. "La arkta magneta poluso a\u016D norda magnetpoluso estas tiu punkto sur la tersurfaco de la norda hemisfero en kiu la tera magnetkampo direkti\u011Das vertikale suben. Tiu punkto varias depende de la tempo. \u011Cia kontra\u016Dparto en la suda hemisfero estas la Antarkta magneta poluso. \u0108ar la tera magnetkampo ne estas ekzakte simetria Arkta kaj Antarkta magnetpolusoj ne estas antipodaj (spegulsimetriaj tra la tercentro): linio inter amba\u016D magnetpolusoj preteriras la tercentron en distanco de 530 km. La plej okulfrapa fenomeno \u0109irka\u016D la magnetpolusoj estas la \"Polaraj lumoj\" (\"norda brilo\"). Ne konfuzu la arktan magnetpoluson kun la malpli konata Arkta geomagneta poluso, kiu estos priskribata poste."@eo . . . . "\u5317\u78C1\u6975"@ja . "\u039F \u03BC\u03B1\u03B3\u03BD\u03B7\u03C4\u03B9\u03BA\u03CC\u03C2 \u03B2\u03CC\u03C1\u03B5\u03B9\u03BF\u03C2 \u03C0\u03CC\u03BB\u03BF\u03C2 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03C4\u03BF \u03C3\u03B7\u03BC\u03B5\u03AF\u03BF \u03C0\u03BF\u03C5 \u03B4\u03B5\u03AF\u03C7\u03BD\u03BF\u03C5\u03BD \u03CC\u03BB\u03B5\u03C2 \u03BF\u03B9 \u03BC\u03B1\u03B3\u03BD\u03B7\u03C4\u03B9\u03BA\u03AD\u03C2 \u03B2\u03B5\u03BB\u03CC\u03BD\u03B5\u03C2 \u03C4\u03C9\u03BD \u03C0\u03C5\u03BE\u03AF\u03B4\u03C9\u03BD, \u03C0\u03BF\u03C5 \u03CC\u03BC\u03C9\u03C2 \u03B4\u03B5\u03BD \u03C4\u03B1\u03C5\u03C4\u03AF\u03B6\u03B5\u03C4\u03B1\u03B9 \u03BC\u03B5 \u03C4\u03BF\u03BD \u03B3\u03B5\u03C9\u03B3\u03C1\u03B1\u03C6\u03B9\u03BA\u03CC \u03B2\u03CC\u03C1\u03B5\u03B9\u03BF \u03C0\u03CC\u03BB\u03BF (\u03B4\u03B5\u03AF\u03C4\u03B5 \u03C3\u03C7\u03B5\u03C4\u03B9\u03BA\u03AC \u03BC\u03B1\u03B3\u03BD\u03B7\u03C4\u03B9\u03BA\u03CC\u03C2 \u03B2\u03BF\u03C1\u03C1\u03AC\u03C2). \u038C\u03C0\u03C9\u03C2 \u03BF\u03B9 \u03BC\u03B1\u03B3\u03BD\u03B7\u03C4\u03B9\u03BA\u03BF\u03AF \u03C0\u03CC\u03BB\u03BF\u03B9 \u03CC\u03BB\u03C9\u03BD \u03C4\u03C9\u03BD \u03C0\u03BB\u03B1\u03BD\u03B7\u03C4\u03CE\u03BD, \u03AD\u03C4\u03C3\u03B9 \u03BA\u03B1\u03B9 \u03C4\u03B7\u03C2 \u0393\u03B7\u03C2 \u03BC\u03B5\u03C4\u03B1\u03C4\u03BF\u03C0\u03AF\u03B6\u03B5\u03C4\u03B1\u03B9 \u03B5\u03BB\u03B1\u03C6\u03C1\u03AC, \u03B1\u03BB\u03BB\u03AC\u03B6\u03BF\u03BD\u03C4\u03B1\u03C2 \u03C3\u03C5\u03BD\u03B5\u03C7\u03CE\u03C2 \u03B8\u03AD\u03C3\u03B7 \u03B3\u03CD\u03C1\u03C9 \u03B1\u03C0\u03CC \u03C4\u03BF\u03BD \u03B3\u03B5\u03C9\u03B3\u03C1\u03B1\u03C6\u03B9\u03BA\u03CC \u03C0\u03CC\u03BB\u03BF. \u0391\u03C5\u03C4\u03CC \u03C3\u03C5\u03BC\u03B2\u03B1\u03AF\u03BD\u03B5\u03B9 \u03BB\u03CC\u03B3\u03C9 \u03C4\u03C9\u03BD \u03BA\u03B9\u03BD\u03AE\u03C3\u03B5\u03C9\u03BD \u03C3\u03C4\u03BF \u03B5\u03C3\u03C9\u03C4\u03B5\u03C1\u03B9\u03BA\u03CC \u03C4\u03B7\u03C2 \u03C4\u03BF \u03C1\u03B5\u03C5\u03C3\u03C4\u03BF\u03CD \u03C5\u03BB\u03B9\u03BA\u03BF\u03CD \u03C0\u03BF\u03C5 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03BA\u03C5\u03C1\u03AF\u03C9\u03C2 \u03C5\u03C0\u03B5\u03CD\u03B8\u03C5\u03BD\u03BF \u03B3\u03B9\u03B1 \u03C4\u03B7 \u03B4\u03B7\u03BC\u03B9\u03BF\u03C5\u03C1\u03B3\u03AF\u03B1 \u03BA\u03B1\u03B9 \u03C3\u03C5\u03BD\u03C4\u03AE\u03C1\u03B7\u03C3\u03B7 \u03C4\u03BF\u03C5 \u03BC\u03B1\u03B3\u03BD\u03B7\u03C4\u03B9\u03BA\u03BF\u03CD \u03C0\u03B5\u03B4\u03AF\u03BF\u03C5. \u03A3\u03CD\u03BC\u03C6\u03C9\u03BD\u03B1 \u03BC\u03B5 \u03BC\u03B5\u03C4\u03C1\u03AE\u03C3\u03B5\u03B9\u03C2 \u03C4\u03B7\u03C2 \u039A\u03B1\u03BD\u03B1\u03B4\u03B9\u03BA\u03AE\u03C2 \u039A\u03C5\u03B2\u03AD\u03C1\u03BD\u03B7\u03C3\u03B7\u03C2, \u03BF \u03BC\u03B1\u03B3\u03BD\u03B7\u03C4\u03B9\u03BA\u03CC\u03C2 \u03B2\u03CC\u03C1\u03B5\u03B9\u03BF\u03C2 \u03C0\u03CC\u03BB\u03BF\u03C2 \u03C3\u03C5\u03BD\u03B5\u03C7\u03AF\u03B6\u03B5\u03B9 \u03BD\u03B1 \u03BC\u03B5\u03C4\u03B1\u03BA\u03B9\u03BD\u03B5\u03AF\u03C4\u03B1\u03B9 \u03B2\u03CC\u03C1\u03B5\u03B9\u03B1. \u03A4\u03BF 1996 \u03C4\u03BF \u03C3\u03B7\u03BC\u03B5\u03AF\u03BF \u03C4\u03BF\u03C5 \u03B2\u03C1\u03AD\u03B8\u03B7\u03BA\u03B5 \u03C3\u03C4\u03BF \u03B3\u03B5\u03C9\u03B3\u03C1\u03B1\u03C6\u03B9\u03BA\u03CC \u03C3\u03C4\u03AF\u03B3\u03BC\u03B1 78\u00B035.7\u2032 N, 104\u00B011.9\u2032 W. \u03A4\u03BF 2005 \u03B2\u03C1\u03AD\u03B8\u03B7\u03BA\u03B5 \u03C3\u03C4\u03BF 82\u00B007\u2032 N, 114\u00B004\u2032 W. \u039A\u03B1\u03C4\u03AC \u03C4\u03B7 \u03B4\u03B9\u03AC\u03C1\u03BA\u03B5\u03B9\u03B1 \u03C4\u03BF\u03C5 20\u03BF\u03C5 \u03B1\u03B9\u03CE\u03BD\u03B1 \u03BC\u03B5\u03C4\u03B1\u03BA\u03B9\u03BD\u03AE\u03B8\u03B7\u03BA\u03B5 1100 \u03C7\u03B9\u03BB\u03B9\u03CC\u03BC\u03B5\u03C4\u03C1\u03B1, \u03BA\u03B1\u03B9 \u03BC\u03B5\u03C4\u03AC \u03C4\u03BF 1970 \u03B7 \u03BC\u03B5\u03C4\u03B1\u03BA\u03AF\u03BD\u03B7\u03C3\u03AE \u03C4\u03BF\u03C5 \u03B5\u03C0\u03B9\u03C4\u03B1\u03C7\u03CD\u03BD\u03B8\u03B7\u03BA\u03B5 \u03B1\u03C0\u03CC \u03C4\u03B1 9 \u03C7\u03BB\u03BC/\u03AD\u03C4\u03BF\u03C2 \u03C3\u03C4\u03B1 41 \u03C7\u03BB\u03BC/\u03AD\u03C4\u03BF\u03C2. \u0395\u03AC\u03BD \u03C3\u03C5\u03BD\u03B5\u03C7\u03AF\u03C3\u03B5\u03B9 \u03BC\u03B5 \u03B1\u03C5\u03C4\u03CC \u03C4\u03BF \u03C1\u03C5\u03B8\u03BC\u03CC, \u03B1\u03BD\u03B1\u03BC\u03AD\u03BD\u03B5\u03C4\u03B1\u03B9 \u03C3\u03B5 48\u03C7\u03C1\u03CC\u03BD\u03B9\u03B1 \u03BD\u03B1 \u03B2\u03C1\u03AF\u03C3\u03BA\u03B5\u03C4\u03B1\u03B9 \u03C3\u03C4\u03B7 \u03A3\u03B9\u03B2\u03B7\u03C1\u03AF\u03B1. \u03A0\u03AC\u03BD\u03C4\u03C9\u03C2, \u03BC\u03B5\u03BB\u03AD\u03C4\u03B5\u03C2 \u03B4\u03B5\u03AF\u03C7\u03BD\u03BF\u03C5\u03BD \u03CC\u03C4\u03B9 \u03BF \u03C1\u03C5\u03B8\u03BC\u03CC\u03C2 \u03B1\u03C5\u03C4\u03CC\u03C2 \u03B8\u03B1 \u03B5\u03C0\u03B9\u03B2\u03C1\u03B1\u03B4\u03C5\u03BD\u03B8\u03B5\u03AF."@el . . "-110.8000030517578"^^ . . . . . . . . "Iparburu magnetikoa edo ipar polo magnetikoa Lurraren ipar hemisferioko azaleko puntu mugikor bat da, non planetaren eremu magnetikoak beherantz jotzen duen bertikalki (hau da, iparrorratz magnetiko baten orratzari ardatz horizontalean biratzen uzten bazaio, zuzen beherantz seinalatuko du). Hori toki bakar batean gertatzen da, iparburu geografikotik eta iparburu geomagnetikotatik hurbil (baina bi horietatik bereizita)."@eu . . . . . . . . . . "El polo norte magn\u00E9tico es la direcci\u00F3n que se\u00F1ala la aguja imantada de una br\u00FAjula, direcci\u00F3n que no coincide con la del polo norte geogr\u00E1fico, excepto en los puntos del hemisferio norte, situados en el mismo meridiano que el norte magn\u00E9tico. Actualmente est\u00E1 situado a unos 1600 km del polo norte geogr\u00E1fico, cerca de la isla de Bathurst, en la parte septentrional de Canad\u00E1, en el territorio de Nunavut."@es . "\u5317\u78C1\u6975\uFF08\u307B\u304F\u3058\u304D\u3087\u304F\u3001\u82F1: North Magnetic Pole\uFF09\u3068\u306F\u3001\u5929\u4F53\u306E\u5317\u534A\u7403\u306E\u5730\u8868\u9762\u3067\u3001\u78C1\u529B\u7DDA\u306E\u65B9\u5411\u304C\u925B\u76F4\u306B\u306A\u3063\u3066\u3044\u308B\u5730\u70B9\u3067\u3042\u308B\u3002\u78C1\u5317\u6975\uFF08\u3058\u307B\u3063\u304D\u3087\u304F\uFF09\u3068\u3082\u3044\u3046\u3002\u4EE5\u4E0B\u3001\u7279\u306B\u65AD\u3089\u306A\u3044\u9650\u308A\u3001\u5730\u7403\u306E\u5317\u78C1\u6975\u306B\u3064\u3044\u3066\u8FF0\u3079\u308B\u3002"@ja . . "\uC790\uBD81\uADF9(\u78C1\u5317\u6975) \uB610\uB294 \uC790\uBD81(\u78C1\u5317)\uC740 \uC9C0\uAD6C\uC758 \uC790\uAE30\uC7A5\uC774 \uC218\uC9C1\uC758 \uC544\uB798 \uBC29\uD5A5\uC73C\uB85C \uAC00\uB9AC\uD0A4\uB294 \uC9C0\uAD6C \uD45C\uBA74\uC758 \uC9C0\uC810\uC73C\uB85C, \uC2DC\uAC04\uC774 \uC9C0\uB0A8\uC5D0 \uB530\uB77C \uC810\uC810 \uC774\uB3D9\uD55C\uB2E4. \uC790\uBD81\uC740 \uD754\uD788 '\uC9C0\uC790\uAE30 \uBD81\uADF9(Geomagnetic pole)'\uACFC \uD63C\uB3D9\uB418\uAE30\uB3C4 \uD55C\uB2E4. 2005\uB144\uC758 \uC790\uBD81\uC740 \uCE90\uB098\uB2E4 \uBD81\uBD80\uC758 \uC5D8\uC988\uBBF8\uC5B4\uC12C \uBD80\uADFC(\uBD81\uC704 82.7\u00B0, \uC11C\uACBD 114.4\u00B0)\uC5D0 \uB193\uC5EC \uC788\uC5C8\uB2E4. \uC9C0\uAD6C \uC790\uAE30\uB294 \uC644\uBCBD\uD55C \uB300\uCE6D\uC774 \uC544\uB2C8\uBBC0\uB85C, \uC790\uBD81\uACFC \uADF8 \uBC18\uB300 \uC9C0\uC810\uC778 \uC790\uB0A8\uC740 \uC9C0\uB9AC\uC0C1 \uC815\uBC18\uB300\uC5D0 \uC788\uC9C0 \uC54A\uB2E4. \uC790\uBD81\uC5D0\uC11C \uC790\uB0A8\uC744 \uC9C0\uB098\uB294 \uC120\uC740 \uC9C0\uAD6C\uC758 \uC911\uC2EC\uC744 \uC9C0\uB098\uC9C0 \uC54A\uC73C\uBA70, \uC2E4\uC81C\uB85C\uB294 \uC57D 530km \uB5A8\uC5B4\uC9C4 \uACF3\uC744 \uC9C0\uB098\uAC04\uB2E4."