. . . . . "\u062A\u0630\u0628\u0630\u0628 \u0627\u0644\u0642\u0637\u0628 \u0627\u0644\u0634\u0645\u0627\u0644\u064A (\u0625\u064A\u0647 \u0623\u0648) \u0623\u0648 \u0627\u0644\u0648\u0636\u0639 \u0627\u0644\u062D\u0644\u0642\u064A \u0627\u0644\u0634\u0645\u0627\u0644\u064A/ \u0627\u0644\u0648\u0636\u0639 \u0627\u0644\u062D\u0644\u0642\u064A \u0641\u064A \u0646\u0635\u0641 \u0627\u0644\u0643\u0631\u0629 \u0627\u0644\u0634\u0645\u0627\u0644\u064A (\u0625\u0646 \u0625\u064A\u0647 \u0625\u0645) \u0647\u0648 \u0638\u0627\u0647\u0631\u0629 \u0645\u0646\u0627\u062E\u064A\u0629 \u0641\u064A \u0627\u0644\u0642\u0637\u0628\u064A\u0646 \u0634\u0645\u0627\u0644 \u062E\u0637 \u0627\u0644\u0639\u0631\u0636 20 \u062F\u0631\u062C\u0629. \u0648\u0647\u0648 \u062D\u0627\u0644\u0629 \u0645\u0647\u0645\u0629 \u0644\u0644\u0646\u0645\u0637 \u0627\u0644\u0645\u0646\u0627\u062E\u064A \u0641\u064A \u0646\u0635\u0641 \u0627\u0644\u0643\u0631\u0629 \u0627\u0644\u0634\u0645\u0627\u0644\u064A. \u0648\u062A\u064F\u0633\u0645\u0649 \u0627\u0644\u062D\u0627\u0644\u0629 \u0627\u0644\u0646\u0638\u064A\u0631\u0629 \u0644\u0647 \u0641\u064A \u0646\u0635\u0641 \u0627\u0644\u0643\u0631\u0629 \u0627\u0644\u062C\u0646\u0648\u0628\u064A \u0628\u0640 \u062A\u0630\u0628\u0630\u0628 \u0627\u0644\u0642\u0637\u0628 \u0627\u0644\u062C\u0646\u0648\u0628\u064A \u0623\u0648 \u0627\u0644\u0648\u0636\u0639 \u0627\u0644\u062D\u0644\u0642\u064A \u0627\u0644\u062C\u0646\u0648\u0628\u064A (\u0625\u0633 \u0625\u064A\u0647 \u0625\u0645). \u0648\u064A\u062A\u063A\u064A\u0631 \u0627\u0644\u0645\u0624\u0634\u0631 \u0628\u0645\u0631\u0648\u0631 \u0627\u0644\u0648\u0642\u062A \u062F\u0648\u0646 \u0623\u064A \u0641\u062A\u0631\u0627\u062A \u0632\u0645\u0646\u064A\u0629 \u0645\u062D\u062F\u062F\u0629 \u0648\u0627\u0636\u062D\u0629\u060C \u0648\u064A\u062A\u0633\u0645 \u0628\u0634\u0630\u0648\u0630 \u0636\u063A\u0637 \u063A\u064A\u0631 \u0645\u0648\u0633\u0645\u064A \u0639\u0644\u0649 \u0645\u0633\u062A\u0648\u0649 \u0633\u0637\u062D \u0627\u0644\u0628\u062D\u0631 \u0645\u0646 \u062F\u0644\u0627\u0644\u0629 \u0648\u0627\u062D\u062F\u0629 \u0641\u064A \u0627\u0644\u0642\u0637\u0628 \u0627\u0644\u0634\u0645\u0627\u0644\u064A\u060C \u064A\u0648\u0627\u0632\u0646\u0647\u0627 \u0627\u0644\u0634\u0630\u0648\u0630 \u0645\u0646 \u0627\u0644\u062F\u0644\u0627\u0644\u0629 \u0627\u0644\u0645\u0639\u0627\u0643\u0633\u0629 \u0627\u0644\u0645\u062A\u0645\u0631\u0643\u0632\u0629 \u0646\u062D\u0648 37-45 \u0634\u0645\u0627\u0644\u064B\u0627."@ar . "Arktisk oscillation (AO) \u00E4r ett index \u00F6ver lufttrycksvariationer norr om den tjugonde breddgraden (20\u00BAN). Tryckavvikelser fr\u00E5n normala indexmedelv\u00E4rden i Arktis brukar motsvaras av motsatta tryckavvikelser i zonen mellan breddgraderna 37\u00BA-45\u00BAN. Teorierna kring indexet lades fram 2001 av meteorologerna David Thompson och John Michael Wallace. Den nordatlantiska oscillationen spelar ocks\u00E5 roll f\u00F6r klimatet p\u00E5 det norra halvklotet och det r\u00E5der delade meningar om vilket av klimatfenomenen som b\u00E4st f\u00F6rklarar dynamiken i de atmosf\u00E4riska v\u00E4xlingarna."@sv . "La oscilaci\u00F3n \u00E1rtica (acr\u00F3nimo en ingl\u00E9s AO) es el patr\u00F3n dominante de las variaciones no estacionales de presi\u00F3n atmosf\u00E9rica (SLP) al norte de los 20\u00BA N, y se caracteriza por anomal\u00EDas en la presi\u00F3n de magnitudes positivas o negativas en el \u00C1rtico, y anomal\u00EDas de magnitudes opuestas localizadas cerca de los 37-45\u00BA N. La oscilaci\u00F3n del Atl\u00E1ntico Norte (NAO) tiene una relaci\u00F3n estrecha con la AO y hay argumentos acerca de si es uno o el otro el que representa mejor la din\u00E1mica de la atm\u00F3sfera."