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<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Permafrost definieras som ett tillst\u00E5nd d\u00E4r temperaturen i marken inte n\u00E5r upp \u00F6ver noll grader under minst tv\u00E5 \u00E5r i rad. Ovanp\u00E5 permafrosten finns ett aktivt lager som tinar om v\u00E5ren och sommaren och fryser igen under vintern. Det aktiva lagrets tjocklek beror p\u00E5 klimatet och markens v\u00E4rmeledande egenskaper men \u00E4r p\u00E5 de flesta platser mellan en halvmeter och ett par meter. Permafrostens tjocklek beror bland annat p\u00E5 det nuvarande och det historiska klimatet. I omr\u00E5den l\u00E5ngt norrut som har haft ett kallt klimat v\u00E4ldigt l\u00E4nge, exempelvis norra Sibirien, kan permafrosten vara flera hundra meter tjock."@sv .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"Permafrost is ground that continuously remains below 0 \u00B0C (32 \u00B0F) for two or more years, located on land or under the ocean. Most common in the Northern Hemisphere, around 15% of the Northern Hemisphere or 11% of the global surface is underlain by permafrost, with the total area of around 18 million km2. This includes substantial areas of Alaska, Greenland, Canada and Siberia. It can also be located on mountaintops in the Southern Hemisphere and beneath ice-free areas in the Antarctic. Permafrost does not have to be the first layer that is on the ground. It can be from an inch to several miles deep under the Earth's surface. It frequently occurs in ground ice, but it can also be present in non-porous bedrock. Permafrost is formed from ice holding various types of soil, sand, and rock in combination. Permafrost contains large amounts of biomass and decomposed biomass that has been stored as methane and carbon dioxide, making tundra soil a carbon sink. As global warming heats the ecosystem and causes soil thawing, the permafrost carbon cycle accelerates and releases much of these soil-contained greenhouse gases into the atmosphere, creating a feedback cycle that increases climate change. Thawing of permafrost is one of the effects of climate change. While emissions from thawing permafrost will be significant enough to lead to additional warming, they will likely not be enough to trigger a self-reinforcing feedback leading to \"runaway warming\"."@en .
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<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Permafrost, vanuit het Russisch soms ook merzlota (\"bevroren grond\") genoemd, is het verschijnsel dat in bepaalde gebieden nabij de polen en in het hooggebergte de ondergrond nooit helemaal ontdooit."@nl .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"Wieczna lub wieloletnia zmarzlina, zwana te\u017C czasem wieczn\u0105 marz\u0142oci\u0105 lub marz\u0142oci\u0105 trwa\u0142\u0105 lub zlodowaceniem podziemnym \u2013 zjawisko trwa\u0142ego (minimum dwa kolejne lata) utrzymywania si\u0119 cz\u0119\u015Bci skorupy ziemskiej w temperaturze poni\u017Cej punktu zamarzania wody niezale\u017Cnie od pory roku. Powstaje w warunkach suchego, zimnego klimatu (o \u015Bredniej temperaturze powietrza poni\u017Cej \u221211 \u00B0C). Obejmuje oko\u0142o 80% Alaski, wi\u0119kszo\u015B\u0107 p\u00F3\u0142nocnej Kanady i 65% Syberii (ci\u0105g\u0142a zmarzlina wyst\u0119puje prawie wy\u0142\u0105cznie we wschodniej Syberii, w zachodniej jest obecna tylko na p\u00F3\u0142nocnym wybrze\u017Cu oceanu). Ci\u0105g\u0142a zmarzlina si\u0119ga a\u017C do p\u00F3\u0142nocnej Mongolii, punktowo wyst\u0119puje te\u017C w G\u00F3rach Skandynawskich i na Grenlandii. Natomiast nieci\u0105g\u0142e zmarzliny zajmuj\u0105 tak\u017Ce wi\u0119kszo\u015B\u0107 Tybetu, s\u0105 te\u017C znane z Alp. Wieczn\u0105 zmarzlin\u0119 odkryto r\u00F3wnie\u017C w p\u00F3\u0142nocno-wschodniej Polsce, w okolicy Suwa\u0142k na g\u0142\u0119boko\u015Bci 357 metr\u00F3w poni\u017Cej poziomu gruntu. Jest to pozosta\u0142o\u015B\u0107 po zmarzlinie z okresu ostatniego zlodowacenia, kt\u00F3ra przetrwa\u0142a dzi\u0119ki specyficznym warunkom geologicznym, tak zwanej . Ocenia si\u0119, \u017Ce najstarsza zmarzlina powsta\u0142a na Ziemi ok. 2,6 mln lat temu. Jej g\u0142\u0119boko\u015B\u0107 na tych obszarach, na kt\u00F3rych przetrwa\u0142a od plejstocenu waha si\u0119 w granicach od 150\u2013300 metr\u00F3w w p\u00F3\u0142nocnej Kanadzie (maksymalnie dochodzi tam do 700 m), we wschodniej Syberii dochodzi do 1500 m. Przewa\u017Cnie ma kilkadziesi\u0105t metr\u00F3w. W miesi\u0105cach letnich wierzchnia warstwa gruntu \u2013 do oko\u0142o dw\u00F3ch metr\u00F3w \u2013 ulega rozmarzni\u0119ciu, wskutek czego staje si\u0119 on cz\u0119sto grz\u0105skim bagnem, w g\u0142\u0105b kt\u00F3rego nie mo\u017Ce (z powodu zamarzni\u0119tych g\u0142\u0119bszych warstw) wsi\u0105kn\u0105\u0107 nadmiar wody. Sytuacja ta utrudnia rozw\u00F3j ro\u015Blinno\u015Bci, uniemo\u017Cliwiaj\u0105c m.in. zasiedlanie pokrytych wieczn\u0105 zmarzlin\u0105 obszar\u00F3w drzewom o g\u0142\u0119bszym systemie korzeniowym, tak\u017Ce z powodu niedostatecznej spoisto\u015Bci gleby w miesi\u0105cach letnich. Dawniej, zmarzlina znacz\u0105co utrudnia\u0142a wznoszenie budynk\u00F3w. Oparcie fundament\u00F3w na zmarzlinie powoduje stopniowe wtapianie si\u0119 budynku i osiadanie, nieraz o kilka metr\u00F3w. Typowym przyk\u0142adem s\u0105 starsze budynki w Irkucku, kt\u00F3rych pierwsze pi\u0119tro znajduje si\u0119 obecnie na poziomie gruntu. Wieloletnia zmarzlina ma charakter reliktowy. Jest pozosta\u0142o\u015Bci\u0105 zlodowacenia, kt\u00F3re w plejstocenie obejmowa\u0142o znaczn\u0105 cz\u0119\u015B\u0107 obszar\u00F3w l\u0105dowych p\u00F3\u0142kuli p\u00F3\u0142nocnej. Marz\u0142o\u0107 to warstwa gruntu, le\u017C\u0105ca na r\u00F3\u017Cnych g\u0142\u0119boko\u015Bciach, kt\u00F3ra co najmniej przez dwa kolejne lata zachowuje temperatur\u0119 ni\u017Csz\u0105 ni\u017C 0 \u00B0C (poni\u017Cej punktu zamarzania).Rodzaje marz\u0142oci: \n* \u2013 nie zawiera lodu jako materia\u0142u spajaj\u0105cego (np. ska\u0142a) \n* wilgotna \u2013 najcz\u0119\u015Bciej spotykana, l\u00F3d wype\u0142nia wolne przestrzenie gruntu lub pory ska\u0142 Typy marz\u0142oci (ze wzgl\u0119du na zasi\u0119g warstwy odmarzaj\u0105cej): \n* \u2013 grunt pozostaje zamarzni\u0119ty na ca\u0142ym obszarze, przy \u015Bredniej temperaturze roku poni\u017Cej \u22128 \u00B0C \n* \u2013 z niezamarzni\u0119tymi \u201Ewyspami\u201D, przy \u015Bredniej temperaturze roku od \u22124 do \u22128 \u00B0C \n* \u2013 p\u0142aty marz\u0142oci w niejednolicie zamarzaj\u0105cym gruncie, przy \u015Bredniej temperaturze roku od \u22121 do \u22124 \u00B0C"@pl .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"El permafrost\u200B (ocasionalmente traducido como permahielo, gelisuelo,\u200B permagel o permacongelamiento)\u200B es la capa de suelo permanentemente congelado \u2014pero no permanentemente cubierto de hielo o nieve\u2014 de las regiones muy fr\u00EDas o periglaciares, como la tundra. Puede encontrarse en \u00E1reas circumpolares de Canad\u00E1, Alaska, Groenlandia, Siberia, T\u00EDbet, Noruega y en varias islas del oc\u00E9ano Atl\u00E1ntico sur como las islas Georgias del Sur y las islas Sandwich del Sur.[cita requerida] El permafrost se puede dividir en pergelisol, que es la capa helada m\u00E1s profunda, y mollisol, el estrato m\u00E1s superficial que suele descongelarse. Durante cientos de miles de a\u00F1os, el permafrost del \u00C1rtico\u200B ha acumulado grandes reservas de carbono org\u00E1nico (se estima que de 1,4 a 1,85 billones de toneladas m\u00E9tricas). Los pron\u00F3sticos predicen una disminuci\u00F3n en las \u00E1reas de permafrost debido al aumento del calentamiento global.\u200B\u200B Cuando el permafrost se descongela, se libera di\u00F3xido de carbono\u200B y metano.\u200B Tambi\u00E9n permite el resurgimiento de virus y bacterias desconocidos que pasaron decenas de miles de a\u00F1os congelados as\u00ED como subproductos de combustibles f\u00F3siles y productos qu\u00EDmicos como el DDT, que actualmente se encuentra prohibidos por los da\u00F1os a la salud y al ambiente.\u200B"@es .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"\u0411\u0430\u0433\u0430\u0442\u043E\u0440\u0456\u0301\u0447\u043D\u0430 \u043C\u0435\u0440\u0437\u043B\u043E\u0442\u0430\u0301 \u0430\u0431\u043E \u0432\u0456\u0301\u0447\u043D\u0430 \u043C\u0435\u0440\u0437\u043B\u043E\u0442\u0430 \u2014 \u0447\u0430\u0441\u0442\u0438\u043D\u0430 \u043A\u0440\u0456\u043E\u043B\u0456\u0442\u043E\u0437\u043E\u043D\u0438, \u0434\u0435 \u043F\u043E\u0440\u043E\u0434\u0438 \u043C\u0430\u044E\u0442\u044C \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u0443, \u043D\u0438\u0436\u0447\u0443 \u0437\u0430 0 \u00B0C \u0456 \u043C\u0456\u0441\u0442\u044F\u0442\u044C \u043F\u0456\u0434\u0437\u0435\u043C\u043D\u0438\u0439 \u043B\u0456\u0434. \u0427\u0430\u0441 \u0456\u0441\u043D\u0443\u0432\u0430\u043D\u043D\u044F \u2014 \u0432\u0456\u0434 \u0434\u0435\u043A\u0456\u043B\u044C\u043A\u043E\u0445 \u0440\u043E\u043A\u0456\u0432 \u0434\u043E \u0441\u043E\u0442\u0435\u043D\u044C \u0442\u0438\u0441\u044F\u0447 \u0440\u043E\u043A\u0456\u0432. \u041F\u043E\u0448\u0438\u0440\u0435\u043D\u043D\u044F \u2014 \u0432\u0456\u0434 \u043E\u0441\u0442\u0440\u0456\u0432\u043D\u043E\u0433\u043E \u0434\u043E \u0441\u0443\u0446\u0456\u043B\u044C\u043D\u043E\u0433\u043E. \u041F\u043E\u0442\u0443\u0436\u043D\u0456\u0441\u0442\u044C \u0432\u0456\u0434 \u0434\u0435\u043A\u0456\u043B\u044C\u043A\u043E\u0445 \u043C\u0435\u0442\u0440\u0456\u0432 \u0434\u043E 1500 \u043C \u0456 \u0431\u0456\u043B\u044C\u0448\u0435 (\u0432 \u0433\u043E\u0440\u0430\u0445). \u042F\u0432\u0438\u0449\u0435 \u0431\u0430\u0433\u0430\u0442\u043E\u0440\u0456\u0447\u043D\u043E\u0457 \u043C\u0435\u0440\u0437\u043B\u043E\u0442\u0438 \u0437\u043C\u0456\u043D\u044E\u0454\u0442\u044C\u0441\u044F \u0440\u0430\u0437\u043E\u043C \u0437\u0456 \u0437\u043C\u0456\u043D\u043E\u044E \u0444\u0456\u0437\u0438\u043A\u043E-\u0433\u0435\u043E\u0433\u0440\u0430\u0444\u0456\u0447\u043D\u043E\u0433\u043E \u0441\u0435\u0440\u0435\u0434\u043E\u0432\u0438\u0449\u0430."@uk .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Melnikov_Permafrost_Institute> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Gravel> .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Zygomycota> .