@ko . . . . "O Polo Norte magn\u00E9tico \u00E9 um ponto vari\u00E1vel \u00E0 superf\u00EDcie da Terra para o qual as linhas do campo magn\u00E9tico que envolvem o planeta terra apontam que, por mera conven\u00E7\u00E3o, localiza-se em algum ponto do hemisf\u00E9rio norte. Nesse sentido, polo norte magn\u00E9tico n\u00E3o deve ser confundido com o menos conhecido Polo norte geomagn\u00E9tico (explicado abaixo) e nem com o secular Polo Norte Astron\u00F4mico. Em 2005 o polo norte magn\u00E9tico situava-se pr\u00F3xima da Ilha Ellesmere no norte do Canad\u00E1, aproximadamente em 82.7\u00B0 N 114.4\u00B0 O. O ponto correspondente no hemisf\u00E9rio sul \u00E9 o Polo sul magn\u00E9tico. Uma vez que o campo magn\u00E9tico terrestre n\u00E3o \u00E9 propriamente sim\u00E9trico, os polos magn\u00E9ticos n\u00E3o s\u00E3o ant\u00EDpodas um do outro: a linha que os une n\u00E3o passa no centro da Terra (fica a cerca de 530 km).E tamb\u00E9m \u00E9 para aonde as b\u00FAssolas apontam normalmente."@pt . . . "\u0421\u0435\u0301\u0432\u0435\u0440\u043D\u044B\u0439 \u043C\u0430\u0433\u043D\u0438\u0301\u0442\u043D\u044B\u0439 \u043F\u043E\u0301\u043B\u044E\u0441 \u2014 \u0443\u0441\u043B\u043E\u0432\u043D\u0430\u044F \u0442\u043E\u0447\u043A\u0430 \u0432 \u0441\u0435\u0432\u0435\u0440\u043D\u043E\u0439 \u043F\u043E\u043B\u044F\u0440\u043D\u043E\u0439 \u043E\u0431\u043B\u0430\u0441\u0442\u0438 \u0437\u0435\u043C\u043D\u043E\u0439 \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u043E\u0441\u0442\u0438, \u0432 \u043A\u043E\u0442\u043E\u0440\u043E\u0439 \u043C\u0430\u0433\u043D\u0438\u0442\u043D\u043E\u0435 \u043F\u043E\u043B\u0435 \u0417\u0435\u043C\u043B\u0438 \u043D\u0430\u043F\u0440\u0430\u0432\u043B\u0435\u043D\u043E \u0441\u0442\u0440\u043E\u0433\u043E \u0432\u043D\u0438\u0437 (\u043F\u043E\u0434 \u0443\u0433\u043B\u043E\u043C 90\u00B0 \u043A \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u043E\u0441\u0442\u0438)."@ru . . . . . . . . . . . . "Le p\u00F4le Nord magn\u00E9tique de la Terre est un point errant unique sur la surface o\u00F9 le champ magn\u00E9tique terrestre pointe vers le bas. C'est-\u00E0-dire que le \u00AB Dip \u00BB (plongeon) est de 90\u00B0. L'aiguille d'une boussole pointe approximativement vers ce lieu (plus ou moins approximativement suivant le lieu o\u00F9 on se trouve ; exactement la boussole est tangente \u00E0 la ligne de champ). Ne pas confondre le p\u00F4le nord magn\u00E9tique, qui est un point, avec le nord magn\u00E9tique qui est la direction du nord donn\u00E9e par une boussole."@fr . "Magnetiska nordpolen (egentligen nordpolens magnetiska pol, som \u00E4r en sydpol) \u00E4r den punkt p\u00E5 jordytan p\u00E5 norra halvklotet d\u00E4r inklinationen \u00E4r 90\u00B0, s\u00E5 att den horisontella komposanten i jordens magnetf\u00E4lt \u00E4r noll och en perfekt kompassn\u00E5l d\u00E4rmed vill peka rakt ned\u00E5t. Denna magnetiska pol ligger inte vid den geografiska nordpolen, utan ungef\u00E4r 190 mil s\u00F6der om den geografiska nordpolen. En kompass p\u00E5 jordytan l\u00E5ngt fr\u00E5n den magnetiska nordpolen inriktar sig efter magnetf\u00E4ltet p\u00E5 den plats den befinner sig och pekar mot den punkt d\u00E4r jordens magnetiska dipolaxel sk\u00E4r jordytan, vilken ibland kallas den geomagnetiska polen. Att dessa poler inte sammanfaller beror p\u00E5 oj\u00E4mnheter i jordens magnetf\u00E4lt. Resultatet \u00E4r att kompassens nordpol p\u00E5 de flesta st\u00E4llen p\u00E5 jorden varken pekar mot den geografiska nordpolen eller mot den magnetiska polen i dennas n\u00E4rhet. Beteckningen \"magnetiska nordpolen\" \u00E4r en praktisk konvention. Man har kommit att beteckna den pol som kompassn\u00E5lens nordpil