@es . "\u5317\u6975\u632F\u76EA\uFF08\u82F1\u8A9E\uFF1AArctic Oscillation\uFF0C\u7E2E\u5BEB\uFF1AAO\uFF1BNorthern Annular Mode/Northern Hemisphere Annular Mode\uFF08NAM\uFF09\uFF09\uFF0C\u53C8\u7A31\u5317\u6975\u9707\u8361\uFF0C\u662F\u6307\u5317\u6975\u7684\u6C23\u58D3\u8207\u5317\u534A\u7403\u4E2D\u7DEF\u5EA6\u5730\u5E36\u7684\u6C23\u58D3\u5448\u73FE\u53CD\u5411\u8B8A\u52D5\u95DC\u4FC2\u7684\u73FE\u8C61\u3002\u6B64\u73FE\u8C61\u63CF\u8FF0\u65BC1998\u5E74\u7531\u7F8E\u570B\u83EF\u76DB\u9813\u5927\u5B78\u7684\u6C23\u8C61\u5B78\u8005\u5927\u885B\u00B7\u6E6F\u666E\u751F\uFF08David W. J. Thompson\uFF09\u8207\u63D0\u51FA\u3002\u76F8\u4F3C\u7684\u73FE\u8C61\u5728\u5357\u6975\u8207\u5357\u534A\u7403\u4E2D\u7DEF\u5EA6\u5730\u5E36\u4EA6\u6709\u89C0\u6E2C\u5230\uFF0C\u7A31\u70BA\u5357\u6975\u632F\u76EA\uFF08\u82F1\u8A9E\uFF1AAntarctic oscillation\uFF0C\u7E2E\u5BEB\uFF1AAAO\uFF0C\u591A\u52A0\u4E00\u500BA\u4EE5\u8207\u5317\u6975\u632F\u76EA\u5340\u5225\uFF09\u3002\u53E6\u5916\uFF0C\u5728\u5317\u6975\u632F\u76EA\u8AAA\u88AB\u63D0\u51FA\u4E4B\u524D\uFF0C\u65BC1920\u5E74\u4EE3\u5373\u89C0\u6E2C\u5230\u7684\u5317\u5927\u897F\u6D0B\u632F\u76EA\uFF08\u82F1\u8A9E\uFF1ANorth Atlantic Oscillation\uFF0C\u7E2E\u5BEB\uFF1ANAO\uFF09\u56E0\u8207\u5317\u6975\u632F\u76EA\u76F8\u7576\u4E00\u81F4\uFF0C\u6240\u4EE5\u4E5F\u6709\u7814\u7A76\u8005\u5C07\u5169\u8005\u5408\u4F75\u70BA\u300CAO/NAO\u300D\u3002\u5317\u6975\u6E26\u65CB\u901A\u5E38\u662F\u5728\u5317\u6975\u5708\u9644\u8FD1\uFF0C\u51B7\u7A7A\u6C23\u6700\u51B7\uFF0C\u4F46\u662F\u5076\u723E\u6703\u6709\u6696\u7A7A\u6C23\u5165\u4FB5\u5230\u5317\u6975\u5708\u88E1\u9762\uFF0C\u9019\u6642\u5317\u6975\u5708\u88E1\u9762\u7684\u51B7\u7A7A\u6C23\uFF0C\u5C31\u6703\u88AB\u64E0\u51FA\u4F86\uFF0C\u7A31\u4F5C\u300C\u8CA0\u5317\u6975\u632F\u76EA\u300D"@zh . . . "Artikoaren oszilazioa (ingelesez: Arctic Oscillation, AO edo Northern Annular Mode/Northern Hemisphere Annular Mode, NAM) latitude polarretan eta ertainetan presio atmosferikoak fase negatiboen eta positiboen artean fluktuatzen duenean sortzen den patroia da. Patroia lehendabizikoz Edward Norton Lorenzek identifikatu zuen eta 1998an David W. J. Thompson eta John Michael Wallace adituek egungo izena eman zioten. Ipar Atlantikoko oszilaziorekin (NAO) lotura handia du baina bere eremua NAOren baino handiagoa da."@eu . . "\uBD81\uADF9\uC9C4\uB3D9"@ko . . . . . . "Artikoaren oszilazioa (ingelesez: Arctic Oscillation, AO edo Northern Annular Mode/Northern Hemisphere Annular Mode, NAM) latitude polarretan eta ertainetan presio atmosferikoak fase negatiboen eta positiboen artean fluktuatzen duenean sortzen den patroia da. Patroia lehendabizikoz Edward Norton Lorenzek identifikatu zuen eta 1998an David W. J. Thompson eta John Michael Wallace adituek egungo izena eman zioten. Ipar Atlantikoko oszilaziorekin (NAO) lotura handia du baina bere eremua NAOren baino handiagoa da."