0430\u0435 \u043F\u043E\u043B\u043D\u043E\u0433\u043E \u0440\u0430\u0437\u0440\u0443\u0448\u0435\u043D\u0438\u044F \u0438 \u0442\u0430\u044F\u043D\u0438\u044F \u044D\u0442\u043E\u0433\u043E \u043B\u0435\u0434\u043D\u0438\u043A\u0430 \u0443\u0440\u043E\u0432\u0435\u043D\u044C \u041C\u0438\u0440\u043E\u0432\u043E\u0433\u043E \u043E\u043A\u0435\u0430\u043D\u0430 \u0432\u044B\u0440\u0430\u0441\u0442\u0435\u0442 \u043D\u0430 0,6 \u043C (\u0447\u0442\u043E \u0441\u043F\u043E\u0441\u043E\u0431\u043D\u043E \u043F\u043E\u0432\u043B\u0435\u0447\u044C \u0434\u0430\u043B\u044C\u043D\u0435\u0439\u0448\u0435\u0435 \u043F\u043E\u0434\u043D\u044F\u0442\u0438\u0435 \u0443\u0440\u043E\u0432\u043D\u044F \u043C\u043E\u0440\u044F \u0434\u043E \u0442\u0440\u0435\u0445 \u043C\u0435\u0442\u0440\u043E\u0432), \u0435\u0433\u043E \u0441\u043E\u0432\u0440\u0435\u043C\u0435\u043D\u043D\u043E\u0435 \u0442\u0430\u044F\u043D\u0438\u0435 \u043E\u0442\u0432\u0435\u0442\u0441\u0442\u0432\u0435\u043D\u043D\u043E \u0437\u0430 4 % \u043E\u0442 \u0432\u0441\u0435\u0433\u043E \u0442\u0435\u043A\u0443\u0449\u0435\u0433\u043E \u0440\u043E\u0441\u0442\u0430 \u0443\u0440\u043E\u0432\u043D\u044F \u043C\u043E\u0440\u044F. \u0415\u0436\u0435\u0433\u043E\u0434\u043D\u043E \u0441 \u043B\u0435\u0434\u043D\u0438\u043A\u0430 \u043F\u043E\u0441\u0442\u0443\u043F\u0430\u0435\u0442 \u0432 \u043E\u043A\u0435\u0430\u043D 50 \u043C\u043B\u0440\u0434 \u0442\u043E\u043D\u043D \u043B\u044C\u0434\u0430. \u0421\u043E\u0433\u043B\u0430\u0441\u043D\u043E \u0438\u0441\u0441\u043B\u0435\u0434\u043E\u0432\u0430\u043D\u0438\u044F\u043C \u0412\u0430\u0448\u0438\u043D\u0433\u0442\u043E\u043D\u0441\u043A\u043E\u0433\u043E \u0443\u043D\u0438\u0432\u0435\u0440\u0441\u0438\u0442\u0435\u0442\u0430, \u043F\u0440\u043E\u0432\u0435\u0434\u0451\u043D\u043D\u044B\u043C \u0432 2014 \u0433\u043E\u0434\u0443 \u0441 \u0438\u0441\u043F\u043E\u043B\u044C\u0437\u043E\u0432\u0430\u043D\u0438\u0435\u043C \u0441\u043F\u0443\u0442\u043D\u0438\u043A\u043E\u0432\u044B\u0445 \u0438\u0437\u043C\u0435\u0440\u0435\u043D\u0438\u0439 \u0438 \u043A\u043E\u043C\u043F\u044C\u044E\u0442\u0435\u0440\u043D\u044B\u0445 \u043C\u043E\u0434\u0435\u043B\u0435\u0439, \u043B\u0435\u0434\u043D\u0438\u043A \u0431\u0443\u0434\u0435\u0442 \u043F\u043E\u0441\u0442\u0435\u043F\u0435\u043D\u043D\u043E \u0442\u0430\u044F\u0442\u044C, \u0447\u0442\u043E \u043F\u0440\u0438\u0432\u0435\u0434\u0451\u0442 \u043A \u0435\u0433\u043E \u043D\u0435\u043E\u0431\u0440\u0430\u0442\u0438\u043C\u043E\u043C\u0443 \u043A\u043E\u043B\u043B\u0430\u043F\u0441\u0443 \u0432 \u0441\u043B\u0435\u0434\u0443\u044E\u0449\u0438\u0435 200\u20141000 \u043B\u0435\u0442. \u041F\u043E \u0443\u0442\u043E\u0447\u043D\u0451\u043D\u043D\u044B\u043C \u0434\u0430\u043D\u043D\u044B\u043C 2021 \u0433\u043E\u0434\u0430 \u043F\u043B\u0430\u0432\u0430\u044E\u0449\u0430\u044F \u0447\u0430\u0441\u0442\u044C \u043B\u0435\u0434\u043D\u0438\u043A\u0430 \u043C\u043E\u0436\u0435\u0442 \u0440\u0430\u0437\u0440\u0443\u0448\u0438\u0442\u044C\u0441\u044F \u0437\u0430 \u0441\u043B\u0435\u0434\u0443\u044E\u0449\u0438\u0435 5 \u0438\u043B\u0438 10 \u043B\u0435\u0442. \u0414\u043B\u044F \u0438\u0437\u0443\u0447\u0435\u043D\u0438\u044F \u0442\u0430\u044F\u043D\u0438\u044F \u043B\u0435\u0434\u043D\u0438\u043A\u0430 \u0432\u044B\u0434\u0435\u043B\u0435\u043D\u043E $50 \u043C\u043B\u043D, \u0437\u0430 \u0441\u0447\u0451\u0442 \u043A\u043E\u0442\u043E\u0440\u044B\u0445 \u043F\u0440\u043E\u0432\u043E\u0434\u0438\u0442\u0441\u044F \u043F\u044F\u0442\u0438\u043B\u0435\u0442\u043D\u0435\u0435 \u043C\u0435\u0436\u0434\u0443\u043D\u0430\u0440\u043E\u0434\u043D\u043E\u0435 \u0438\u0441\u0441\u043B\u0435\u0434\u043E\u0432\u0430\u043D\u0438\u0435."@ru . . . "\u601D\u97CB\u8328\u51B0\u5DDD\uFF08\u82F1\u8A9E\uFF1AThwaites Glacier\uFF09\u662F\u5357\u6975\u6D32\u7684\u51B0\u5DDD\uFF0C\u4F4D\u65BC\u746A\u9E97\u4F2F\u5FB7\u5730\u7684\u6C83\u723E\u683C\u6797\u6D77\u5CB8\uFF0C\u6700\u7D42\u6CE8\u5165\u963F\u8499\u68EE\u6D77\uFF0C\u4EE5\u5A01\u65AF\u5EB7\u8F9B\u5927\u5B78\u9EA5\u8FEA\u905C\u5206\u6821\u7684\u5730\u8CEA\u5B78\u5BB6\u547D\u540D\uFF0C\u73FE\u6642\u7531\u5357\u6975\u689D\u7D04\u9AD4\u7CFB\u7BA1\u7406\u3002\u898F\u6A21\u5B8F\u5927\uFF0C\u800C\u5728\u5168\u7403\u6696\u5316\u5E95\u4E0B\uFF0C\u88AB\u8A8D\u70BA\u53EF\u80FD\u5C0D\u6D77\u5E73\u9762\u4E0A\u5347\u5E36\u4F86\u91CD\u5927\u5F71\u97FF\uFF0C\u6545\u53C8\u88AB\u7A31\u70BA\u672B\u65E5\u51B0\u5DDD \uFF08\u82F1\u8A9E\uFF1ADoomsday Glacier\uFF09\u3002"@zh . . "Glacier Thwaites"@fr . "Thwaites Glacier \u00E4r en glaci\u00E4r i Antarktis. Den ligger i V\u00E4stantarktis och fl\u00F6dar in i Pine Island Bay. Glaci\u00E4ren ben\u00E4mns ibland \"Domedagsglaci\u00E4ren\" p\u00E5 grund av dess potential att orsaka havsniv\u00E5h\u00F6jning."@sv . . . . "Thwaites Glacier"@en . . . "\u601D\u97CB\u8328\u51B0\u5DDD"@zh . . . "Pine Island Bay, part of the Amundsen Sea"@en . . "Thwaites-Gletscher"@de . "Glaciar Thwaites"@pt . "-106.75"^^ . . . . "\u041B\u0435\u0434\u043D\u0438\u043A \u0422\u0443\u044D\u0439\u0442\u0441\u0430"@ru . "El glaciar Thwaites es un gran glaciar de la Ant\u00E1rtida. Desemboca en el mar de Amundsen a unos 30 kil\u00F3metros al este del monte Murphy, en la tierra de Marie Byrd.\u200B Se encuentra en el sector ant\u00E1rtico que no es reclamado por ning\u00FAn pa\u00EDs.\u200B Sus velocidades de superficie exceden los 2 km por a\u00F1o cerca de su l\u00EDnea de tierra, y su hielo que fluye m\u00E1s r\u00E1pido se centra entre 50 y 100 km al este del Monte Murphy.