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<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Talamh at\u00E1 oighrithe go buan i r\u00E9igi\u00FAin an-fhuara an Domhain. Go domhain faoina bhun t\u00E1 talamh neamhoighrithe, agus os a chionn ciseal gn\u00EDomhach a reonn sa samhradh is a athoighr\u00EDonn sa bhf\u00F3mhar. Gineann an t-oighri\u00FA s\u00EDos \u00F3n dromchla gach geimhreadh br\u00FA ar na cisil neamhoighrithe uisceluchtaithe den chrios gn\u00EDomhach seo, agus uaireanta is f\u00E9idir go bhfuascla\u00EDtear an br\u00FA seo tr\u00ED scoilteanna sa chiseal dromchlach oighrithe. Is m\u00F3r an fhadhb \u00E9 seo do th\u00F3g\u00E1il b\u00F3ithre, foirgneamh is p\u00EDobl\u00EDnte. Nuair a th\u00F3gtar an f\u00E1sra inslithe chun si\u00FAil i r\u00E9igi\u00FAin sh\u00EDorsioctha, d\u00E9anann s\u00E9 sin an crios gn\u00EDomhach n\u00EDos doimhne tr\u00ED le\u00E1 na tal\u00FAn s\u00EDorshioctha, agus tugann s\u00E9 faoi ag an dromchla."@ga .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Fauna> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"Il termine inglese permafrost (pron. /\u02C8p\u0259\u02D0m\u0259fr\u0252st/; composto di perma(nent), \"permanente\", e frost, \"gelato\"), in italiano permagelo, designa un terreno tipico delle regioni fredde ad esempio dell'estremo Nord Europa, della Siberia e dell'America settentrionale dove il suolo \u00E8 perennemente ghiacciato (non necessariamente con presenza di masse di acqua congelata)."@it .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Storflaket> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/classificationSystem>	<http://dbpedia.org/resource/International_Permafrost_Association> .
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<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://nl.dbpedia.org/resource/Permafrost> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://id.dbpedia.org/resource/Ibun_abadi> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:Commons_category> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Global_warming> .
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<http://dbpedia.org/resource/Permafrost>	<http://xmlns.com/foaf/0.1/isPrimaryTopicOf>	<http://en.wikipedia.org/wiki/Permafrost> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Canada> .
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<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://fr.dbpedia.org/resource/Perg\u00E9lisol> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Estonians> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://sco.dbpedia.org/resource/Permafrost> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Last_Glacial_Maximum> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://simple.dbpedia.org/resource/Permafrost> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Category:Periglacial_landforms> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/United_States_Geological_Survey_Library> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://tr.dbpedia.org/resource/Donmu\u015F_toprak> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Pithovirus> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#label>	"\u0411\u0430\u0433\u0430\u0442\u043E\u0440\u0456\u0447\u043D\u0430 \u043C\u0435\u0440\u0437\u043B\u043E\u0442\u0430"@uk .
<http://dbpedia.org/resource/Permafrost>	<http://purl.org/dc/terms/subject>	<http://dbpedia.org/resource/Category:Periglacial_landforms> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Permafrost (ingelesezko perma-, permanent, \"betiere\" + frost, \"antzigar\"/\"izotzaldi\") udan izoztuta mantentzen den lurzoruari deritzo, gutxienez bi urtez iraun duena. Lurzoru mota hau ohikoa da Siberia, Alaska eta Kanada iparraldean. Hedaduraz, Artikoko lurraldeetako lur beti izoztuari ere deritzo."@eu .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/imageSize>	"250"^^<http://www.w3.org/2001/XMLSchema#integer> .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Southern_Ocean> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Water> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Ice_sheet> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Category:Pedology> .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Yedoma> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"Permafrost, vanuit het Russisch soms ook merzlota (\"bevroren grond\") genoemd, is het verschijnsel dat in bepaalde gebieden nabij de polen en in het hooggebergte de ondergrond nooit helemaal ontdooit."@nl .
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<http://dbpedia.org/resource/Permafrost>	<http://purl.org/linguistics/gold/hypernym>	<http://dbpedia.org/resource/Soil> .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Mount_Kilimanjaro> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/New_Jersey> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Geothermal_gradient> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Effects_of_climate_change> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://www.wikidata.org/entity/Q179918> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"El permafrost\u200B (ocasionalmente traducido como permahielo, gelisuelo,\u200B permagel o permacongelamiento)\u200B es la capa de suelo permanentemente congelado \u2014pero no permanentemente cubierto de hielo o nieve\u2014 de las regiones muy fr\u00EDas o periglaciares, como la tundra. Puede encontrarse en \u00E1reas circumpolares de Canad\u00E1, Alaska, Groenlandia, Siberia, T\u00EDbet, Noruega y en varias islas del oc\u00E9ano Atl\u00E1ntico sur como las islas Georgias del Sur y las islas Sandwich del Sur.[cita requerida]"@es .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/File:Massive_ice_-_retrogressive_thaw_slump_-_Herschel_Island.png> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://eo.dbpedia.org/resource/\u0108iamfrosta_grundo> .
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<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"O permafrost ou pergelissolo (em portugu\u00EAs) \u00E9 uma camada do subsolo da crosta terrestre que est\u00E1 permanentemente congelada. A maior parte est\u00E1 localizada no hemisf\u00E9rio norte, concentrando-se, principalmente, na regi\u00E3o do \u00C1rtico, sobretudo em partes da R\u00FAssia (Sib\u00E9ria), Estados Unidos (Alasca), Canad\u00E1 e Dinamarca (Groenl\u00E2ndia)."@pt .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://it.dbpedia.org/resource/Permafrost> .