@eu . . . . . . . . . . "Oscillation arctique"@fr . . "\u5317\u6975\u632F\u52D5\uFF08\u307B\u3063\u304D\u3087\u304F\u3057\u3093\u3069\u3046\u3001\u82F1\u8A9E\uFF1AArctic Oscillation\uFF1AAO\uFF09\u3068\u306F\u3001\u5317\u6975\u3068\u5317\u534A\u7403\u4E2D\u7DEF\u5EA6\u5730\u57DF\u306E\u6C17\u5727\u304C\u76F8\u53CD\u3057\u3066\u5909\u52D5\u3059\u308B\u73FE\u8C61\u306E\u3053\u3068\u3067\u3042\u308B\u3002\u30C6\u30EC\u30B3\u30CD\u30AF\u30B7\u30E7\u30F3\uFF08\u5927\u6C17\u632F\u52D5\uFF09\u306E\u4E00\u7A2E\u3067\u3001\u6C17\u6E29\u3084\u4E0A\u7A7A\u306E\u30B8\u30A7\u30C3\u30C8\u6C17\u6D41\u6D41\u8DEF\u7B49\u306B\u3082\u5909\u5316\u3092\u3082\u305F\u3089\u3059\u3002\u51AC\u5B63\u306B\u3053\u306E\u632F\u52D5\u306E\u5E45\u304C\u5927\u304D\u304F\u306A\u308B\u3068\u3001\u5317\u534A\u7403\u306E\u9AD8\u7DEF\u5EA6\u30FB\u4E2D\u7DEF\u5EA6\u5730\u57DF\u3067\u5BD2\u6CE2\u3084\u305D\u308C\u306B\u4F34\u3046\u5927\u96EA\u3001\u7570\u5E38\u9AD8\u6E29\u304C\u8D77\u304D\u308B\u3002"@ja . . "Arctic oscillation"@en . "L'oscillazione artica (inglese: Arctic Oscillation) o indice AO \u00E8 un indice descrittivo che fa parte delle teleconnessioni atmosferiche. Detto indice varia in modo non stagionale e senza particolari periodicit\u00E0. L'indice AO \u00E8 calcolato in base alla differenza di pressione tra l'artico e le medio-basse latitudini, generalmente comprese tra il 37\u00BA e il 45\u00BA parallelo. La differenza di pressione tra l'artico e le medie latitudini descrive la forza del vortice polare. L'indice AO \u00E8 strettamente collegato all'indice NAM. L'oscillazione tra le pressioni a livello del mare a latitudini polari e temperate \u00E8 stata identificata da Edward Lorenz e definitivamente accettato nel 1998 da David WJ Thompson e John Michael Wallace.La strutturazione del vortice polare \u00E8 particolarmente importante in inverno, quando determina le sorti meteorologiche di Europa, Asia centrosettentrionale e Nord America, determinando quanto l'aria fredda del vortice polare \u00E8 in grado di influenzare il clima delle medie latitudini.Si caratterizza da due fasi: fase positiva e fase negativa."@it . . "L\u2019oscillation arctique (OA) est une variation de la diff\u00E9rence de pression atmosph\u00E9rique, au niveau de la mer, entre 20\u00B0 N et le P\u00F4le, d'une ann\u00E9e \u00E0 l'autre. Cette variation est reli\u00E9e \u00E0 l'intensit\u00E9 et la position moyenne des d\u00E9pressions et anticyclones entre l'Arctique et les latitudes de 37\u00B0 \u00E0 45\u00B0 nord ; ainsi que celle du vortex polaire. Elle couvre tout l\u2019h\u00E9misph\u00E8re nord alors que d'autres oscillations similaires, comme l\u2019oscillation nord-atlantique, couvrent des bassins oc\u00E9aniques particuliers."@fr . . . . "1121829047"^^ . . . . "Die Arktische Oszillation (AO) (engl. auch Northern Hemispheric Annular Mode (NAM)) ist Ausdruck des Luftdruckgegensatzes zwischen den arktischen und den mittleren Breiten auf der Nordhemisph\u00E4re. Arktische und antarktische Oszillation sind gro\u00DFe Systeme der Telekonnektion der Erde, s. a. Polarwirbel."@de . . . "La oscilaci\u00F3n \u00E1rtica (acr\u00F3nimo en ingl\u00E9s AO) es el patr\u00F3n dominante de las variaciones no estacionales de presi\u00F3n atmosf\u00E9rica (SLP) al norte de los 20\u00BA N, y se caracteriza por anomal\u00EDas en la presi\u00F3n de magnitudes positivas o negativas en el \u00C1rtico, y anomal\u00EDas de magnitudes opuestas localizadas cerca de los 37-45\u00BA N. La oscilaci\u00F3n del Atl\u00E1ntico Norte (NAO) tiene una relaci\u00F3n estrecha con la AO y hay argumentos acerca de si es uno o el otro el que representa mejor la din\u00E1mica de la atm\u00F3sfera."