\u200B"@es . . . . "-75.5 -106.75" . "Il ghiacciaio Thwaites (75\u00B030\u2032S 106\u00B045\u2032W\uFEFF / \uFEFF75.5\u00B0S 106.75\u00B0W) \u00E8 un ampio ed inusualmente vasto ghiacciaio dell'Antartide che fluisce nella baia Pine Island, parte del Mare di Amundsen, ad est del , sulla costa di Walgreen della Terra di Marie Byrd. Le velocit\u00E0 della sua superficie superano i 2 km/anno nei pressi della sua linea di galleggiamento, e il ghiaccio che fluisce con maggiore velocit\u00E0 al suolo si centra tra i 50 e i 100 km ad est del monte Murphy. Venne denominato dall'ACAN in onore di Fredrik T. Thwaites, un geologo glaciale, geomorfologo e professore emerito all'University of Wisconsin\u2013Madison. Il ghiacciaio Thwaites defluisce nel mare di Amundsen nell'Antartide occidentale e viene attentamente monitorato per il pericolo potenziale che potrebbe rappresentare, dato che se scivolasse nell'oceano potrebbe causare l'innalzamento globale del livello dei mari di oltre mezzo metro, aprendo poi la strada allo scioglimento di tutto l'Antartide occidentale Assieme al ghiacciaio Pine Island, il Thwaites Glacier \u00E8 stato descritto come parte del \"ventre molle\" della calotta glaciale dell'Antartide Occidentale, a causa della sua apparente vulnerabilit\u00E0 a correnti marine e venti tiepidi che possono provocare la loro significativa ritirata. Questa ipotesi si basa sia su studi teorici sulla stabilit\u00E0 delle coltri di ghiaccio marittime e alla recente osservazione di grandi cambiamenti in questi due ghiacciai. In anni recenti, il flusso di entrambi i ghiacciai si \u00E8 accelerato, le loro superfici sono diminuite nell'altezza compressiva e la linea di perdita di contatto alla base con il terreno sostituita dal mare si sono ritirate verso l'interno del continente. Nel 2011, utilizzando dati geofisici raccolti da sorvoli del Thwaites Glacier (ottenuti nel corso della campagna della NASA \"Ice Bridge\"), uno studio eseguito dal Lamont-Doherty Earth Observatory della Columbia University dimostr\u00F2 l'esistenza di un gigantesco sperone montuoso di roccia sottomarino, una cresta alta 700 metri che aiuta l'ancoraggio del ghiacciaio e che in effetti rallenta lo slittamento del ghiacciaio verso il mare. Lo studio conferma anche l'importanza della topografia nel predire come questi ghiacciai si comporteranno nel futuro prossimo."@it . . "\u30B9\u30A6\u30A7\u30A4\u30C4\u6C37\u6CB3\uFF08\u30B9\u30A6\u30A7\u30A4\u30C4\u3072\u3087\u3046\u304C\u3001\u82F1\u8A9E: Thwaites Glacier\uFF09\u306F\u3001\u5357\u6975\u306E\u4ED8\u8FD1\u306B\u3042\u308B\u6C37\u6CB3\u3067\u3042\u308B\u3002\u79FB\u52D5\u901F\u5EA6\u304C\u5927\u304D\u3044\u6C37\u6CB3\u3067\u3042\u308A\u3001\u79FB\u52D5\u901F\u5EA6\u306F 2 km/year \u4EE5\u4E0A\u3067\u3042\u308B\u3002 \u3053\u306E\u6C37\u6CB3\u306F\u878D\u89E3\u304C\u9032\u884C\u3057\u3066\u304A\u308A\u3001\u5730\u7403\u6E29\u6696\u5316\u306B\u3088\u308B\u6D77\u9762\u4E0A\u6607\u306B\u5F71\u97FF\u3092\u4E0E\u3048\u308B\u304A\u305D\u308C\u304C\u5927\u304D\u3044\u3002"@ja . . "yes"@en . "Doomsday Glacier"@en . . "Thwaites Glacier \u00E4r en glaci\u00E4r i Antarktis. Den ligger i V\u00E4stantarktis och fl\u00F6dar in i Pine Island Bay. Glaci\u00E4ren ben\u00E4mns ibland \"Domedagsglaci\u00E4ren\" p\u00E5 grund av dess potential att orsaka havsniv\u00E5h\u00F6jning."