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<http://dbpedia.org/resource/Permafrost>	<http://purl.org/dc/terms/subject>	<http://dbpedia.org/resource/Category:Geography_of_the_Arctic> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Siberian> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Greenhouse_gas_emissions> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Southern_hemisphere> .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"Permafrost (t\u00E9\u017E v\u011B\u010Dn\u011B nebo dlouhodob\u011B zmrzl\u00E1 p\u016Fda, pergelisol) je hornina, nebo p\u016Fda, jej\u00ED\u017E teplota je po dobu dvou \u010Di v\u00EDce let ni\u017E\u0161\u00ED ne\u017E 0 \u00B0C. Voda v takov\u00E9 p\u016Fd\u011B je zmrzl\u00E1 a tvo\u0159\u00ED spolu s \u010D\u00E1ste\u010Dkami p\u00EDsku, hl\u00EDny a kamen\u00ED tvrdou krustu. Permafrost je sou\u010D\u00E1st\u00ED zemsk\u00E9 kryosf\u00E9ry a zab\u00EDr\u00E1 p\u0159ibli\u017En\u011B 11 % zemsk\u00E9ho povrchu a 25 % povrchu severn\u00ED polokoule. Term\u00EDn permafrost vznikl slou\u010Den\u00EDm anglick\u00FDch slov \u201Epermanent\u201D a \u201Efrost(y)\u201D (trval\u00FD a zmrzl\u00FD). Mocnost permafrostu dosahuje a\u017E n\u011Bkolika stovek metr\u016F, promrz\u00E1 tedy nejenom p\u016Fda, ale i skaln\u00ED podlo\u017E\u00ED. Nejhlub\u0161\u00ED zn\u00E1m\u00FD permafrost je na Sibi\u0159i a sah\u00E1 do hloubky cca 1500 m. V n\u011Bkter\u00FDch p\u0159\u00EDpadech se permafrost nach\u00E1z\u00ED pod nezamrzlou p\u016Fdou a v to v r\u016Fzn\u00E9 hloubce. Permafrost obsahuje velk\u00E9 mno\u017Estv\u00ED rozlo\u017Een\u00E9 biomasy. S postupn\u00FDm odt\u00E1v\u00E1n\u00EDm permafrostu se do atmosf\u00E9ry Zem\u011B uvol\u0148uj\u00ED plyny jako metan a oxid uhli\u010Dit\u00FD, co\u017E v\u00FDznamn\u011B umoc\u0148uje sklen\u00EDkov\u00FD efekt v atmosf\u00E9\u0159e na\u0161\u00ED planety a tedy i glob\u00E1ln\u00ED oteplov\u00E1n\u00ED. V oblastech tundry a tajgy svrchn\u00ED \u010D\u00E1st permafrostu p\u0159es l\u00E9to pravideln\u011B taje. Tato \u010D\u00E1st permafrostu se naz\u00FDv\u00E1 aktivn\u00ED vrstva a mohou na n\u00ED r\u016Fst rostliny. V situaci, kdy je podlo\u017E\u00ED st\u00E1le zmrzl\u00E9, ale aktivn\u00ED vrstva taje, mohou vznikat zvl\u00E1\u0161tn\u00ED povrchov\u00E9 geomorfologick\u00E9 jevy jako nap\u0159. opil\u00FD les, , , pingo, , apod. Permafrost se tak\u00E9 m\u016F\u017Ee vyskytovat pod mo\u0159skou hladinou. Po posledn\u00ED dob\u011B ledov\u00E9 byl takov\u00FD permafrost zatopen zvy\u0161uj\u00EDc\u00ED se hladinou oce\u00E1nu, ale z\u00E1rove\u0148 teplota takov\u00E9ho oce\u00E1nu dodnes nen\u00ED natolik vysok\u00E1, aby zp\u016Fsobila rozt\u00E1t\u00ED dan\u00E9ho permafrostu. Jedn\u00E1 se o \u010D\u00E1st Severn\u00EDho ledov\u00E9ho oce\u00E1nu. S postupn\u00FDm oh\u0159evem oce\u00E1n\u016F v\u0161ak i tento permafrost za\u010Dal t\u00E1t a vypou\u0161t\u011Bt z\u00E1soby sklen\u00EDkov\u00FDch plyn\u016F. Permafrost se tak\u00E9 nach\u00E1z\u00ED na jin\u00FDch planet\u00E1ch a vesm\u00EDrn\u00FDch objektech. Lze ho identifikovat t\u0159eba na Marsu \u010Di na M\u011Bs\u00EDci."@cs .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"\u591A\u5E74\u51CD\u571F\uFF08\u82F1\u8A9E\uFF1APermafrost\uFF09\u662F\u4E00\u500B\u5730\u8CEA\u5B78\u540D\u8A5E\uFF0C\u6307\u6EAB\u5EA6\u57280\u00B0C\u6216\u4F4E\u65BC0\u00B0C\uFF0C\u4E14\u81F3\u5C11\u9023\u7E8C\u51CD\u7D50\u5169\u5E74\u7684\u5CA9\u571F\u5C64\u3002"@zh .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"Le perg\u00E9lisol, parfois d\u00E9sign\u00E9 par le terme anglais permafrost, est la partie d'un cryosol gel\u00E9e en permanence, au moins pendant deux ans, et de ce fait imperm\u00E9able. Le perg\u00E9lisol existe dans les hautes latitudes (perg\u00E9lisol polaire) mais aussi dans les hautes altitudes (perg\u00E9lisol alpin). Il couvre un cinqui\u00E8me de la surface \u00E9merg\u00E9e, dont 90 % du Groenland, 80 % de l'Alaska, 50 % du Canada et de la Russie (plus particuli\u00E8rement dans sa partie sib\u00E9rienne). Le perg\u00E9lisol polaire en Sib\u00E9rie est plut\u00F4t un perg\u00E9lisol continu au-del\u00E0 du 60e degr\u00E9 de latitude. Le perg\u00E9lisol alpin est plus sporadique \u00E0 cause du terrain coup\u00E9 avec des expositions tr\u00E8s diverses. Il est constitu\u00E9 thermiquement de trois couches : la premi\u00E8re dite \u00AB active \u00BB d\u00E9g\u00E8le en \u00E9t\u00E9 et peut atteindre jusque deux \u00E0 trois m\u00E8tres ; la seconde, soumise \u00E0 des fluctuations saisonni\u00E8res mais constamment sous le point de cong\u00E9lation, constitue la partie du perg\u00E9lisol stricto sensu et s'\u00E9tend \u00E0 une profondeur de 10 \u00E0 15 m\u00E8tres ; la troisi\u00E8me peut atteindre plusieurs centaines de m\u00E8tres, voire d\u00E9passer le millier de m\u00E8tres (en Yakoutie), ne conna\u00EEt pas de variation saisonni\u00E8re de temp\u00E9rature et est constamment congel\u00E9e. La temp\u00E9rature s'y \u00E9l\u00E8ve vers le bas sous l'influence des flux g\u00E9othermique et atteint 0 \u00B0C \u00E0 la limite basse du perg\u00E9lisol. Dans le perg\u00E9lisol, la glace peut obturer les pores du sol ou constituer des corps de glace de diff\u00E9rentes gen\u00E8ses. Les r\u00E9gions subarctiques sont en outre, du fait du caract\u00E8re imperm\u00E9able de la glace, des zones humides anoxiques de marais et de tourbi\u00E8re o\u00F9 ont pu se d\u00E9velopper des micro-organismes m\u00E9thanog\u00E8nes. Du m\u00E9thane se trouve par ailleurs dans les lacs de thermokarst ou alass. Les formations, persistance ou disparition du perg\u00E9lisol, et son \u00E9paisseur sont tr\u00E8s \u00E9troitement li\u00E9es aux changements climatiques. C'est pourquoi le perg\u00E9lisol est \u00E9tudi\u00E9 en tant qu'indicateur du r\u00E9chauffement climatique par un r\u00E9seau mondial de chercheurs s'appuyant sur des sondages, des mesures de temp\u00E9rature et un suivi satellitaire, \u00E0 l'initiative du r\u00E9seau mondial de surveillance terrestre du perg\u00E9lisol. Le d\u00E9gel rapide pourrait augmenter consid\u00E9rablement les quantit\u00E9s de gaz \u00E0 effet de serre \u00E9mises par les plantes et animaux anciens gel\u00E9s."@fr .
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<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Il termine inglese permafrost (pron. /\u02C8p\u0259\u02D0m\u0259fr\u0252st/; composto di perma(nent), \"permanente\", e frost, \"gelato\"), in italiano permagelo, designa un terreno tipico delle regioni fredde ad esempio dell'estremo Nord Europa, della Siberia e dell'America settentrionale dove il suolo \u00E8 perennemente ghiacciato (non necessariamente con presenza di masse di acqua congelata)."@it .
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<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"\u03A9\u03C2 \u03BC\u03CC\u03BD\u03B9\u03BC\u03BF \u03C0\u03B1\u03B3\u03C9\u03BC\u03AD\u03BD\u03BF \u03AD\u03B4\u03B1\u03C6\u03BF\u03C2, \u03B3\u03BD\u03C9\u03C3\u03C4\u03CC \u03BA\u03B1\u03B9 \u03C9\u03C2 \u03C0\u03AD\u03C1\u03BC\u03B1\u03C6\u03C1\u03BF\u03C3\u03C4, \u03BF\u03C1\u03AF\u03B6\u03B5\u03C4\u03B1\u03B9 \u03C4\u03BF \u03C0\u03B1\u03B3\u03C9\u03BC\u03AD\u03BD\u03BF \u03AD\u03B4\u03B1\u03C6\u03BF\u03C2, \u03AF\u03B6\u03B7\u03BC\u03B1 \u03AE \u03C0\u03AD\u03C4\u03C1\u03C9\u03BC\u03B1. \u0397 \u03BA\u03B1\u03C4\u03AC\u03C4\u03B1\u03BE\u03B7 \u03C4\u03BF\u03C5 \u03B5\u03B4\u03AC\u03C6\u03BF\u03C5\u03C2 \u03C9\u03C2 \u03BC\u03CC\u03BD\u03B9\u03BC\u03B1 \u03C0\u03B1\u03B3\u03C9\u03BC\u03AD\u03BD\u03BF \u03C3\u03C7\u03B5\u03C4\u03AF\u03B6\u03B5\u03C4\u03B1\u03B9 \u03B1\u03C0\u03BF\u03BA\u03BB\u03B5\u03B9\u03C3\u03C4\u03B9\u03BA\u03AC \u03BC\u03B5 \u03C4\u03B7 \u03B8\u03B5\u03C1\u03BC\u03BF\u03BA\u03C1\u03B1\u03C3\u03AF\u03B1, \u03CC\u03C7\u03B9 \u03BC\u03B5 \u03C4\u03B7\u03BD \u03C5\u03B3\u03C1\u03B1\u03C3\u03AF\u03B1 \u03AE \u03BF\u03C0\u03BF\u03B9\u03B1\u03C3\u03B4\u03AE\u03C0\u03BF\u03C4\u03B5 \u03BC\u03BF\u03C1\u03C6\u03AE\u03C2 . \u0393\u03B9\u03B1 \u03BD\u03B1 \u03B8\u03B5\u03C9\u03C1\u03B7\u03B8\u03B5\u03AF \u03BC\u03CC\u03BD\u03B9\u03BC\u03B1 \u03C0\u03B1\u03B3\u03C9\u03BC\u03AD\u03BD\u03BF, \u03C4\u03BF \u03AD\u03B4\u03B1\u03C6\u03BF\u03C2 \u03B8\u03B1 \u03C0\u03C1\u03AD\u03C0\u03B5\u03B9 \u03BD\u03B1 \u03B2\u03C1\u03AF\u03C3\u03BA\u03B5\u03C4\u03B1\u03B9 \u03C3\u03B5 \u03B8\u03B5\u03C1\u03BC\u03BF\u03BA\u03C1\u03B1\u03C3\u03AF\u03B1 \u03BC\u03B9\u03BA\u03C1\u03CC\u03C4\u03B5\u03C1\u03B7 \u03AE \u03AF\u03C3\u03B7 \u03C4\u03C9\u03BD -2\u00B0C \u03B5\u03C0\u03AF \u03B4\u03CD\u03BF \u03C4\u03BF\u03C5\u03BB\u03AC\u03C7\u03B9\u03C3\u03C4\u03BF\u03BD \u03C7\u03C1\u03CC\u03BD\u03B9\u03B1. \u038C\u03C0\u03C9\u03C2 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03C6\u03C5\u03C3\u03B9\u03BA\u03CC, \u03C4\u03AD\u03C4\u03BF\u03B9\u03BF\u03C5 \u03B5\u03AF\u03B4\u03BF\u03C5\u03C2 \u03AD\u03B4\u03B1\u03C6\u03BF\u03C2 \u03BC\u03C0\u03BF\u03C1\u03B5\u03AF \u03BD\u03B1 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03C7\u03B9\u03BB\u03B9\u03AC\u03B4\u03C9\u03BD \u03B5\u03C4\u03CE\u03BD \u03C3\u03B5 \u03BF\u03C1\u03B9\u03C3\u03BC\u03AD\u03BD\u03B5\u03C2 \u03C0\u03B5\u03C1\u03B9\u03BF\u03C7\u03AD\u03C2 \u03C4\u03BF\u03C5 \u03C0\u03BB\u03B1\u03BD\u03AE\u03C4\u03B7."@el .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"\u0108iamfrosta grundo - anka\u016D la\u016D anglalingva pa\u016Dsa\u0135o permafrosto a\u016D permafrosta grundo - estas tero, en kiu temperaturo de tavoloj de la tero de certa profundo dum multaj jaroj (kaj vintre kaj somere) estas malpli ol 0 \u00B0C. \u0108ar tero plejofte enhavas akvon multjare frosti\u011Dinta tero kutime enhavas glacion, kaj do estas ekde certa profundo frosti\u011Dinta. \u0108iamfrostareoj - do insuloj kun da\u016Dre frosti\u011Dinta grundo - ekzistas anka\u016D en la altmontaraj regionoj, kiel ekzemple en la Alpoj. Ili ekestis dum la Glaciepoko, kiam la grundo frosti\u011Dis kelkloke \u011Dis 1000 metroj da profundeco."@eo .