@es . . "December 2021"@en . "L'Oscil\u00B7laci\u00F3 \u00C0rtica o el Mode Anul\u00B7lar del Nord/Mode Anul\u00B7lar de l'Hemisferi Nord (en angl\u00E8s Arctic Oscillation, AO o Northern Annular Mode/Northern Hemisphere Annular Mode, NAM) \u00E9s el patr\u00F3 de variabilitat dominant del camp de pressi\u00F3 a nivell del mar a l'Hemisferi Nord per damunt de la latitud 20\u00B0 N. Aquest patr\u00F3 de variabilitat atmosf\u00E8rica ve caracteritzat per anomalies de pressi\u00F3 d'un signe a l'\u00C0rtic amb anomalies oposades centrades sobre les latituds 37-45\u00B0 N. Les variacions de pressi\u00F3 provocades per aquest patr\u00F3 de variabilitat estan relacionades amb la intensitat i la posici\u00F3 mitjana de les altes i baixes pressions entre l'\u00C0rtic i les latituds 37-45\u00B0N. El grau en qu\u00E8 l'aire de l'\u00C0rtic penetra cap a latituds mitjanes est\u00E0 relacionat amb la magnitud de l'Oscil\u00B7laci\u00F3 \u00C0rtica. L'\u00EDndex de l'AO quan es troba en la seva fase positiva, la pressi\u00F3 en superf\u00EDcie \u00E9s m\u00E9s baixa que l'habitual a la regi\u00F3 polar. Aix\u00F2 ajuda a fer que el corrent en jet a latituds mitjanes sigui m\u00E9s intens i amb una component m\u00E9s zonal (d'oest a est). Aquest refor\u00E7ament provoca un confinament major de l'aire fred de l'\u00C0rtic a la regi\u00F3 polar. En canvi, quan l'\u00EDndex de l'AO es troba en la seva fase negativa, la pressi\u00F3 en superf\u00EDcie sopbre la zona polar \u00E9s m\u00E9s alta que la normal, amb una disminuci\u00F3 dels vents zonals que al mateix temps permet una major circulaci\u00F3 d'aire fred polar cap a latituds mitjanes. Aquest patr\u00F3 va ser identificat per primera vegada per i anomenat com es coneix actualment per David W.J. Thompson i John Michael Wallace el 1998. L'Oscil\u00B7laci\u00F3 de l'Atl\u00E0ntic Nord (NAO), que \u00E9s un patr\u00F3 de varibilitat atmosf\u00E8rica de l'Atl\u00E0ntic Nord, est\u00E0 estretament relacionada amb l'AO, per\u00F2 el seu abast espacial \u00E9s menor que el de l'AO."@ca . . "phrase introduced by \"that\" expected, so that the \"so ... that ...\" would be complete"@en . . . "Arktisk oscillation (AO) \u00E4r ett index \u00F6ver lufttrycksvariationer norr om den tjugonde breddgraden (20\u00BAN). Tryckavvikelser fr\u00E5n normala indexmedelv\u00E4rden i Arktis brukar motsvaras av motsatta tryckavvikelser i zonen mellan breddgraderna 37\u00BA-45\u00BAN. Teorierna kring indexet lades fram 2001 av meteorologerna David Thompson och John Michael Wallace. Positivt AO-index k\u00E4nnetecknas av l\u00E5gtryck i Arktis, som permanenteras av omgivande varma v\u00E4stliga stormvindar (jetstr\u00F6mmar) och hindrar den arktiska k\u00F6ldluften fr\u00E5n att sprida sig s\u00F6derut. Negativt AO-index motsvaras av h\u00F6gtryck i Arktis och \u00F6stliga eller v\u00E4stliga jetstr\u00F6mmar kan inte hindra den arktiska k\u00F6ldluften fr\u00E5n att sprida sig s\u00F6derut med nordliga vindar. Den nordatlantiska oscillationen spelar ocks\u00E5 roll f\u00F6r klimatet p\u00E5 det norra halvklotet och det r\u00E5der delade meningar om vilket av klimatfenomenen som b\u00E4st f\u00F6rklarar dynamiken i de atmosf\u00E4riska v\u00E4xlingarna. Under n\u00E4stan hela 1900-talet pendlade den arktiska oscillationen mellan positiva och negativa faser. Med b\u00F6rjan p\u00E5 1970-talet tenderade indexet att stanna p\u00E5 den positiva sidan vilket motsvarades av l\u00E4gre lufttryck \u00E4n normalt i Arktis och h\u00F6gre temperaturer i USA, norra Europa och Sibirien. Vid millennieskiftet planade indexkurvan ut och i slutet av 00-talet fanns en ned\u00E5tg\u00E5ende tendens. Vad det beror p\u00E5 \u00E4r \u00E4nnu ok\u00E4nt f\u00F6r forskarna. En teori \u00E4r att \u00F6kade utsl\u00E4pp av v\u00E4xthusgaser \u00E4r en viktig faktor i ett komplext samband. En annan teori \u00E4r att de sm\u00E4ltande medf\u00F6rt st\u00F6rre och varmare havsyta i Arktis. Mot teorin om v\u00E4xthusgasers p\u00E5verkan talar det faktum att AO v\u00E4xlade mellan positiv och negativ fas \u00E4ven under f\u00F6rsta halvan av 1900-talet d\u00E5 koldioxid var kvar p\u00E5 f\u00F6rindustriella 290 ppm."