pekar mot som magnetiska nordpolen, \u00E4ven om den i fysikens mening \u00E4r en magnetisk sydpol \u2013 motsatt polaritet attraherar, samma polaritet repellerar. P\u00E5 samma s\u00E4tt \u00E4r det som konventionellt kallas \"magnetiska sydpolen\" enligt fysiken en magnetisk nordpol. Det som refereras till som den magnetiska nordpolen (jordens magnetiska sydpol) ligger f\u00F6r n\u00E4rvarande i norra Kanada, d\u00E4r den p\u00E5 kartan har r\u00F6rt sig i nordlig riktning. Fr\u00E5n Sveriges horisont har den r\u00F6rt sig l\u00E5ngsamt v\u00E4sterut - med ca 1/2 grad \u00F6ver en tio\u00E5rsperiod. Jordens magnetf\u00E4lt har aldrig varit konstant utan har bytt riktning vid ett stort antal tillf\u00E4llen i jordens historia. Nord\u00E4ndan p\u00E5 magnetisk kompassn\u00E5l pekar i verkligheten varken mot den magnetiska eller den geografiska nordpolen. Riktningsavvikelsen till den geografiska nordpolen kallas missvisning. Ett avl\u00E4st v\u00E4rde p\u00E5 en magnetkompass m\u00E5ste d\u00E4rf\u00F6r korrigeras p\u00E5 de flesta platser p\u00E5 jorden f\u00F6r att vara anv\u00E4ndbart. I Sverige \u00E4r missvisningen f\u00F6r n\u00E4rvarande (2008) relativt liten - fr\u00E5n omkring 8 grader plus i Haparanda till n\u00E5gon grad plus vid v\u00E4stkusten - men i omr\u00E5den n\u00E4rmare jordens magnetiska poler kan den vara avsev\u00E4rd vilket g\u00F6r det sv\u00E5rt eller om\u00F6jligt att anv\u00E4nda magnetkompasser i s\u00E5dana omr\u00E5den."@sv . . "O Polo Norte magn\u00E9tico \u00E9 um ponto vari\u00E1vel \u00E0 superf\u00EDcie da Terra para o qual as linhas do campo magn\u00E9tico que envolvem o planeta terra apontam que, por mera conven\u00E7\u00E3o, localiza-se em algum ponto do hemisf\u00E9rio norte. Nesse sentido, polo norte magn\u00E9tico n\u00E3o deve ser confundido com o menos conhecido Polo norte geomagn\u00E9tico (explicado abaixo) e nem com o secular Polo Norte Astron\u00F4mico."@pt . "Iparburu magnetikoa edo ipar polo magnetikoa Lurraren ipar hemisferioko azaleko puntu mugikor bat da, non planetaren eremu magnetikoak beherantz jotzen duen bertikalki (hau da, iparrorratz magnetiko baten orratzari ardatz horizontalean biratzen uzten bazaio, zuzen beherantz seinalatuko du). Hori toki bakar batean gertatzen da, iparburu geografikotik eta iparburu geomagnetikotatik hurbil (baina bi horietatik bereizita). Iparburu magnetikoa denborarekin mugituz doa, Lurraren nukleoan gertatzen diren aldaketa magnetikoen eraginez. 2001ean, Kanadaren Geologia Ikerketak zehaztu zuen iparburu magnetikoa Ellesmere uhartearen mendebaldean zegoela, Kanada iparraldean, 81\u00B018\u2032N 110\u00B048\u2032W\uFEFF / \uFEFF81.300\u00B0N 110.800\u00B0W koordenatuetan. 2005ean, 83\u00B006\u2032N 117\u00B048\u2032W\uFEFF / \uFEFF83.100\u00B0N 117.800\u00B0W koordenatuetan zegoen. 2009an, oraindik Kanadako artikoaren barruan zegoen, 84\u00B054\u2032N 131\u00B000\u2032W\uFEFF / \uFEFF84.900\u00B0N 131.000\u00B0W koordenatuetan, baina urtean 55 - 60 kilometro mugitzen ari zen Errusia alderantz. Egindako proiekzioek ziotenez, 2019 urtetik aurrera iparburua Kanadako artikotik kanpo egotekoa zen, 86\u00B026\u203252.8\u2033N 175\u00B020\u203245.06\u2033E\uFEFF / \uFEFF86.448000\u00B0N 175.3458500\u00B0E koordenatuetan. Iparburu magnetikoaren hego hemisferioko kidekoa da. Lurraren eremu magnetikoa guztiz simetrikoa ez denez, ipar eta hego buru magnetikoak ez dira antipodalak, hau da, batetik bestera marraztutako lerro zuzen bat ez da Lurraren erdigune geometrikotik igaroko."