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<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Le perg\u00E9lisol, parfois d\u00E9sign\u00E9 par le terme anglais permafrost, est la partie d'un cryosol gel\u00E9e en permanence, au moins pendant deux ans, et de ce fait imperm\u00E9able. Le perg\u00E9lisol existe dans les hautes latitudes (perg\u00E9lisol polaire) mais aussi dans les hautes altitudes (perg\u00E9lisol alpin). Il couvre un cinqui\u00E8me de la surface \u00E9merg\u00E9e, dont 90 % du Groenland, 80 % de l'Alaska, 50 % du Canada et de la Russie (plus particuli\u00E8rement dans sa partie sib\u00E9rienne). Le perg\u00E9lisol polaire en Sib\u00E9rie est plut\u00F4t un perg\u00E9lisol continu au-del\u00E0 du 60e degr\u00E9 de latitude. Le perg\u00E9lisol alpin est plus sporadique \u00E0 cause du terrain coup\u00E9 avec des expositions tr\u00E8s diverses."@fr .
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<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#label>	"Talamh sh\u00EDorshioctha"@ga .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"\u591A\u5E74\u51CD\u571F\uFF08\u82F1\u8A9E\uFF1APermafrost\uFF09\u662F\u4E00\u500B\u5730\u8CEA\u5B78\u540D\u8A5E\uFF0C\u6307\u6EAB\u5EA6\u57280\u00B0C\u6216\u4F4E\u65BC0\u00B0C\uFF0C\u4E14\u81F3\u5C11\u9023\u7E8C\u51CD\u7D50\u5169\u5E74\u7684\u5CA9\u571F\u5C64\u3002"@zh .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Drunken_trees> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Wieczna lub wieloletnia zmarzlina, zwana te\u017C czasem wieczn\u0105 marz\u0142oci\u0105 lub marz\u0142oci\u0105 trwa\u0142\u0105 lub zlodowaceniem podziemnym \u2013 zjawisko trwa\u0142ego (minimum dwa kolejne lata) utrzymywania si\u0119 cz\u0119\u015Bci skorupy ziemskiej w temperaturze poni\u017Cej punktu zamarzania wody niezale\u017Cnie od pory roku. Powstaje w warunkach suchego, zimnego klimatu (o \u015Bredniej temperaturze powietrza poni\u017Cej \u221211 \u00B0C). Obejmuje oko\u0142o 80% Alaski, wi\u0119kszo\u015B\u0107 p\u00F3\u0142nocnej Kanady i 65% Syberii (ci\u0105g\u0142a zmarzlina wyst\u0119puje prawie wy\u0142\u0105cznie we wschodniej Syberii, w zachodniej jest obecna tylko na p\u00F3\u0142nocnym wybrze\u017Cu oceanu). Ci\u0105g\u0142a zmarzlina si\u0119ga a\u017C do p\u00F3\u0142nocnej Mongolii, punktowo wyst\u0119puje te\u017C w G\u00F3rach Skandynawskich i na Grenlandii. Natomiast nieci\u0105g\u0142e zmarzliny zajmuj\u0105 tak\u017Ce wi\u0119kszo\u015B\u0107 Tybetu, s\u0105 te\u017C znane z Alp. Wieczn\u0105 zmarzlin\u0119 odkryto r\u00F3"@pl .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"O permafrost ou pergelissolo (em portugu\u00EAs) \u00E9 uma camada do subsolo da crosta terrestre que est\u00E1 permanentemente congelada. A maior parte est\u00E1 localizada no hemisf\u00E9rio norte, concentrando-se, principalmente, na regi\u00E3o do \u00C1rtico, sobretudo em partes da R\u00FAssia (Sib\u00E9ria), Estados Unidos (Alasca), Canad\u00E1 e Dinamarca (Groenl\u00E2ndia)."@pt .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Mars_Reconnaissance_Orbiter> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"Permafrost (ingelesezko perma-, permanent, \"betiere\" + frost, \"antzigar\"/\"izotzaldi\") udan izoztuta mantentzen den lurzoruari deritzo, gutxienez bi urtez iraun duena. Lurzoru mota hau ohikoa da Siberia, Alaska eta Kanada iparraldean. Hedaduraz, Artikoko lurraldeetako lur beti izoztuari ere deritzo. Hiru motatakoa izan daiteke: jarraitua, lurpeko 0,5 m-tik 500 m-ra bitarteko parteak izozturik irauten duena; zatikakoa, permafrostaren barnean izoztu gabeko parte batzuk dituena; eta permafrostaren barnean parte gehienak izoztu gabe irauten duena. Klimak, tenperaturak, ezaugarri eta landarediak eragiten dute permafrosten sorrera eta bilakaera. Lurrazalaren % 25 inguru hartzen du permafrostak, hormategiak barne. Azken hamarkada eta urteetan, permafrosta gero eta lasterrago ari da urtzen klima aldaketa dela eta. Permafrostak metano eta karbono kopuru handiak biltegiratzen dituenez, urtzearen ondorioz emisioak ugari askatzen ari dira atmosferara eta, beraz, berotegi efektuko gasak. 2019an, 1.600.000 megatona karbono zeuden permafrostean; atmosferan barreiatuta, berriz, 870.000 megatona."@eu .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageExternalLink>	<http://www.ipa-permafrost.org> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Silene_stenophylla> .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"\u0108iamfrosta grundo - anka\u016D la\u016D anglalingva pa\u016Dsa\u0135o permafrosto a\u016D permafrosta grundo - estas tero, en kiu temperaturo de tavoloj de la tero de certa profundo dum multaj jaroj (kaj vintre kaj somere) estas malpli ol 0 \u00B0C. \u0108ar tero plejofte enhavas akvon multjare frosti\u011Dinta tero kutime enhavas glacion, kaj do estas ekde certa profundo frosti\u011Dinta. Grandaj \u0109iamfrostareoj trovi\u011Das sur la tero en regionoj kun arkta kaj antarkta influo. La senarbaj tundroj de nia tero ofte estas \u0109iamfrostregionoj. La\u016D geografia vidpunkto temas pri grandaj partoj de norda Kanado, Alasko, Gronlando kaj orienta Siberio. Suden kelkaj \u0109iamfrostregionoj atingas Mongolion. \u0108iamfrosto diversprofunde enpenetras la grundon: En norda Ruslando la \u0109iamfrosto atingas grundprofundon de 1.450 metroj, en Skandinavio nur de 20 metroj. \u0108iamfrostareoj - do insuloj kun da\u016Dre frosti\u011Dinta grundo - ekzistas anka\u016D en la altmontaraj regionoj, kiel ekzemple en la Alpoj. Ili ekestis dum la Glaciepoko, kiam la grundo frosti\u011Dis kelkloke \u011Dis 1000 metroj da profundeco. \u0108iamfrostaj grundoj en somero povas supra\u0135e degeli; la ofte atingas profundon de pluraj metroj, dum la grundo sub \u011Di restas frosti\u011Dinta."@eo .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"Dalam geologi, ibun abadi (bahasa Inggris: permafrost) atau tanah beku abadi adalah lapisan tanah beku yang berada di bawah suhu 0 \u00B0C selama beberapa tahun. Ibun abadi terbentuk dari es-es yang menggenggam berbagai macam tanah, pasir, dan bebatuan. Ibun abadi umumnya terletak di lintang tinggi, yaitu dekat kutub utara dan selatan. Ibun abadi biasa terbentuk dalam iklim dengan suhu udara rata-rata tahunan kurang dari titik beku air."@in .