@sv . . . "L\u2019oscillation arctique (OA) est une variation de la diff\u00E9rence de pression atmosph\u00E9rique, au niveau de la mer, entre 20\u00B0 N et le P\u00F4le, d'une ann\u00E9e \u00E0 l'autre. Cette variation est reli\u00E9e \u00E0 l'intensit\u00E9 et la position moyenne des d\u00E9pressions et anticyclones entre l'Arctique et les latitudes de 37\u00B0 \u00E0 45\u00B0 nord ; ainsi que celle du vortex polaire. Elle couvre tout l\u2019h\u00E9misph\u00E8re nord alors que d'autres oscillations similaires, comme l\u2019oscillation nord-atlantique, couvrent des bassins oc\u00E9aniques particuliers."@fr . . . . "\u0410\u0440\u043A\u0442\u0438\u0447\u0435\u0441\u043A\u0430\u044F \u043E\u0441\u0446\u0438\u043B\u043B\u044F\u0446\u0438\u044F \u0438\u043B\u0438 \u0418\u0437\u043C\u0435\u043D\u0435\u043D\u0438\u044F \u0441\u0435\u0432\u0435\u0440\u043D\u043E\u0439 \u0446\u0438\u0440\u043A\u0443\u043B\u044F\u0446\u0438\u0438 \u2014 \u0438\u043D\u0434\u0435\u043A\u0441 \u0438\u0437\u043C\u0435\u043D\u0435\u043D\u0438\u044F \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u044F \u043D\u0430 \u0443\u0440\u043E\u0432\u043D\u0435 \u043C\u043E\u0440\u044F \u043A \u0441\u0435\u0432\u0435\u0440\u0443 \u043E\u0442 20\u00B0 \u0441.\u0448., \u0445\u0430\u0440\u0430\u043A\u0442\u0435\u0440\u0438\u0437\u0443\u044E\u0449\u0438\u0439 \u0430\u043D\u043E\u043C\u0430\u043B\u0438\u044E \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u044F \u0432 \u0410\u0440\u043A\u0442\u0438\u043A\u0435 \u043F\u043E \u043E\u0442\u043D\u043E\u0448\u0435\u043D\u0438\u044E \u043A \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u044E \u0432 \u0431\u043E\u043B\u0435\u0435 \u044E\u0436\u043D\u044B\u0445 \u0448\u0438\u0440\u043E\u0442\u0430\u0445 \u0441\u0435\u0432\u0435\u0440\u043D\u043E\u0433\u043E \u043F\u043E\u043B\u0443\u0448\u0430\u0440\u0438\u044F \u0441 \u0446\u0435\u043D\u0442\u0440\u043E\u043C \u0438\u0437\u043C\u0435\u0440\u0435\u043D\u0438\u044F \u043D\u0430 \u0448\u0438\u0440\u043E\u0442\u0430\u0445 37-45\u00B0 \u0441.\u0448. \u0410\u0440\u043A\u0442\u0438\u0447\u0435\u0441\u043A\u0430\u044F \u043E\u0441\u0446\u0438\u043B\u043B\u044F\u0446\u0438\u044F \u044F\u0432\u043B\u044F\u0435\u0442\u0441\u044F \u043E\u0434\u043D\u0438\u043C \u0438\u0437 \u043E\u0441\u043D\u043E\u0432\u043D\u044B\u0445 \u0444\u0430\u043A\u0442\u043E\u0440\u043E\u0432, \u043E\u043F\u0440\u0435\u0434\u0435\u043B\u044F\u044E\u0449\u0438\u0445 \u0445\u0430\u0440\u0430\u043A\u0442\u0435\u0440 \u043F\u043E\u0433\u043E\u0434\u044B \u0441\u0435\u0432\u0435\u0440\u043D\u043E\u0433\u043E \u043F\u043E\u043B\u0443\u0448\u0430\u0440\u0438\u044F \u0432 \u0442\u0435\u0447\u0435\u043D\u0438\u0435 \u0437\u0438\u043C\u043D\u0435\u0433\u043E \u043F\u0435\u0440\u0438\u043E\u0434\u0430. \u0418\u0437\u043C\u0435\u043D\u0435\u043D\u0438\u0435 \u0438\u043D\u0434\u0435\u043A\u0441\u0430 \u043D\u0430 \u043F\u0440\u043E\u0442\u044F\u0436\u0435\u043D\u0438\u0438 \u0434\u043B\u0438\u0442\u0435\u043B\u044C\u043D\u044B\u0445 \u0438\u043D\u0442\u0435\u0440\u0432\u0430\u043B\u043E\u0432 \u0432\u0440\u0435\u043C\u0435\u043D\u0438 \u043D\u0435 \u0438\u043C\u0435\u0435\u0442 \u0441\u0442\u0440\u043E\u0433\u043E\u0439 \u043F\u0435\u0440\u0438\u043E\u0434\u0438\u0447\u043D\u043E\u0441\u0442\u0438. \n* \u0410\u0440\u043A\u0442\u0438\u0447\u0435\u0441\u043A\u0430\u044F \u043E\u0441\u0446\u0438\u043B\u043B\u044F\u0446\u0438\u044F \u0432 \u0437\u0438\u043C\u043D\u0438\u0435 \u0441\u0435\u0437\u043E\u043D\u044B 1899\u20132011 \u0433\u0433."