@eu . . . . . . . "\u041F\u0456\u0432\u043D\u0456\u0447\u043D\u0438\u0439 \u043C\u0430\u0433\u043D\u0456\u0442\u043D\u0438\u0439 \u043F\u043E\u043B\u044E\u0441"@uk . "\u0627\u0644\u0642\u0637\u0628 \u0627\u0644\u0634\u0645\u0627\u0644\u064A \u0627\u0644\u0645\u063A\u0646\u0627\u0637\u064A\u0633\u064A \u0647\u0648 \u0646\u0642\u0637\u0629 \u0639\u0644\u0649 \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636 \u062A\u0642\u0639 \u0641\u064A \u0646\u0635\u0641 \u0627\u0644\u0623\u0631\u0636 \u0627\u0644\u0634\u0645\u0627\u0644\u064A \u0648\u064A\u0643\u0648\u0646 \u0639\u0646\u062F\u0647\u0627 \u0627\u062A\u062C\u0627\u0647 \u0627\u0644\u062D\u0642\u0644 \u0627\u0644\u0645\u063A\u0646\u0627\u0637\u064A\u0633\u064A \u0627\u0644\u0623\u0631\u0636\u064A \u0639\u0645\u0648\u062F\u064A\u0627\u064B \u0628\u0627\u062A\u062C\u0627\u0647 \u0627\u0644\u0623\u0633\u0641\u0644\u060C \u0623\u064A \u0623\u0646\u0647 \u0625\u0630\u0627 \u0633\u0645\u062D \u0644\u0628\u0648\u0635\u0644\u0629 \u0623\u0646 \u062A\u062F\u0648\u0631 \u0628\u0634\u0643\u0644 \u062D\u0631 \u0641\u0625\u0646\u0647\u0627 \u0633\u062A\u062A\u062C\u0647 \u0646\u062D\u0648 \u0627\u0644\u0623\u0633\u0641\u0644. \u062A\u0642\u0639 \u0647\u0630\u0647 \u0627\u0644\u0645\u0646\u0637\u0642\u0629 \u0628\u0627\u0644\u0642\u0631\u0628 \u0645\u0646 \u0627\u0644\u0642\u0637\u0628 \u0627\u0644\u0634\u0645\u0627\u0644\u064A \u0627\u0644\u062C\u063A\u0631\u0627\u0641\u064A\u060C \u0648\u0647\u064A \u063A\u064A\u0631 \u062B\u0627\u0628\u062A\u0629 \u0641\u064A \u0645\u0643\u0627\u0646\u0647\u0627 \u0648\u062A\u062A\u062D\u0631\u0643 \u0645\u0639 \u0645\u0631\u0648\u0631 \u0627\u0644\u0648\u0642\u062A \u0628\u0633\u0628\u0628 \u062D\u062F\u0648\u062B \u062A\u063A\u064A\u0631\u0627\u062A \u0645\u063A\u0646\u0627\u0637\u064A\u0633\u064A\u0629 \u0641\u064A \u0627\u0644\u0644\u0628 \u0627\u0644\u062E\u0627\u0631\u062C\u064A \u0644\u0644\u0623\u0631\u0636."@ar . . . "30871810"^^ . "POINT(-110.80000305176 81.300003051758)"^^ . . . . . "81.3 -110.8" . . . . "Polo norte magn\u00E9tico"@es . . . . . . . . "Severn\u00ED geomagnetick\u00FD p\u00F3lje m\u00EDsto, kde osa magnetick\u00E9ho dip\u00F3lu nejl\u00E9pe aproximuj\u00EDc\u00EDho zemsk\u00E9 magnetick\u00E9 pole prot\u00EDn\u00E1 na severu povrch Zem\u011B. Le\u017E\u00ED v severoz\u00E1padn\u00EDm Gr\u00F3nsku na 79\u00B0 severn\u00ED \u0161\u00ED\u0159ky a 290\u00B0 v\u00FDchodn\u00ED d\u00E9lky, \u010Dili asi 1 250 km od geografick\u00E9ho severn\u00EDho p\u00F3lu. Osa tohoto dip\u00F3lu sv\u00EDr\u00E1 \u00FAhel 11\u00B0 s zemskou osou, dip\u00F3l m\u00E1 magnetick\u00FD moment 8,0.1022 J T\u22121. S \u010Dasem se poloha t\u00E9to osy m\u011Bn\u00ED. Severn\u00ED magnetick\u00FD p\u00F3l je pohybuj\u00EDc\u00ED se m\u00EDsto na Zemi, ze kter\u00E9ho induk\u010Dn\u00ED \u010D\u00E1ry geomagnetick\u00E9ho pole sm\u011B\u0159uj\u00ED svisle vzh\u016Fru. Magnetick\u00E1 inklinace je zde +90\u00B0; magnetick\u00E1 deklinace zde nen\u00ED definov\u00E1na, sb\u00EDhaj\u00ED se zde v\u0161echny izogonick\u00E9 linie. Magnetick\u00FD p\u00F3l na severn\u00ED polokouli je fyzik\u00E1ln\u011B ji\u017En\u00ED p\u00F3l. Magnetick\u00FD sever a jih byly toti\u017E definov\u00E1ny podle orientace st\u0159elky kompasu. Severn\u00ED p\u00F3l st\u0159elky je tedy p\u0159itahov\u00E1n ji\u017En\u00EDm magnetick\u00FDm p\u00F3lem Zem\u011B. Severn\u00ED magnetick\u00FD p\u00F3l nen\u00ED p\u0159esn\u011B protilehl\u00FD v\u016F\u010Di ji\u017En\u00EDmu magnetick\u00E9mu p\u00F3lu, jejich spojnice neproch\u00E1z\u00ED st\u0159edem Zem\u011B, oba se nach\u00E1zej\u00ED na z\u00E1padn\u00ED polokouli."@cs . . "Severn\u00ED geomagnetick\u00FD p\u00F3l"@cs . . . . . . . . . "Pol nord magn\u00E8tic"@ca . "\u5317\u78C1\u6975\uFF08\u307B\u304F\u3058\u304D\u3087\u304F\u3001\u82F1: North Magnetic Pole\uFF09\u3068\u306F\u3001\u5929\u4F53\u306E\u5317\u534A\u7403\u306E\u5730\u8868\u9762\u3067\u3001\u78C1\u529B\u7DDA\u306E\u65B9\u5411\u304C\u925B\u76F4\u306B\u306A\u3063\u3066\u3044\u308B\u5730\u70B9\u3067\u3042\u308B\u3002\u78C1\u5317\u6975\uFF08\u3058\u307B\u3063\u304D\u3087\u304F\uFF09\u3068\u3082\u3044\u3046\u3002\u4EE5\u4E0B\u3001\u7279\u306B\u65AD\u3089\u306A\u3044\u9650\u308A\u3001\u5730\u7403\u306E\u5317\u78C1\u6975\u306B\u3064\u3044\u3066\u8FF0\u3079\u308B\u3002"@ja . "\u041F\u0456\u0432\u043D\u0456\u0447\u043D\u0438\u0439 \u043C\u0430\u0433\u043D\u0456\u0442\u043D\u0438\u0439 \u043F\u043E\u043B\u044E\u0441 \u2014 \u0443\u043C\u043E\u0432\u043D\u0430 \u0442\u043E\u0447\u043A\u0430 \u043D\u0430 \u0437\u0435\u043C\u043D\u0456\u0439 \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u0456, \u0432 \u044F\u043A\u0456\u0439 \u043C\u0430\u0433\u043D\u0456\u0442\u043D\u0435 \u043F\u043E\u043B\u0435 \u0417\u0435\u043C\u043B\u0456 \u0441\u043F\u0440\u044F\u043C\u043E\u0432\u0430\u043D\u043E \u043F\u0440\u044F\u043C\u043E\u0432\u0438\u0441\u043D\u043E (\u043F\u0456\u0434 \u043A\u0443\u0442\u043E\u043C 90 \u00B0 \u0434\u043E \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u0456). \u0421\u043B\u0456\u0434 \u0437\u0430\u0437\u043D\u0430\u0447\u0438\u0442\u0438, \u0449\u043E \u0437 \u0444\u0456\u0437\u0438\u0447\u043D\u043E\u0433\u043E \u043F\u043E\u0433\u043B\u044F\u0434\u0443 \u0446\u0435\u0439 \u043F\u043E\u043B\u044E\u0441 \u0454 \u00AB\u043F\u0456\u0432\u0434\u0435\u043D\u043D\u0438\u043C\u00BB, \u043E\u0441\u043A\u0456\u043B\u044C\u043A\u0438 \u043F\u0440\u0438\u0442\u044F\u0433\u0443\u0454 \u043F\u0456\u0432\u043D\u0456\u0447\u043D\u0438\u0439 \u043F\u043E\u043B\u044E\u0441 \u0441\u0442\u0440\u0456\u043B\u043A\u0438 \u043A\u043E\u043C\u043F\u0430\u0441\u0430."@uk . . "\u5730\u78C1\u5317\u6781\u662F\u5730\u7403\u8868\u9762\u5730\u7403\u78C1\u573A\u65B9\u5411\u5782\u76F4\u5411\u4E0B\u7684\u70B9\u3002\u5730\u78C1\u5317\u6781\u4E0E\u5730\u7406\u5317\u6781\u5E76\u4E0D\u76F8\u540C\u3002\u5730\u78C1\u5317\u6781\u6B63\u5728\u4E0D\u65B7\u7684\u6539\u8B8A\uFF0C\u4EE5\u6BCF\u592920.5\u516C\u5C3A\u7684\u901F\u5EA6\u79FB\u52D5\u3002\u53E6\u5916\uFF0C\u7531\u4E8E\u5730\u7403\u78C1\u573A\u5E76\u4E0D\u662F\u5B8C\u5168\u5BF9\u79F0\u7684\uFF0C\u5730\u78C1\u5317\u6781\u4E0E\u5730\u78C1\u5357\u6781\u5E76\u4E0D\u662F\u5904\u5728\u5BF9\u8E60\u70B9\u4F4D\u7F6E\u4E0A\u3002 \n* 2001\u5E74\uFF0C\u5730\u78C1\u5317\u6781\u5904\u4E8E\u5728\u52A0\u62FF\u5927\u5317\u90E8\u57C3\u5C14\u65AF\u7C73\u5C14\u5C9B\u9644\u8FD1\uFF0C\u7ECF\u7EAC\u5EA6\u4E3A81\u00B018\u2032N 110\u00B048\u2032W\uFEFF / \uFEFF81.3\u00B0N 110.8\u00B0W \n* 2005\u5E74\uFF0C\u5730\u78C1\u5317\u6781\u4F4D\u7F6E\u5728\u52A0\u62FF\u5927\u5317\u65B9\u7684\u5317\u51B0\u6D0B\u4E0A\uFF0C\u7D93\u7DEF\u5EA6\u70BA83\u00B006\u2032N 117\u00B048\u2032W\uFEFF / \uFEFF83.1\u00B0N 117.8\u00B0W \n* 2009\u5E74\uFF0C\u5730\u78C1\u5317\u6781\u5411\u5317\u79FB\u52D5\uFF0C\u7D93\u7DEF\u5EA6\u70BA84\u00B054\u2032N 141\u00B000\u2032W\uFEFF / \uFEFF84.9\u00B0N 141.0\u00B0W \n* 2016\u5E74\uFF0C\u5730\u78C1\u5317\u6975\u6301\u7E8C\u5F80\u4FC4\u7F85\u65AF\u79FB\u52D5\uFF0C\u7D93\u7DEF\u5EA6\u70BA86\u00B024\u2032N 166\u00B018\u2032W\uFEFF / \uFEFF86.4\u00B0N 166.3\u00B0W \u53E6\u5916\u9700\u8981\u6CE8\u610F\u7684\u662F\u5730\u78C1\u5317\u6781\u5B9E\u9645\u662F\u7269\u7406\u4E0A\u7684\u78C1\u573A\u5357\u6781\u3002\u51FA\u73B0\u8FD9\u79CD\u72B6\u51B5\u7684\u539F\u56E0\u662F\u4EBA\u4EEC\u5728\u53D1\u73B0\u78C1\u6781\u5F02\u6027\u76F8\u5438\u3001\u540C\u6027\u76F8\u65A5\u7684\u89C4\u5F8B\u4E4B\u524D\u5C31\u5B9A\u4E49\u4E86\u5730\u78C1\u5317\u6781\u8FD9\u4E2A\u540D\u8BCD\u3002\u9996\u5148\uFF0C\u4EBA\u4EEC\u5B9A\u4E49\u4E86\u6307\u5357\u9488\u6307\u5411\u5730\u7406\u5317\u6781\u7684\u4E00\u7AEF\u4E3A\u78C1\u573A\u5317\u6781\uFF0C\u7531\u4E8E\u8FD9\u4E2A\u5B9A\u4E49\u662F\u968F\u610F\u7684\uFF0C\u56E0\u6B64\u662F\u53EF\u4EE5\u63A5\u53D7\u7684\u3002\u7136\u540E\uFF0C\u4EBA\u4EEC\u6839\u636E\u5317\u65B9\u7684\u5730\u78C1\u573A\u6781\u70B9\u63A5\u8FD1\u5730\u7406\u5317\u6781\u7684\u77E5\u8BC6\uFF0C\u5B9A\u4E49\u4E86\u8FD9\u4E2A\u6781\u70B9\u4E3A\u5730\u78C1\u5317\u6781\u3002\u53EF\u662F\uFF0C\u5F53\u4EBA\u4EEC\u6700\u540E\u53D1\u73B0\u78C1\u573A\u539F\u6765\u662F\u540C\u6027\u76F8\u65A5\u7684\u89C4\u5F8B\u4EE5\u540E\uFF0C\u5730\u78C1\u5317\u6781\u4E5F\u5C31\u53EA\u80FD\u4F5C\u4E3A\u4E60\u60EF\u7528\u6CD5\u88AB\u4FDD\u7559\u4E0B\u6765\u4E86\u3002\u76F8\u5E94\u5730\uFF0C\u5730\u78C1\u5357\u6781\u5B9E\u9645\u4E0A\u662F\u7269\u7406\u4E0A\u7684\u78C1\u573A\u5317\u6781\u3002"@zh . . "1121584171"^^ . "\u0627\u0644\u0642\u0637\u0628 \u0627\u0644\u0634\u0645\u0627\u0644\u064A \u0627\u0644\u0645\u063A\u0646\u0627\u0637\u064A\u0633\u064A"@ar . . . . . . . . . . . . . . . . "81.30000305175781"^^ . . . . "North magnetic pole"@en . . . . . "\u5730\u78C1\u5317\u6781\u662F\u5730\u7403\u8868\u9762\u5730\u7403\u78C1\u573A\u65B9\u5411\u5782\u76F4\u5411\u4E0B\u7684\u70B9\u3002\u5730\u78C1\u5317\u6781\u4E0E\u5730\u7406\u5317\u6781\u5E76\u4E0D\u76F8\u540C\u3002\u5730\u78C1\u5317\u6781\u6B63\u5728\u4E0D\u65B7\u7684\u6539\u8B8A\uFF0C\u4EE5\u6BCF\u592920.5\u516C\u5C3A\u7684\u901F\u5EA6\u79FB\u52D5\u3002\u53E6\u5916\uFF0C\u7531\u4E8E\u5730\u7403\u78C1\u573A\u5E76\u4E0D\u662F\u5B8C\u5168\u5BF9\u79F0\u7684\uFF0C\u5730\u78C1\u5317\u6781\u4E0E\u5730\u78C1\u5357\u6781\u5E76\u4E0D\u662F\u5904\u5728\u5BF9\u8E60\u70B9\u4F4D\u7F6E\u4E0A\u3002 \n* 2001\u5E74\uFF0C\u5730\u78C1\u5317\u6781\u5904\u4E8E\u5728\u52A0\u62FF\u5927\u5317\u90E8\u57C3\u5C14\u65AF\u7C73\u5C14\u5C9B\u9644\u8FD1\uFF0C\u7ECF\u7EAC\u5EA6\u4E3A81\u00B018\u2032N 110\u00B048\u2032W\uFEFF / \uFEFF81.3\u00B0N 110.8\u00B0W \n* 2005\u5E74\uFF0C\u5730\u78C1\u5317\u6781\u4F4D\u7F6E\u5728\u52A0\u62FF\u5927\u5317\u65B9\u7684\u5317\u51B0\u6D0B\u4E0A\uFF0C\u7D93\u7DEF\u5EA6\u70BA83\u00B006\u2032N 117\u00B048\u2032W\uFEFF / \uFEFF83.1\u00B0N 117.8\u00B0W \n* 2009\u5E74\uFF0C\u5730\u78C1\u5317\u6781\u5411\u5317\u79FB\u52D5\uFF0C\u7D93\u7DEF\u5EA6\u70BA84\u00B054\u2032N 141\u00B000\u2032W\uFEFF / \uFEFF84.9\u00B0N 141.0\u00B0W \n* 2016\u5E74\uFF0C\u5730\u78C1\u5317\u6975\u6301\u7E8C\u5F80\u4FC4\u7F85\u65AF\u79FB\u52D5\uFF0C\u7D93\u7DEF\u5EA6\u70BA86\u00B024\u2032N 166\u00B018\u2032W\uFEFF / \uFEFF86.4\u00B0N 166.3\u00B0W \u53E6\u5916\u9700\u8981\u6CE8\u610F\u7684\u662F\u5730\u78C1\u5317\u6781\u5B9E\u9645\u662F\u7269\u7406\u4E0A\u7684\u78C1\u573A\u5357\u6781\u3002\u51FA\u73B0\u8FD9\u79CD\u72B6\u51B5\u7684\u539F\u56E0\u662F\u4EBA\u4EEC\u5728\u53D1\u73B0\u78C1\u6781\u5F02\u6027\u76F8\u5438\u3001\u540C\u6027\u76F8\u65A5\u7684\u89C4\u5F8B\u4E4B\u524D\u5C31\u5B9A\u4E49\u4E86\u5730\u78C1\u5317\u6781\u8FD9\u4E2A\u540D\u8BCD\u3002\u9996\u5148\uFF0C\u4EBA\u4EEC\u5B9A\u4E49\u4E86\u6307\u5357\u9488\u6307\u5411\u5730\u7406\u5317\u6781\u7684\u4E00\u7AEF\u4E3A\u78C1\u573A\u5317\u6781\uFF0C\u7531\u4E8E\u8FD9\u4E2A\u5B9A\u4E49\u662F\u968F\u610F\u7684\uFF0C\u56E0\u6B64\u662F\u53EF\u4EE5\u63A5\u53D7\u7684\u3002\u7136\u540E\uFF0C\u4EBA\u4EEC\u6839\u636E\u5317\u65B9\u7684\u5730\u78C1\u573A\u6781\u70B9\u63A5\u8FD1\u5730\u7406\u5317\u6781\u7684\u77E5\u8BC6\uFF0C\u5B9A\u4E49\u4E86\u8FD9\u4E2A\u6781\u70B9\u4E3A\u5730\u78C1\u5317\u6781\u3002\u53EF\u662F\uFF0C\u5F53\u4EBA\u4EEC\u6700\u540E\u53D1\u73B0\u78C1\u573A\u539F\u6765\u662F\u540C\u6027\u76F8\u65A5\u7684\u89C4\u5F8B\u4EE5\u540E\uFF0C\u5730\u78C1\u5317\u6781\u4E5F\u5C31\u53EA\u80FD\u4F5C\u4E3A\u4E60\u60EF\u7528\u6CD5\u88AB\u4FDD\u7559\u4E0B\u6765\u4E86\u3002\u76F8\u5E94\u5730\uFF0C\u5730\u78C1\u5357\u6781\u5B9E\u9645\u4E0A\u662F\u7269\u7406\u4E0A\u7684\u78C1\u573A\u5317\u6781\u3002 \u7B80\u5355\u7684\u8BF4\uFF0C\u6240\u6709\u78C1\u94C1\u90FD\u6709\u4E24\u4E2A\u78C1\u6781\uFF0C\u88AB\u79F0\u4E3A\u78C1\u94C1\u7684\u201C\u5317\u201D\u548C\u201C\u5357\u201D\u6781\u3002\u56E0\u4E3A\u5B83\u4EEC\u5728\u53D1\u660E\u6307\u5357\u9488\u4E2D\u4F7F\u7528\u65F6\uFF0C\u6307\u5411\u5317\u6781\u7684\u65B9\u5411\u88AB\u5B9A\u4E49\u4E3A\u5317\u6781\u3002\u4F46\u56E0\u4E3A\u5F02\u6781\u76F8\u5438\uFF0C\u8FD9\u610F\u5473\u7740\u5982\u679C\u4F5C\u4E3A\u7269\u7406\u78C1\u94C1\uFF0C\u5730\u7403\u7684\u78C1\u5317\u6781\u5B9E\u9645\u4E0A\u5728\u5357\u6781\u3002"@zh . . "\uC790\uBD81\uADF9"@ko . . "Severn\u00ED geomagnetick\u00FD p\u00F3lje m\u00EDsto, kde osa magnetick\u00E9ho dip\u00F3lu nejl\u00E9pe aproximuj\u00EDc\u00EDho zemsk\u00E9 magnetick\u00E9 pole prot\u00EDn\u00E1 na severu povrch Zem\u011B. Le\u017E\u00ED v severoz\u00E1padn\u00EDm Gr\u00F3nsku na 79\u00B0 severn\u00ED \u0161\u00ED\u0159ky a 290\u00B0 v\u00FDchodn\u00ED d\u00E9lky, \u010Dili asi 1 250 km od geografick\u00E9ho severn\u00EDho p\u00F3lu. Osa tohoto dip\u00F3lu sv\u00EDr\u00E1 \u00FAhel 11\u00B0 s zemskou osou, dip\u00F3l m\u00E1 magnetick\u00FD moment 8,0.1022 J T\u22121. S \u010Dasem se poloha t\u00E9to osy m\u011Bn\u00ED. Magnetick\u00FD p\u00F3l na severn\u00ED polokouli je fyzik\u00E1ln\u011B ji\u017En\u00ED p\u00F3l. Magnetick\u00FD sever a jih byly toti\u017E definov\u00E1ny podle orientace st\u0159elky kompasu. Severn\u00ED p\u00F3l st\u0159elky je tedy p\u0159itahov\u00E1n ji\u017En\u00EDm magnetick\u00FDm p\u00F3lem Zem\u011B."