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<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Permafrost bezeichnet in den Geowissenschaften einen Untergrund, dessen Temperatur f\u00FCr mindestens zwei Jahre ununterbrochen (perennierend) unter 0 \u00B0C liegt. Bei dem Untergrund kann es sich um Boden, Lockergestein oder Festgestein handeln. Permafrost tritt abh\u00E4ngig von den klimatischen Bedingungen mit unterschiedlicher M\u00E4chtigkeit und Tiefe auf; er kann mehrere hundert Meter tief reichen und besitzt dann meist ein Alter von vielen tausend Jahren. Die gr\u00F6\u00DFte Ausdehnung haben Permafrostb\u00F6den unter den Eisschilden und in den K\u00E4ltew\u00FCsten der beiden Polargebiete sowie in den angrenzenden hochkontinentalen Klimaten der (n\u00F6rdlichen) borealen Zone. Dort kann der Boden \u00FCber dem Permafrost im Sommer auftauen (siehe Auftauboden). Weitere gro\u00DFfl\u00E4chige Bereiche befinden sich in der Massenerhebung Hochas"@de .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"Permafrost definieras som ett tillst\u00E5nd d\u00E4r temperaturen i marken inte n\u00E5r upp \u00F6ver noll grader under minst tv\u00E5 \u00E5r i rad. Ovanp\u00E5 permafrosten finns ett aktivt lager som tinar om v\u00E5ren och sommaren och fryser igen under vintern. Det aktiva lagrets tjocklek beror p\u00E5 klimatet och markens v\u00E4rmeledande egenskaper men \u00E4r p\u00E5 de flesta platser mellan en halvmeter och ett par meter. Permafrostens tjocklek beror bland annat p\u00E5 det nuvarande och det historiska klimatet. I omr\u00E5den l\u00E5ngt norrut som har haft ett kallt klimat v\u00E4ldigt l\u00E4nge, exempelvis norra Sibirien, kan permafrosten vara flera hundra meter tjock. Permafrostomr\u00E5den finns i cirka en fj\u00E4rdedel av landmassan p\u00E5 norra halvklotet, framf\u00F6r allt i Ryssland, Kanada och Alaska men \u00E4ven i Skandinavien, Gr\u00F6nland, Mongoliet, Himalaya och Alperna. Det finns permafrost p\u00E5 alla kontinenter utom i Australien. I Sverige f\u00F6rekommer permafrost i vissa delar av fj\u00E4llkedjan, exempelvis runt Kebnekaise, och i s\u00E5 kallade palsmyrar i nordligaste Sverige. I myrar bildas och skyddas permafrosten av att torven har speciella v\u00E4rmeledande egenskaper. N\u00E4r markytan \u00E4r varm p\u00E5 sommaren \u00E4r torven oftast mycket torr och leder d\u00E4rf\u00F6r v\u00E4rme d\u00E5ligt, men p\u00E5 h\u00F6sten \u00F6kar fukten i torven och n\u00E4r torven fryser \u00F6kar v\u00E4rmeledningsf\u00F6rm\u00E5gan. P\u00E5 s\u00E5 s\u00E4tt kyls marken av effektivt p\u00E5 vintern, men den v\u00E4rms inte lika effektivt p\u00E5 sommaren. Permafrost inneb\u00E4r en utmaning n\u00E4r man ska bygga hus. Uppv\u00E4rmningen av huset kan f\u00E5 permafrosten att tina under huset s\u00E5 att huset sjunker. Man kan l\u00F6sa det genom att bygga huset p\u00E5 pelare (antingen s\u00E5 att luften n\u00E5r under huset, eller p\u00E5 pelare som n\u00E5r ner till stabil permafrost, runt 15 meter ned), eller genom att l\u00E4gga ett tjockt stabilt stenlager som isolerar huset ned\u00E5t. N\u00E4r man ska ha vattenledningar brukar de l\u00E4ggas ovan marken, f\u00F6r att de kan tina upp permafrosten annars och f\u00F6r att det \u00E4r sv\u00E5rt att gr\u00E4va i frosten. V\u00E4gar blir l\u00E4tt d\u00E5liga i permafrost. P\u00E5 Svalbard \u00E4r marken, utom en liten del av det \u00F6versta lagret sommartid, fruset ned till mellan 100 meters och 300 meters djup. Minst tjocklek \u00E4r det i l\u00E5gl\u00E4nta l\u00E4gen och invid bergens f\u00F6tter. S\u00E5ledes har till exempel i Josefine- och Sofiegruvorna i Ny-\u00C5lesund m\u00E4tts permafrost ned till 130\u2013140 respektive 150 meter och i Sveagruva 320 meter. Den sibiriska staden Jakutsk \u00E4r den st\u00F6rsta staden som \u00E4r byggd p\u00E5 permafrost."@sv .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Europe> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Permafrost (t\u00E9\u017E v\u011B\u010Dn\u011B nebo dlouhodob\u011B zmrzl\u00E1 p\u016Fda, pergelisol) je hornina, nebo p\u016Fda, jej\u00ED\u017E teplota je po dobu dvou \u010Di v\u00EDce let ni\u017E\u0161\u00ED ne\u017E 0 \u00B0C. Voda v takov\u00E9 p\u016Fd\u011B je zmrzl\u00E1 a tvo\u0159\u00ED spolu s \u010D\u00E1ste\u010Dkami p\u00EDsku, hl\u00EDny a kamen\u00ED tvrdou krustu. Permafrost je sou\u010D\u00E1st\u00ED zemsk\u00E9 kryosf\u00E9ry a zab\u00EDr\u00E1 p\u0159ibli\u017En\u011B 11 % zemsk\u00E9ho povrchu a 25 % povrchu severn\u00ED polokoule. Term\u00EDn permafrost vznikl slou\u010Den\u00EDm anglick\u00FDch slov \u201Epermanent\u201D a \u201Efrost(y)\u201D (trval\u00FD a zmrzl\u00FD). Permafrost se tak\u00E9 nach\u00E1z\u00ED na jin\u00FDch planet\u00E1ch a vesm\u00EDrn\u00FDch objektech. Lze ho identifikovat t\u0159eba na Marsu \u010Di na M\u011Bs\u00EDci."@cs .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://la.dbpedia.org/resource/Congelatio_aeterna> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/File:Vertical_Temperature_Profile_in_Permafrost_(English_Text).jpg> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Methane> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Climate> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Relict_(geology)> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Trans-Alaska_Pipeline> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Frost_heaving> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#label>	"\u041C\u043D\u043E\u0433\u043E\u043B\u0435\u0442\u043D\u044F\u044F \u043C\u0435\u0440\u0437\u043B\u043E\u0442\u0430"@ru .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Fort_Simpson> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:Periglacial_environment> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Tuktoyaktuk> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#label>	"Permafrost"@es .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:Use_dmy_dates> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Iowa> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Heat_pipe> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Drakensberg> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageExternalLink>	<https://www.youtube.com/watch%3Fv=lxixy1u8GjY> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/imageCaption>	"Map showing extent and types of permafrost in the Northern Hemisphere"@en .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Sediment> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:Val> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Pingo> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Soil> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Ambarnaya> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Carbon_sink> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"En geologia, permagel o pergelisol (en angl\u00E8s, permafrost, de perma-, permanent i frost, gelat) s\u00F3n aquelles capes de s\u00F2l, roca o terra que romanen per sota del punt de congelaci\u00F3 de l'aigua (0 \u00B0C) durant com a m\u00EDnim dos anys seguits. El permagel est\u00E0 situat entre el , la capa superficial activa que respon a les oscil\u00B7lacions del clima, i la roca profunda no gelada, m\u00E9s afectada pel flux geot\u00E8rmic que pel clima. Els s\u00F2ls es classifiquen com a permagel continu (90 a 100% de cobertura de la superf\u00EDcie amb permagel), discontinu (50 a 90%), espor\u00E0dic (10 a 50%), isolat (>10%) i sense permagel."@ca .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Eurasia> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#label>	"Permafrost"@eu .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Rock_(geology)> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#label>	"\u6C38\u4E45\u51CD\u571F"@ja .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Qinghai-Tibet_Plateau> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"\u062A\u0639\u0631\u0641 \u0627\u0644\u062A\u064F\u0631\u0628\u064E\u0629\u064F \u0627\u0644\u0635\u064E\u0651\u0642\u0650\u064A\u0639\u0650\u064A\u0651\u0629 Permafrost \u0628\u0623\u0646\u0647\u0627 \u0627\u0644\u0645\u0646\u0637\u0642\u0629 \u0627\u0644\u062A\u064A \u0645\u062A\u0648\u0633\u0637 \u062F\u0631\u062C\u0629 \u062D\u0631\u0627\u0631\u0629 \u0623\u0631\u0636\u0647\u0627 \u0627\u0644\u0633\u0646\u0648\u064A mean annual ground temperature MAGT \u0623\u0642\u0644 \u0645\u0646 \u0636\u063A\u0637 \u0646\u0642\u0637\u0629 \u0627\u0644\u0627\u0646\u0635\u0647\u0627\u0631 \u0639\u0644\u0649 \u0627\u0644\u0623\u0642\u0644 \u062E\u0644\u0627\u0644 \u0633\u0646\u062A\u0627\u0646 \u0639\u0644\u0649 \u0627\u0644\u062A\u0648\u0627\u0644\u064A. \u0648\u0647\u064A \u062A\u0642\u0627\u0628\u0644 \u0627\u0644\u0645\u0646\u0627\u0637\u0642 \u0627\u0644\u062A\u064A \u064A\u0643\u0648\u0646 \u0645\u062A\u0648\u0633\u0637 \u062F\u0631\u062C\u0629 \u062D\u0631\u0627\u0631\u0629 \u0627\u0644\u0647\u0648\u0627\u0621 mean annual air temperature MAAT \u0646\u0627\u0642\u0635 \u062F\u0631\u062C\u062A\u0627\u0646 \u0645\u0626\u0648\u064A\u0629 \u0623\u0648 \u0623\u0642\u0644"@ar .