@ru . . . . . . . . . "AO December to March precipitation pattern."@en . . . . . . "Oscil\u00B7laci\u00F3 \u00C0rtica"@ca . . . . . . "1277797"^^ . . . . . . . . . . . "AO_Temperature.png"@en . "AO December to March temperature pattern."@en . . "Artikoaren oszilazio"@eu . "L'Oscil\u00B7laci\u00F3 \u00C0rtica o el Mode Anul\u00B7lar del Nord/Mode Anul\u00B7lar de l'Hemisferi Nord (en angl\u00E8s Arctic Oscillation, AO o Northern Annular Mode/Northern Hemisphere Annular Mode, NAM) \u00E9s el patr\u00F3 de variabilitat dominant del camp de pressi\u00F3 a nivell del mar a l'Hemisferi Nord per damunt de la latitud 20\u00B0 N. Aquest patr\u00F3 de variabilitat atmosf\u00E8rica ve caracteritzat per anomalies de pressi\u00F3 d'un signe a l'\u00C0rtic amb anomalies oposades centrades sobre les latituds 37-45\u00B0 N. Les variacions de pressi\u00F3 provocades per aquest patr\u00F3 de variabilitat estan relacionades amb la intensitat i la posici\u00F3 mitjana de les altes i baixes pressions entre l'\u00C0rtic i les latituds 37-45\u00B0N."@ca . . "Oscilaci\u00F3n \u00E1rtica"@es . . "\u5317\u6975\u632F\u52D5\uFF08\u307B\u3063\u304D\u3087\u304F\u3057\u3093\u3069\u3046\u3001\u82F1\u8A9E\uFF1AArctic Oscillation\uFF1AAO\uFF09\u3068\u306F\u3001\u5317\u6975\u3068\u5317\u534A\u7403\u4E2D\u7DEF\u5EA6\u5730\u57DF\u306E\u6C17\u5727\u304C\u76F8\u53CD\u3057\u3066\u5909\u52D5\u3059\u308B\u73FE\u8C61\u306E\u3053\u3068\u3067\u3042\u308B\u3002\u30C6\u30EC\u30B3\u30CD\u30AF\u30B7\u30E7\u30F3\uFF08\u5927\u6C17\u632F\u52D5\uFF09\u306E\u4E00\u7A2E\u3067\u3001\u6C17\u6E29\u3084\u4E0A\u7A7A\u306E\u30B8\u30A7\u30C3\u30C8\u6C17\u6D41\u6D41\u8DEF\u7B49\u306B\u3082\u5909\u5316\u3092\u3082\u305F\u3089\u3059\u3002\u51AC\u5B63\u306B\u3053\u306E\u632F\u52D5\u306E\u5E45\u304C\u5927\u304D\u304F\u306A\u308B\u3068\u3001\u5317\u534A\u7403\u306E\u9AD8\u7DEF\u5EA6\u30FB\u4E2D\u7DEF\u5EA6\u5730\u57DF\u3067\u5BD2\u6CE2\u3084\u305D\u308C\u306B\u4F34\u3046\u5927\u96EA\u3001\u7570\u5E38\u9AD8\u6E29\u304C\u8D77\u304D\u308B\u3002"@ja . . "L'oscillazione artica (inglese: Arctic Oscillation) o indice AO \u00E8 un indice descrittivo che fa parte delle teleconnessioni atmosferiche. Detto indice varia in modo non stagionale e senza particolari periodicit\u00E0. L'indice AO \u00E8 calcolato in base alla differenza di pressione tra l'artico e le medio-basse latitudini, generalmente comprese tra il 37\u00BA e il 45\u00BA parallelo. La differenza di pressione tra l'artico e le medie latitudini descrive la forza del vortice polare."@it . "\u5317\u6975\u632F\u76EA\uFF08\u82F1\u8A9E\uFF1AArctic Oscillation\uFF0C\u7E2E\u5BEB\uFF1AAO\uFF1BNorthern Annular Mode/Northern Hemisphere Annular Mode\uFF08NAM\uFF09\uFF09\uFF0C\u53C8\u7A31\u5317\u6975\u9707\u8361\uFF0C\u662F\u6307\u5317\u6975\u7684\u6C23\u58D3\u8207\u5317\u534A\u7403\u4E2D\u7DEF\u5EA6\u5730\u5E36\u7684\u6C23\u58D3\u5448\u73FE\u53CD\u5411\u8B8A\u52D5\u95DC\u4FC2\u7684\u73FE\u8C61\u3002\u6B64\u73FE\u8C61\u63CF\u8FF0\u65BC1998\u5E74\u7531\u7F8E\u570B\u83EF\u76DB\u9813\u5927\u5B78\u7684\u6C23\u8C61\u5B78\u8005\u5927\u885B\u00B7\u6E6F\u666E\u751F\uFF08David