@sv . . . "UQ782Nz2VHs"@en . "Thwaites Glacier, nicknamed the Doomsday Glacier, is an unusually broad and vast Antarctic glacier flowing into Pine Island Bay, part of the Amundsen Sea, east of Mount Murphy, on the Walgreen Coast of Marie Byrd Land. Its surface speeds exceed 2 kilometres (1.2 miles) per year near its grounding line. Its fastest-flowing grounded ice is centered between 50 and 100 kilometres (31 and 62 mi) east of Mount Murphy. In 1967, the Advisory Committee on Antarctic Names named the glacier after Fredrik T. Thwaites (1883\u20131961), a glacial geologist, geomorphologist and professor emeritus at the University of Wisconsin\u2013Madison."@en . "-75.5"^^ . . . . . . . . . . . "Thwaites Glacier, nicknamed the Doomsday Glacier, is an unusually broad and vast Antarctic glacier flowing into Pine Island Bay, part of the Amundsen Sea, east of Mount Murphy, on the Walgreen Coast of Marie Byrd Land. Its surface speeds exceed 2 kilometres (1.2 miles) per year near its grounding line. Its fastest-flowing grounded ice is centered between 50 and 100 kilometres (31 and 62 mi) east of Mount Murphy. In 1967, the Advisory Committee on Antarctic Names named the glacier after Fredrik T. Thwaites (1883\u20131961), a glacial geologist, geomorphologist and professor emeritus at the University of Wisconsin\u2013Madison. Thwaites Glacier is closely monitored for its potential to raise sea levels. Along with the Pine Island Glacier, it has been described as part of the \"weak underbelly\" of the West Antarctic Ice Sheet, because of its apparent vulnerability to significant retreat. This hypothesis is based on both theoretical studies of the stability of marine ice sheets and observations of large changes on these two glaciers. In recent years, the flow of both of these glaciers has accelerated, their surfaces have lowered, and their grounding lines have retreated. The Thwaites Ice Shelf, a floating ice shelf which braces and restrains the eastern portion of Thwaites Glacier, is likely to collapse within a decade from 2021. While the glacier itself would still take approximately several centuries to collapse even after the loss of its ice shelf, its outflow and contribution to sea-level rise would accelerate substantially; while it currently amounts to 4% of global sea level rise, it would become equivalent to 5% in the short term, and likely accelerate further in the longer term. For this reason, Thwaites Glacier and its ice shelf have been proposed as sites for climate engineering interventions to stabilize and preserve its ice."@en . . . . . "Doomsday Glacier"@en . . . . . . . . . "Receding"@en . . "Tidewater valley"@en . "Gletser Thwaites"@in . . . . . . . . "Thwaites Glacier"@en . . "Thwaites Glacier"@en . "120"^^ .