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://kk.dbpedia.org/resource/\u041C\u04D9\u04A3\u0433\u0456_\u0442\u043E\u04A3> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"\u03A9\u03C2 \u03BC\u03CC\u03BD\u03B9\u03BC\u03BF \u03C0\u03B1\u03B3\u03C9\u03BC\u03AD\u03BD\u03BF \u03AD\u03B4\u03B1\u03C6\u03BF\u03C2, \u03B3\u03BD\u03C9\u03C3\u03C4\u03CC \u03BA\u03B1\u03B9 \u03C9\u03C2 \u03C0\u03AD\u03C1\u03BC\u03B1\u03C6\u03C1\u03BF\u03C3\u03C4, \u03BF\u03C1\u03AF\u03B6\u03B5\u03C4\u03B1\u03B9 \u03C4\u03BF \u03C0\u03B1\u03B3\u03C9\u03BC\u03AD\u03BD\u03BF \u03AD\u03B4\u03B1\u03C6\u03BF\u03C2, \u03AF\u03B6\u03B7\u03BC\u03B1 \u03AE \u03C0\u03AD\u03C4\u03C1\u03C9\u03BC\u03B1. \u0397 \u03BA\u03B1\u03C4\u03AC\u03C4\u03B1\u03BE\u03B7 \u03C4\u03BF\u03C5 \u03B5\u03B4\u03AC\u03C6\u03BF\u03C5\u03C2 \u03C9\u03C2 \u03BC\u03CC\u03BD\u03B9\u03BC\u03B1 \u03C0\u03B1\u03B3\u03C9\u03BC\u03AD\u03BD\u03BF \u03C3\u03C7\u03B5\u03C4\u03AF\u03B6\u03B5\u03C4\u03B1\u03B9 \u03B1\u03C0\u03BF\u03BA\u03BB\u03B5\u03B9\u03C3\u03C4\u03B9\u03BA\u03AC \u03BC\u03B5 \u03C4\u03B7 \u03B8\u03B5\u03C1\u03BC\u03BF\u03BA\u03C1\u03B1\u03C3\u03AF\u03B1, \u03CC\u03C7\u03B9 \u03BC\u03B5 \u03C4\u03B7\u03BD \u03C5\u03B3\u03C1\u03B1\u03C3\u03AF\u03B1 \u03AE \u03BF\u03C0\u03BF\u03B9\u03B1\u03C3\u03B4\u03AE\u03C0\u03BF\u03C4\u03B5 \u03BC\u03BF\u03C1\u03C6\u03AE\u03C2 . \u0393\u03B9\u03B1 \u03BD\u03B1 \u03B8\u03B5\u03C9\u03C1\u03B7\u03B8\u03B5\u03AF \u03BC\u03CC\u03BD\u03B9\u03BC\u03B1 \u03C0\u03B1\u03B3\u03C9\u03BC\u03AD\u03BD\u03BF, \u03C4\u03BF \u03AD\u03B4\u03B1\u03C6\u03BF\u03C2 \u03B8\u03B1 \u03C0\u03C1\u03AD\u03C0\u03B5\u03B9 \u03BD\u03B1 \u03B2\u03C1\u03AF\u03C3\u03BA\u03B5\u03C4\u03B1\u03B9 \u03C3\u03B5 \u03B8\u03B5\u03C1\u03BC\u03BF\u03BA\u03C1\u03B1\u03C3\u03AF\u03B1 \u03BC\u03B9\u03BA\u03C1\u03CC\u03C4\u03B5\u03C1\u03B7 \u03AE \u03AF\u03C3\u03B7 \u03C4\u03C9\u03BD -2\u00B0C \u03B5\u03C0\u03AF \u03B4\u03CD\u03BF \u03C4\u03BF\u03C5\u03BB\u03AC\u03C7\u03B9\u03C3\u03C4\u03BF\u03BD \u03C7\u03C1\u03CC\u03BD\u03B9\u03B1. \u038C\u03C0\u03C9\u03C2 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03C6\u03C5\u03C3\u03B9\u03BA\u03CC, \u03C4\u03AD\u03C4\u03BF\u03B9\u03BF\u03C5 \u03B5\u03AF\u03B4\u03BF\u03C5\u03C2 \u03AD\u03B4\u03B1\u03C6\u03BF\u03C2 \u03BC\u03C0\u03BF\u03C1\u03B5\u03AF \u03BD\u03B1 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03C7\u03B9\u03BB\u03B9\u03AC\u03B4\u03C9\u03BD \u03B5\u03C4\u03CE\u03BD \u03C3\u03B5 \u03BF\u03C1\u03B9\u03C3\u03BC\u03AD\u03BD\u03B5\u03C2 \u03C0\u03B5\u03C1\u03B9\u03BF\u03C7\u03AD\u03C2 \u03C4\u03BF\u03C5 \u03C0\u03BB\u03B1\u03BD\u03AE\u03C4\u03B7. \u03A4\u03BF \u03BC\u03CC\u03BD\u03B9\u03BC\u03B1 \u03C0\u03B1\u03B3\u03C9\u03BC\u03AD\u03BD\u03BF \u03AD\u03B4\u03B1\u03C6\u03BF\u03C2 \u03C0\u03BF\u03C5 \u03AD\u03C7\u03B5\u03B9 \u03B1\u03C0\u03C9\u03BB\u03AD\u03C3\u03B5\u03B9 \u03C4\u03B7\u03BD \u03C5\u03B3\u03C1\u03B1\u03C3\u03AF\u03B1 \u03C4\u03BF\u03C5 \u03BA\u03B1\u03B9 \u03C3\u03C5\u03BD\u03B5\u03C0\u03CE\u03C2 \u03B4\u03B5\u03BD \u03C0\u03B5\u03C1\u03B9\u03AD\u03C7\u03B5\u03B9 \u03C0\u03AC\u03B3\u03BF, \u03BF\u03C1\u03AF\u03B6\u03B5\u03C4\u03B1\u03B9 \u03C9\u03C2 \u03BE\u03B7\u03C1\u03CC \u03BC\u03CC\u03BD\u03B9\u03BC\u03B1 \u03C0\u03B1\u03B3\u03C9\u03BC\u03AD\u03BD\u03BF \u03AD\u03B4\u03B1\u03C6\u03BF\u03C2. \u03A4\u03BF \u03BC\u03CC\u03BD\u03B9\u03BC\u03B1 \u03C0\u03B1\u03B3\u03C9\u03BC\u03AD\u03BD\u03BF \u03AD\u03B4\u03B1\u03C6\u03BF\u03C2 \u03B1\u03C0\u03B1\u03BD\u03C4\u03AC\u03C4\u03B1\u03B9 \u03C3\u03B5 \u03C3\u03B7\u03BC\u03B5\u03AF\u03B1 \u03BC\u03B5 \u03C8\u03C5\u03C7\u03C1\u03BF\u03CD\u03C2 \u03C7\u03B5\u03B9\u03BC\u03CE\u03BD\u03B5\u03C2 \u03BC\u03B5 \u03BB\u03AF\u03B3\u03BF \u03C7\u03B9\u03CC\u03BD\u03B9 \u03BA\u03B1\u03B9 \u03C3\u03C7\u03B5\u03C4\u03B9\u03BA\u03AC \u03BE\u03B7\u03C1\u03AC, \u03C8\u03C5\u03C7\u03C1\u03AC \u03BA\u03B1\u03B9 \u03C3\u03CD\u03BD\u03C4\u03BF\u03BC\u03B1 \u03BA\u03B1\u03BB\u03BF\u03BA\u03B1\u03AF\u03C1\u03B9\u03B1. \u03A4\u03AD\u03C4\u03BF\u03B9\u03BF\u03C2 \u03C4\u03CD\u03C0\u03BF\u03C2 \u03B5\u03B4\u03AC\u03C6\u03BF\u03C5\u03C2 \u03B1\u03C0\u03B1\u03BD\u03C4\u03AC\u03C4\u03B1\u03B9 \u03C3\u03C4\u03BF\u03BD \u03B1\u03C1\u03BA\u03C4\u03B9\u03BA\u03CC \u03BA\u03B1\u03B9 \u03C5\u03C0\u03BF\u03B1\u03C1\u03BA\u03C4\u03B9\u03BA\u03CC \u03BA\u03CD\u03BA\u03BB\u03BF \u03BA\u03B1\u03B9 \u03C3\u03C4\u03B7\u03BD \u0391\u03BD\u03C4\u03B1\u03C1\u03BA\u03C4\u03B9\u03BA\u03AE."@el .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/North_America> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Herschel_Island> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://hu.dbpedia.org/resource/Permafroszt> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"\u0411\u0430\u0433\u0430\u0442\u043E\u0440\u0456\u0301\u0447\u043D\u0430 \u043C\u0435\u0440\u0437\u043B\u043E\u0442\u0430\u0301 \u0430\u0431\u043E \u0432\u0456\u0301\u0447\u043D\u0430 \u043C\u0435\u0440\u0437\u043B\u043E\u0442\u0430 \u2014 \u0447\u0430\u0441\u0442\u0438\u043D\u0430 \u043A\u0440\u0456\u043E\u043B\u0456\u0442\u043E\u0437\u043E\u043D\u0438, \u0434\u0435 \u043F\u043E\u0440\u043E\u0434\u0438 \u043C\u0430\u044E\u0442\u044C \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u0443, \u043D\u0438\u0436\u0447\u0443 \u0437\u0430 0 \u00B0C \u0456 \u043C\u0456\u0441\u0442\u044F\u0442\u044C \u043F\u0456\u0434\u0437\u0435\u043C\u043D\u0438\u0439 \u043B\u0456\u0434. \u0427\u0430\u0441 \u0456\u0441\u043D\u0443\u0432\u0430\u043D\u043D\u044F \u2014 \u0432\u0456\u0434 \u0434\u0435\u043A\u0456\u043B\u044C\u043A\u043E\u0445 \u0440\u043E\u043A\u0456\u0432 \u0434\u043E \u0441\u043E\u0442\u0435\u043D\u044C \u0442\u0438\u0441\u044F\u0447 \u0440\u043E\u043A\u0456\u0432. \u041F\u043E\u0448\u0438\u0440\u0435\u043D\u043D\u044F \u2014 \u0432\u0456\u0434 \u043E\u0441\u0442\u0440\u0456\u0432\u043D\u043E\u0433\u043E \u0434\u043E \u0441\u0443\u0446\u0456\u043B\u044C\u043D\u043E\u0433\u043E. \u041F\u043E\u0442\u0443\u0436\u043D\u0456\u0441\u0442\u044C \u0432\u0456\u0434 \u0434\u0435\u043A\u0456\u043B\u044C\u043A\u043E\u0445 \u043C\u0435\u0442\u0440\u0456\u0432 \u0434\u043E 1500 \u043C \u0456 \u0431\u0456\u043B\u044C\u0448\u0435 (\u0432 \u0433\u043E\u0440\u0430\u0445). \u042F\u0432\u0438\u0449\u0435 \u0431\u0430\u0433\u0430\u0442\u043E\u0440\u0456\u0447\u043D\u043E\u0457 \u043C\u0435\u0440\u0437\u043B\u043E\u0442\u0438 \u0437\u043C\u0456\u043D\u044E\u0454\u0442\u044C\u0441\u044F \u0440\u0430\u0437\u043E\u043C \u0437\u0456 \u0437\u043C\u0456\u043D\u043E\u044E \u0444\u0456\u0437\u0438\u043A\u043E-\u0433\u0435\u043E\u0433\u0440\u0430\u0444\u0456\u0447\u043D\u043E\u0433\u043E \u0441\u0435\u0440\u0435\u0434\u043E\u0432\u0438\u0449\u0430."@uk .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"\u6C38\u4E45\u51CD\u571F\uFF08\u3048\u3044\u304D\u3085\u3046\u3068\u3046\u3069\u3001\u82F1\u8A9E: permafrost\uFF09\u3068\u306F\u30012\u5E74\u9593\u4EE5\u4E0A\u306B\u308F\u305F\u308A\u7D99\u7D9A\u3057\u3066\u6E29\u5EA60\u2103\u4EE5\u4E0B\u3092\u3068\u308B\u5730\u76E4\u306E\u3053\u3068\u3067\u3042\u308B\u3002\u3053\u306E\u7528\u8A9E\u306E\u5B9A\u7FA9\u306E\u4E0A\u3067\u306F\u3001\u6C37\u306E\u5B58\u5728\u3067\u306F\u306A\u304F\u6E29\u5EA6\u6761\u4EF6\u3067\u8003\u3048\u308B\u3002 \u82F1\u8A9E\u3067\u306F\u3001\u6C38\u4E45\u51CD\u571F\u306E\u3053\u3068\u3092 permafrost \u3068\u8868\u8A18\u3059\u308B\u304C\u3001permanently frozen ground\uFF08\u6C38\u4E45\u306B\u51CD\u3063\u305F\u571F\u58CC\uFF09\u306E\u7701\u7565\u8A9E\u30671945\u5E74\u306B S. W. MULLER\u306B\u3088\u3063\u3066\u4F7F\u308F\u308C\u305F\u3002 \u6C38\u4E45\u51CD\u571F\u306F\u5317\u534A\u7403\u306E\u5927\u9678\u306E\u7D0420%\u306B\u5E83\u304C\u3063\u3066\u3044\u308B\u3002\u6C38\u4E45\u51CD\u571F\u306E\u539A\u3055\u306F\u6570\u767Em\uFF08\u30A2\u30E9\u30B9\u30AB\u306E Prudhoe Bay \u3067\u306F650m\uFF09\u306B\u3082\u53CA\u3076\u3053\u3068\u3082\u3042\u308B\u3002\u6C38\u4E45\u51CD\u571F\u306E\u4E0A\u90E8\u306B\u306F\u590F\u306E\u9593\u878D\u3051\u3066\u3044\u308B\u6D3B\u52D5\u5C64\u304C\u3042\u308A\u3001\u30DD\u30C9\u30BE\u30EB\u3068\u3044\u3046\u9178\u6027\u306E\u571F\u58CC\u3068\u306A\u308A\u3001\u30BF\u30A4\u30AC\u3084\u8349\u539F\u3068\u306A\u3063\u3066\u3044\u308B\u3002\u6D3B\u52D5\u5C64\u306E\u539A\u3055\u306F\u5E74\u3084\u5834\u6240\u306B\u3088\u3063\u3066\u5909\u5316\u3059\u308B\u304C\u3001\u5178\u578B\u7684\u306A\u3082\u306E\u3067\u306F0.6-4m\u306E\u539A\u3055\u3067\u3042\u308B\u3002 \u65E5\u672C\u3067\u306F\u3001\u5BCC\u58EB\u5C71\u9802\u4E0A\u4ED8\u8FD1\u304A\u3088\u3073\u5927\u96EA\u5C71\u9802\u4E0A\u4ED8\u8FD1\u3001\u5317\u30A2\u30EB\u30D7\u30B9\u306E\u7ACB\u5C71\u306A\u3069\u306B\u6C38\u4E45\u51CD\u571F\u304C\u78BA\u8A8D\u3055\u308C\u3001\u69CD\u30F6\u5CB3\u30FB\u7A42\u9AD8\u9023\u5CF0\u306E\u5927\u30AD\u30EC\u30C3\u30C8\u30AB\u30FC\u30EB\u5185\u306B\u5B58\u5728\u3057\u3066\u3044\u308B\u53EF\u80FD\u6027\u304C\u9AD8\u3044\u3068\u5831\u544A\u3055\u308C\u3066\u3044\u308B\u3002"@ja .