W. J. Thompson\uFF09\u8207\u63D0\u51FA\u3002\u76F8\u4F3C\u7684\u73FE\u8C61\u5728\u5357\u6975\u8207\u5357\u534A\u7403\u4E2D\u7DEF\u5EA6\u5730\u5E36\u4EA6\u6709\u89C0\u6E2C\u5230\uFF0C\u7A31\u70BA\u5357\u6975\u632F\u76EA\uFF08\u82F1\u8A9E\uFF1AAntarctic oscillation\uFF0C\u7E2E\u5BEB\uFF1AAAO\uFF0C\u591A\u52A0\u4E00\u500BA\u4EE5\u8207\u5317\u6975\u632F\u76EA\u5340\u5225\uFF09\u3002\u53E6\u5916\uFF0C\u5728\u5317\u6975\u632F\u76EA\u8AAA\u88AB\u63D0\u51FA\u4E4B\u524D\uFF0C\u65BC1920\u5E74\u4EE3\u5373\u89C0\u6E2C\u5230\u7684\u5317\u5927\u897F\u6D0B\u632F\u76EA\uFF08\u82F1\u8A9E\uFF1ANorth Atlantic Oscillation\uFF0C\u7E2E\u5BEB\uFF1ANAO\uFF09\u56E0\u8207\u5317\u6975\u632F\u76EA\u76F8\u7576\u4E00\u81F4\uFF0C\u6240\u4EE5\u4E5F\u6709\u7814\u7A76\u8005\u5C07\u5169\u8005\u5408\u4F75\u70BA\u300CAO/NAO\u300D\u3002\u5317\u6975\u6E26\u65CB\u901A\u5E38\u662F\u5728\u5317\u6975\u5708\u9644\u8FD1\uFF0C\u51B7\u7A7A\u6C23\u6700\u51B7\uFF0C\u4F46\u662F\u5076\u723E\u6703\u6709\u6696\u7A7A\u6C23\u5165\u4FB5\u5230\u5317\u6975\u5708\u88E1\u9762\uFF0C\u9019\u6642\u5317\u6975\u5708\u88E1\u9762\u7684\u51B7\u7A7A\u6C23\uFF0C\u5C31\u6703\u88AB\u64E0\u51FA\u4F86\uFF0C\u7A31\u4F5C\u300C\u8CA0\u5317\u6975\u632F\u76EA\u300D"@zh . . . . . . . . . . "The Arctic oscillation (AO) or Northern Annular Mode/Northern Hemisphere Annular Mode (NAM) is a weather phenomenon at the Arctic pole north of 20 degrees latitude. It is an important mode of climate variability for the Northern Hemisphere. The southern hemisphere analogue is called the Antarctic oscillation or Southern Annular Mode (SAM). The index varies over time with no particular periodicity, and is characterized by non-seasonal sea-level pressure anomalies of one sign in the Arctic, balanced by anomalies of opposite sign centered at about 37\u201345\u00B0 N. The North Atlantic oscillation (NAO) is a close relative of the Arctic oscillation. There is debate over whether one or the other is more fundamentally representative of the atmosphere's dynamics. The NAO may be identified in a more physically meaningful way, which may carry more impact on measurable effects of changes in the atmosphere."@en . "Arktisk oscillation"@sv . . . . . . . . "\u0410\u0440\u043A\u0442\u0438\u0447\u0435\u0441\u043A\u0430\u044F \u043E\u0441\u0446\u0438\u043B\u043B\u044F\u0446\u0438\u044F"@ru . "\u5317\u6975\u632F\u76EA"@zh . "\u062A\u0630\u0628\u0630\u0628 \u0627\u0644\u0642\u0637\u0628 \u0627\u0644\u0634\u0645\u0627\u0644\u064A"@ar . . . . "\u0410\u0440\u043A\u0442\u0438\u0447\u0435\u0441\u043A\u0430\u044F \u043E\u0441\u0446\u0438\u043B\u043B\u044F\u0446\u0438\u044F \u0438\u043B\u0438 \u0418\u0437\u043C\u0435\u043D\u0435\u043D\u0438\u044F \u0441\u0435\u0432\u0435\u0440\u043D\u043E\u0439 \u0446\u0438\u0440\u043A\u0443\u043B\u044F\u0446\u0438\u0438 \u2014 \u0438\u043D\u0434\u0435\u043A\u0441 \u0438\u0437\u043C\u0435\u043D\u0435\u043D\u0438\u044F \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u044F \u043D\u0430 \u0443\u0440\u043E\u0432\u043D\u0435 \u043C\u043E\u0440\u044F \u043A \u0441\u0435\u0432\u0435\u0440\u0443 \u043E\u0442 20\u00B0 \u0441.\u0448., \u0445\u0430\u0440\u0430\u043A\u0442\u0435\u0440\u0438\u0437\u0443\u044E\u0449\u0438\u0439 \u0430\u043D\u043E\u043C\u0430\u043B\u0438\u044E \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u044F \u0432 \u0410\u0440\u043A\u0442\u0438\u043A\u0435 \u043F\u043E \u043E\u0442\u043D\u043E\u0448\u0435\u043D\u0438\u044E \u043A \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u044E \u0432 \u0431\u043E\u043B\u0435\u0435 \u044E\u0436\u043D\u044B\u0445 \u0448\u0438\u0440\u043E\u0442\u0430\u0445 \u0441\u0435\u0432\u0435\u0440\u043D\u043E\u0433\u043E \u043F\u043E\u043B\u0443\u0448\u0430\u0440\u0438\u044F \u0441 \u0446\u0435\u043D\u0442\u0440\u043E\u043C \u0438\u0437\u043C\u0435\u0440\u0435\u043D\u0438\u044F \u043D\u0430 \u0448\u0438\u0440\u043E\u0442\u0430\u0445 37-45\u00B0 \u0441.\u0448. \u0410\u0440\u043A\u0442\u0438\u0447\u0435\u0441\u043A\u0430\u044F \u043E\u0441\u0446\u0438\u043B\u043B\u044F\u0446\u0438\u044F \u044F\u0432\u043B\u044F\u0435\u0442\u0441\u044F \u043E\u0434\u043D\u0438\u043C \u0438\u0437 \u043E\u0441\u043D\u043E\u0432\u043D\u044B\u0445 \u0444\u0430\u043A\u0442\u043E\u0440\u043E\u0432, \u043E\u043F\u0440\u0435\u0434\u0435\u043B\u044F\u044E\u0449\u0438\u0445 \u0445\u0430\u0440\u0430\u043A\u0442\u0435\u0440 \u043F\u043E\u0433\u043E\u0434\u044B \u0441\u0435\u0432\u0435\u0440\u043D\u043E\u0433\u043E \u043F\u043E\u043B\u0443\u0448\u0430\u0440\u0438\u044F \u0432 \u0442\u0435\u0447\u0435\u043D\u0438\u0435 \u0437\u0438\u043C\u043D\u0435\u0433\u043E \u043F\u0435\u0440\u0438\u043E\u0434\u0430. \u0418\u0437\u043C\u0435\u043D\u0435\u043D\u0438\u0435 \u0438\u043D\u0434\u0435\u043A\u0441\u0430 \u043D\u0430 \u043F\u0440\u043E\u0442\u044F\u0436\u0435\u043D\u0438\u0438 \u0434\u043B\u0438\u0442\u0435\u043B\u044C\u043D\u044B\u0445 \u0438\u043D\u0442\u0435\u0440\u0432\u0430\u043B\u043E\u0432 \u0432\u0440\u0435\u043C\u0435\u043D\u0438 \u043D\u0435 \u0438\u043C\u0435\u0435\u0442 \u0441\u0442\u0440\u043E\u0433\u043E\u0439 \u043F\u0435\u0440\u0438\u043E\u0434\u0438\u0447\u043D\u043E\u0441\u0442\u0438. \n* \u0410\u0440\u043A\u0442\u0438\u0447\u0435\u0441\u043A\u0430\u044F \u043E\u0441\u0446\u0438\u043B\u043B\u044F\u0446\u0438\u044F \u0432 \u0437\u0438\u043C\u043D\u0438\u0435 \u0441\u0435\u0437\u043E\u043D\u044B 1899\u20132011 \u0433\u0433."@ru . "AO Precipitation.png"@en . "Die Arktische Oszillation (AO) (engl. auch Northern Hemispheric Annular Mode (NAM)) ist Ausdruck des Luftdruckgegensatzes zwischen den arktischen und den mittleren Breiten auf der Nordhemisph\u00E4re. Arktische und antarktische Oszillation sind gro\u00DFe Systeme der Telekonnektion der Erde, s. a. Polarwirbel."@de . . . . . . . "\uBD81\uADF9\uC9C4\uB3D9(\u5317\u6975\u632F\u52D5, arctic oscillation)\uC740 \uBD81\uADF9\uC5D0 \uC874\uC7AC\uD558\uB294 \uCC2C \uACF5\uAE30\uC758 \uADF9\uC18C\uC6A9\uB3CC\uC774\uAC00 \uC218\uC2ED \uC77C \uB610\uB294 \uC218\uC2ED \uB144\uC744 \uC8FC\uAE30\uB85C \uAC15\uC57D\uC744 \uB418\uD480\uC774\uD558\uB294 \uD604\uC0C1\uC774\uB2E4."@ko . . . . . . . "\uBD81\uADF9\uC9C4\uB3D9(\u5317\u6975\u632F\u52D5, arctic oscillation)\uC740 \uBD81\uADF9\uC5D0 \uC874\uC7AC\uD558\uB294 \uCC2C \uACF5\uAE30\uC758 \uADF9\uC18C\uC6A9\uB3CC\uC774\uAC00 \uC218\uC2ED \uC77C \uB610\uB294 \uC218\uC2ED \uB144\uC744 \uC8FC\uAE30\uB85C \uAC15\uC57D\uC744 \uB418\uD480\uC774\uD558\uB294 \uD604\uC0C1\uC774\uB2E4."@ko . . "200"^^ . . . . . "Oscillazione artica"@it . "The Arctic oscillation (AO) or Northern Annular Mode/Northern Hemisphere Annular Mode (NAM) is a weather phenomenon at the Arctic pole north of 20 degrees latitude. It is an important mode of climate variability for the Northern Hemisphere. The southern hemisphere analogue is called the Antarctic oscillation or Southern Annular Mode (SAM). The index varies over time with no particular periodicity, and is characterized by non-seasonal sea-level pressure anomalies of one sign in the Arctic, balanced by anomalies of opposite sign centered at about 37\u201345\u00B0 N."@en . "Arktische Oszillation"@de . . 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"\u5317\u6975\u632F\u52D5"@ja . "13574"^^ .