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/State_of_emergency> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://et.dbpedia.org/resource/Igikelts> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Fennoscandian> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"\u062A\u0639\u0631\u0641 \u0627\u0644\u062A\u064F\u0631\u0628\u064E\u0629\u064F \u0627\u0644\u0635\u064E\u0651\u0642\u0650\u064A\u0639\u0650\u064A\u0651\u0629 Permafrost \u0628\u0623\u0646\u0647\u0627 \u0627\u0644\u0645\u0646\u0637\u0642\u0629 \u0627\u0644\u062A\u064A \u0645\u062A\u0648\u0633\u0637 \u062F\u0631\u062C\u0629 \u062D\u0631\u0627\u0631\u0629 \u0623\u0631\u0636\u0647\u0627 \u0627\u0644\u0633\u0646\u0648\u064A mean annual ground temperature MAGT \u0623\u0642\u0644 \u0645\u0646 \u0636\u063A\u0637 \u0646\u0642\u0637\u0629 \u0627\u0644\u0627\u0646\u0635\u0647\u0627\u0631 \u0639\u0644\u0649 \u0627\u0644\u0623\u0642\u0644 \u062E\u0644\u0627\u0644 \u0633\u0646\u062A\u0627\u0646 \u0639\u0644\u0649 \u0627\u0644\u062A\u0648\u0627\u0644\u064A. \u0648\u0647\u064A \u062A\u0642\u0627\u0628\u0644 \u0627\u0644\u0645\u0646\u0627\u0637\u0642 \u0627\u0644\u062A\u064A \u064A\u0643\u0648\u0646 \u0645\u062A\u0648\u0633\u0637 \u062F\u0631\u062C\u0629 \u062D\u0631\u0627\u0631\u0629 \u0627\u0644\u0647\u0648\u0627\u0621 mean annual air temperature MAAT \u0646\u0627\u0642\u0635 \u062F\u0631\u062C\u062A\u0627\u0646 \u0645\u0626\u0648\u064A\u0629 \u0623\u0648 \u0623\u0642\u0644"@ar .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Pipeline_transport> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Creep_(deformation)> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Rocky_Mountains> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Mikhail_Kim> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"\uC601\uAD6C\uB3D9\uD1A0(\u6C38\u4E45\u51CD\u571F, permafrost)\uB294 2\uB144 \uC774\uC0C1\uC758 \uAE30\uAC04 \uB3D9\uC548 \uD1A0\uC591 \uC628\uB3C4\uAC00 0\u00B0C(\uBB3C\uC758 \uC5B4\uB294\uC810, 32\u00B0F) \uC774\uD558\uB85C \uC720\uC9C0\uB41C \uD1A0\uC591\uC744 \uC77C\uCEEB\uB294\uB2E4. \uB300\uBD80\uBD84\uC758 \uC601\uAD6C\uB3D9\uD1A0\uB294 \uBD81\uADF9\uC774\uB098 \uB0A8\uADF9\uC5D0 \uAC00\uAE4C\uC6B4 \uACE0\uC704\uB3C4 \uC9C0\uC5ED\uC5D0 \uC790\uB9AC\uC7A1\uACE0 \uC788\uC73C\uB098, \uB192\uC740 \uACE0\uB3C4\uC5D0 \uD615\uC131\uB418\uB294 \uACE0\uC0B0 \uC601\uAD6C\uB3D9\uD1A0\uCE35\uC740 \uB0AE\uC740 \uC704\uB3C4\uC5D0\uB3C4 \uC874\uC7AC\uD560 \uC218 \uC788\uB2E4. \uBE59\uACB0\uC740 \uC790\uC8FC \uBC1C\uC0DD\uD558\uB294 \uD604\uC0C1\uC774\uC9C0\uB9CC, \uBB34\uACF5\uC131 \uAE30\uBC18\uC758 \uACBD\uC6B0\uC5D0\uB294 \uBE59\uACB0\uC774 \uD56D\uC0C1 \uBC1C\uC0DD\uD558\uB294 \uAC83\uC740 \uC544\uB2C8\uB2E4. \uC601\uAD6C\uB3D9\uD1A0\uB294 \uC9C0\uAD6C \uC0C1\uC758 \uC218\uBD84 \uC911 0.022%\uB97C \uCC28\uC9C0\uD558\uBA70, \uBD81\uBC18\uAD6C\uC5D0 \uB178\uCD9C\uB41C \uD1A0\uC591\uC758 24%\uC5D0 \uC874\uC7AC\uD55C\uB2E4."@ko .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#label>	"\uC601\uAD6C\uB3D9\uD1A0"@ko .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Prudhoe_Bay,_Alaska> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:Infobox_soil> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/University_of_Alaska_Fairbanks> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:Wiktionary> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://ky.dbpedia.org/resource/\u041A\u04E9\u043F_\u0436\u044B\u043B\u0434\u044B\u043A_\u0442\u043E\u04A3> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/File:K.E.vonBaer_1840_03.jpg> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/ns/prov#wasDerivedFrom>	<http://en.wikipedia.org/wiki/Permafrost?oldid=1124838667&ns=0> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Pseudomonadota> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Carbon_dioxide> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Climate_change> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://hy.dbpedia.org/resource/\u0540\u0561\u057E\u0565\u0580\u056A\u0561\u056F\u0561\u0576_\u057D\u0561\u057C\u0581\u0578\u0582\u0575\u0569> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Permafrost is ground that continuously remains below 0 \u00B0C (32 \u00B0F) for two or more years, located on land or under the ocean. Most common in the Northern Hemisphere, around 15% of the Northern Hemisphere or 11% of the global surface is underlain by permafrost, with the total area of around 18 million km2. This includes substantial areas of Alaska, Greenland, Canada and Siberia. It can also be located on mountaintops in the Southern Hemisphere and beneath ice-free areas in the Antarctic."@en .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:Further> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Acanthamoeba> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:Geotechnical_engineering> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Pyasino> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://sk.dbpedia.org/resource/Permafrost> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/name>	"Permafrost"@en .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageRevisionID>	"1124838667"^^<http://www.w3.org/2001/XMLSchema#integer> .
<http://dbpedia.org/resource/Permafrost>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Massive_ice_-_retrogressive_thaw_slump_-_Herschel_Island.png> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://hr.dbpedia.org/resource/Permafrost> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Changchun> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageLength>	"77928"^^<http://www.w3.org/2001/XMLSchema#nonNegativeInteger> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Dalam geologi, ibun abadi (bahasa Inggris: permafrost) atau tanah beku abadi adalah lapisan tanah beku yang berada di bawah suhu 0 \u00B0C selama beberapa tahun. Ibun abadi terbentuk dari es-es yang menggenggam berbagai macam tanah, pasir, dan bebatuan. Ibun abadi umumnya terletak di lintang tinggi, yaitu dekat kutub utara dan selatan. Ibun abadi biasa terbentuk dalam iklim dengan suhu udara rata-rata tahunan kurang dari titik beku air."@in .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Ocean> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"Permafrost bezeichnet in den Geowissenschaften einen Untergrund, dessen Temperatur f\u00FCr mindestens zwei Jahre ununterbrochen (perennierend) unter 0 \u00B0C liegt. Bei dem Untergrund kann es sich um Boden, Lockergestein oder Festgestein handeln. Permafrost tritt abh\u00E4ngig von den klimatischen Bedingungen mit unterschiedlicher M\u00E4chtigkeit und Tiefe auf; er kann mehrere hundert Meter tief reichen und besitzt dann meist ein Alter von vielen tausend Jahren. Die gr\u00F6\u00DFte Ausdehnung haben Permafrostb\u00F6den unter den Eisschilden und in den K\u00E4ltew\u00FCsten der beiden Polargebiete sowie in den angrenzenden hochkontinentalen Klimaten der (n\u00F6rdlichen) borealen Zone. Dort kann der Boden \u00FCber dem Permafrost im Sommer auftauen (siehe Auftauboden). Weitere gro\u00DFfl\u00E4chige Bereiche befinden sich in der Massenerhebung Hochasiens. Der Permafrostboden (auch Dauerfrostboden) ist eine der wichtigsten Kohlenstoffsenken der Erde. Das gro\u00DFr\u00E4umige Auftauen von Permafrost im Rahmen der globalen Erw\u00E4rmung gilt als eines der bedeutendsten Kippelemente im Klimawandel."@de .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageExternalLink>	<https://pleistocenepark.de/en/> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#label>	"\u0108iamfrosta grundo"@eo .
<http://dbpedia.org/resource/Permafrost>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Ice-wedge_hg.jpg> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Phreatic_zone> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://eu.dbpedia.org/resource/Permafrost> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Planctomycetota> .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Palsa> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Library_of_Congress> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Foundation_(architecture)> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Sweden> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#seeAlso>	<http://dbpedia.org/resource/Thermokarst> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Category:Permafrost> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#label>	"Wieczna zmarzlina"@pl .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://es.dbpedia.org/resource/Permafrost> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Category:Geomorphology> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#label>	"Permafrost"@nl .
<http://dbpedia.org/resource/Permafrost>	<http://purl.org/dc/terms/subject>	<http://dbpedia.org/resource/Category:Permafrost> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/East_Asia> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:Portalbar> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/1999/02/22-rdf-syntax-ns#type>	<http://dbpedia.org/ontology/Species> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:Citation_needed> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://sh.dbpedia.org/resource/Permafrost> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Soil_gas> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Northwest_Territories> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://vi.dbpedia.org/resource/T\u1EA7ng_\u0111\u1EA5t_\u0111\u00F3ng_b\u0103ng_v\u0129nh_c\u1EEDu> .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/University_of_Giessen> .
<http://dbpedia.org/resource/Permafrost>	<http://purl.org/dc/terms/subject>	<http://dbpedia.org/resource/Category:Geomorphology> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://zh.dbpedia.org/resource/\u6C38\u4E45\u51BB\u571F> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Argentina> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/St_Petersburg_Academy_of_Sciences> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Patagonia> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#label>	"Pergelissolo"@pt .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageExternalLink>	<http://www.permanet-alpinespace.eu/home.html/> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"\u041C\u043D\u043E\u0433\u043E\u043B\u0435\u0442\u043D\u044F\u044F \u043C\u0435\u0440\u0437\u043B\u043E\u0442\u0430 (\u043C\u043D\u043E\u0433\u043E\u043B\u0435\u0442\u043D\u044F\u044F \u043A\u0440\u0438\u043E\u043B\u0438\u0442\u043E\u0437\u043E\u043D\u0430, \u00AB\u0432\u0435\u0447\u043D\u0430\u044F \u043C\u0435\u0440\u0437\u043B\u043E\u0442\u0430\u00BB, \u043C\u043D\u043E\u0433\u043E\u043B\u0435\u0442\u043D\u0435-\u043C\u0451\u0440\u0437\u043B\u044B\u0435 \u043F\u043E\u0440\u043E\u0434\u044B) \u2014 \u0447\u0430\u0441\u0442\u044C \u043A\u0440\u0438\u043E\u043B\u0438\u0442\u043E\u0437\u043E\u043D\u044B, \u0445\u0430\u0440\u0430\u043A\u0442\u0435\u0440\u0438\u0437\u0443\u044E\u0449\u0430\u044F\u0441\u044F \u043E\u0442\u0441\u0443\u0442\u0441\u0442\u0432\u0438\u0435\u043C \u043F\u0435\u0440\u0438\u043E\u0434\u0438\u0447\u0435\u0441\u043A\u043E\u0433\u043E \u043F\u0440\u043E\u0442\u0430\u0438\u0432\u0430\u043D\u0438\u044F. \u041E\u0431\u0449\u0430\u044F \u043F\u043B\u043E\u0449\u0430\u0434\u044C \u0432\u0435\u0447\u043D\u043E\u0439 \u043C\u0435\u0440\u0437\u043B\u043E\u0442\u044B \u043D\u0430 \u0417\u0435\u043C\u043B\u0435 \u2014 35 \u043C\u043B\u043D \u043A\u043C\u00B2. \u0420\u0430\u0441\u043F\u0440\u043E\u0441\u0442\u0440\u0430\u043D\u0435\u043D\u0438\u0435 \u2014 \u0441\u0435\u0432\u0435\u0440 \u0410\u043C\u0435\u0440\u0438\u043A\u0438, \u0415\u0432\u0440\u043E\u043F\u044B, \u0410\u0437\u0438\u0438, \u043E\u0441\u0442\u0440\u043E\u0432\u0430 \u0421\u0435\u0432\u0435\u0440\u043D\u043E\u0433\u043E \u041B\u0435\u0434\u043E\u0432\u0438\u0442\u043E\u0433\u043E \u043E\u043A\u0435\u0430\u043D\u0430, \u0410\u043D\u0442\u0430\u0440\u043A\u0442\u0438\u0434\u0430. \u0420\u0430\u0439\u043E\u043D\u044B \u043C\u043D\u043E\u0433\u043E\u043B\u0435\u0442\u043D\u0435\u0439 \u043C\u0435\u0440\u0437\u043B\u043E\u0442\u044B \u2014 \u0432\u0435\u0440\u0445\u043D\u044F\u044F \u0447\u0430\u0441\u0442\u044C \u0437\u0435\u043C\u043D\u043E\u0439 \u043A\u043E\u0440\u044B, \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u0430 \u043A\u043E\u0442\u043E\u0440\u043E\u0439 \u0434\u043E\u043B\u0433\u043E\u0435 \u0432\u0440\u0435\u043C\u044F (\u043E\u0442 2\u20143 \u043B\u0435\u0442 \u0434\u043E \u0442\u044B\u0441\u044F\u0447\u0435\u043B\u0435\u0442\u0438\u0439) \u043D\u0435 \u043F\u043E\u0434\u043D\u0438\u043C\u0430\u0435\u0442\u0441\u044F \u0432\u044B\u0448\u0435 0 \u00B0C. \u0412 \u0437\u043E\u043D\u0435 \u043C\u043D\u043E\u0433\u043E\u043B\u0435\u0442\u043D\u0435\u0439 \u043C\u0435\u0440\u0437\u043B\u043E\u0442\u044B \u0433\u0440\u0443\u043D\u0442\u043E\u0432\u044B\u0435 \u0432\u043E\u0434\u044B \u043D\u0430\u0445\u043E\u0434\u044F\u0442\u0441\u044F \u0432 \u0432\u0438\u0434\u0435 \u043B\u044C\u0434\u0430, \u0435\u0451 \u0433\u043B\u0443\u0431\u0438\u043D\u0430 \u0438\u043D\u043E\u0433\u0434\u0430 \u043F\u0440\u0435\u0432\u044B\u0448\u0430\u0435\u0442 1000 \u043C\u0435\u0442\u0440\u043E\u0432. \u041E\u0431\u0449\u0435\u043F\u0440\u0438\u043D\u044F\u0442\u043E\u0435 \u043D\u0430\u0437\u0432\u0430\u043D\u0438\u0435 \u2014 \u00AB\u0432\u0435\u0447\u043D\u0430\u044F \u043C\u0435\u0440\u0437\u043B\u043E\u0442\u0430\u00BB, \u0442\u0435\u0440\u043C\u0438\u043D \u00AB\u043C\u043D\u043E\u0433\u043E\u043B\u0435\u0442\u043D\u044F\u044F \u043C\u0435\u0440\u0437\u043B\u043E\u0442\u0430\u00BB \u0438\u0441\u043F\u043E\u043B\u044C\u0437\u0443\u0435\u0442\u0441\u044F \u0432 \u043E\u0441\u043D\u043E\u0432\u043D\u043E\u043C \u043F\u0435\u0442\u0435\u0440\u0431\u0443\u0440\u0433\u0441\u043A\u043E\u0439 \u0433\u0435\u043E\u0433\u0440\u0430\u0444\u0438\u0447\u0435\u0441\u043A\u043E\u0439 \u043D\u0430\u0443\u0447\u043D\u043E\u0439 \u0448\u043A\u043E\u043B\u043E\u0439."@ru .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Altai_Mountains> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2000/01/rdf-schema#label>	"Permafrost"@en .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:See_also> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://oc.dbpedia.org/resource/Permafr\u00F2st> .
<http://dbpedia.org/resource/Permafrost>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Phoenix_Sol_0_horizon.jpg> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Karl_Ernst_von_Baer> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/File:Beaufort_Permafrost2.JPG> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Tipping_points_in_the_climate_system> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/climate>	"High latitudes, alpine regions"@en .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://ro.dbpedia.org/resource/Permafrost> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"Talamh at\u00E1 oighrithe go buan i r\u00E9igi\u00FAin an-fhuara an Domhain. Go domhain faoina bhun t\u00E1 talamh neamhoighrithe, agus os a chionn ciseal gn\u00EDomhach a reonn sa samhradh is a athoighr\u00EDonn sa bhf\u00F3mhar. Gineann an t-oighri\u00FA s\u00EDos \u00F3n dromchla gach geimhreadh br\u00FA ar na cisil neamhoighrithe uisceluchtaithe den chrios gn\u00EDomhach seo, agus uaireanta is f\u00E9idir go bhfuascla\u00EDtear an br\u00FA seo tr\u00ED scoilteanna sa chiseal dromchlach oighrithe. Is m\u00F3r an fhadhb \u00E9 seo do th\u00F3g\u00E1il b\u00F3ithre, foirgneamh is p\u00EDobl\u00EDnte. Nuair a th\u00F3gtar an f\u00E1sra inslithe chun si\u00FAil i r\u00E9igi\u00FAin sh\u00EDorsioctha, d\u00E9anann s\u00E9 sin an crios gn\u00EDomhach n\u00EDos doimhne tr\u00ED le\u00E1 na tal\u00FAn s\u00EDorshioctha, agus tugann s\u00E9 faoi ag an dromchla."@ga .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Szeged> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Norilsk> .
<http://dbpedia.org/resource/Permafrost>	<http://www.w3.org/2002/07/owl#sameAs>	<http://sv.dbpedia.org/resource/Permafrost> .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/abstract>	"En geologia, permagel o pergelisol (en angl\u00E8s, permafrost, de perma-, permanent i frost, gelat) s\u00F3n aquelles capes de s\u00F2l, roca o terra que romanen per sota del punt de congelaci\u00F3 de l'aigua (0 \u00B0C) durant com a m\u00EDnim dos anys seguits. El permagel est\u00E0 situat entre el , la capa superficial activa que respon a les oscil\u00B7lacions del clima, i la roca profunda no gelada, m\u00E9s afectada pel flux geot\u00E8rmic que pel clima. Els s\u00F2ls es classifiquen com a permagel continu (90 a 100% de cobertura de la superf\u00EDcie amb permagel), discontinu (50 a 90%), espor\u00E0dic (10 a 50%), isolat (>10%) i sense permagel."@ca .
<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:Excerpt> .
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<http://dbpedia.org/resource/Permafrost>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/International_Permafrost_Association> .