@cs . . . . . . . . . . . . . . "\u039C\u03B1\u03B3\u03BD\u03B7\u03C4\u03B9\u03BA\u03CC\u03C2 \u0392\u03CC\u03C1\u03B5\u03B9\u03BF\u03C2 \u03A0\u03CC\u03BB\u03BF\u03C2"@el . "Magnetiska nordpolen"@sv . . . . "Le p\u00F4le Nord magn\u00E9tique de la Terre est un point errant unique sur la surface o\u00F9 le champ magn\u00E9tique terrestre pointe vers le bas. C'est-\u00E0-dire que le \u00AB Dip \u00BB (plongeon) est de 90\u00B0. L'aiguille d'une boussole pointe approximativement vers ce lieu (plus ou moins approximativement suivant le lieu o\u00F9 on se trouve ; exactement la boussole est tangente \u00E0 la ligne de champ). Il s'agit en fait du p\u00F4le sud de l'aimant constitu\u00E9 par la Terre. Induit par les d\u00E9placements du noyau ferreux de la Terre, ce p\u00F4le est en d\u00E9placement avec une vitesse acc\u00E9l\u00E9r\u00E9e (auparavant 10 km par an, mais depuis 2001, 55 km environ par an) : il a franchi en 2005 la c\u00F4te canadienne pour prendre ensuite la direction de la Russie. Il est estim\u00E9 que dans les ann\u00E9es 2030, il aura boug\u00E9 d'entre 390 et 660 km. Certains sp\u00E9cialistes consid\u00E8rent qu'il s'agit du d\u00E9but du ph\u00E9nom\u00E8ne d'inversion des p\u00F4les Nord et Sud, ayant lieu en moyenne tous les 250 000 ans, le dernier datant d'environ 780 000 ans Ne pas confondre le p\u00F4le nord magn\u00E9tique, qui est un point, avec le nord magn\u00E9tique qui est la direction du nord donn\u00E9e par une boussole."@fr . "Magnetiska nordpolen (egentligen nordpolens magnetiska pol, som \u00E4r en sydpol) \u00E4r den punkt p\u00E5 jordytan p\u00E5 norra halvklotet d\u00E4r inklinationen \u00E4r 90\u00B0, s\u00E5 att den horisontella komposanten i jordens magnetf\u00E4lt \u00E4r noll och en perfekt kompassn\u00E5l d\u00E4rmed vill peka rakt ned\u00E5t. Denna magnetiska pol ligger inte vid den geografiska nordpolen, utan ungef\u00E4r 190 mil s\u00F6der om den geografiska nordpolen."@sv . . . . . "A TV show is not a reliable source, especially not about their own accomplishments."@en . . . . . "\u0421\u0435\u0432\u0435\u0440\u043D\u044B\u0439 \u043C\u0430\u0433\u043D\u0438\u0442\u043D\u044B\u0439 \u043F\u043E\u043B\u044E\u0441"@ru . . . "February 2014"@en . . . "\u0421\u0435\u0301\u0432\u0435\u0440\u043D\u044B\u0439 \u043C\u0430\u0433\u043D\u0438\u0301\u0442\u043D\u044B\u0439 \u043F\u043E\u0301\u043B\u044E\u0441 \u2014 \u0443\u0441\u043B\u043E\u0432\u043D\u0430\u044F \u0442\u043E\u0447\u043A\u0430 \u0432 \u0441\u0435\u0432\u0435\u0440\u043D\u043E\u0439 \u043F\u043E\u043B\u044F\u0440\u043D\u043E\u0439 \u043E\u0431\u043B\u0430\u0441\u0442\u0438 \u0437\u0435\u043C\u043D\u043E\u0439 \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u043E\u0441\u0442\u0438, \u0432 \u043A\u043E\u0442\u043E\u0440\u043E\u0439 \u043C\u0430\u0433\u043D\u0438\u0442\u043D\u043E\u0435 \u043F\u043E\u043B\u0435 \u0417\u0435\u043C\u043B\u0438 \u043D\u0430\u043F\u0440\u0430\u0432\u043B\u0435\u043D\u043E \u0441\u0442\u0440\u043E\u0433\u043E \u0432\u043D\u0438\u0437 (\u043F\u043E\u0434 \u0443\u0433\u043B\u043E\u043C 90\u00B0 \u043A \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u043E\u0441\u0442\u0438)."@ru . "\u0627\u0644\u0642\u0637\u0628 \u0627\u0644\u0634\u0645\u0627\u0644\u064A \u0627\u0644\u0645\u063A\u0646\u0627\u0637\u064A\u0633\u064A \u0647\u0648 \u0646\u0642\u0637\u0629 \u0639\u0644\u0649 \u0633\u0637\u062D \u0627\u0644\u0623\u0631\u0636 \u062A\u0642\u0639 \u0641\u064A \u0646\u0635\u0641 \u0627\u0644\u0623\u0631\u0636 \u0627\u0644\u0634\u0645\u0627\u0644\u064A \u0648\u064A\u0643\u0648\u0646 \u0639\u0646\u062F\u0647\u0627 \u0627\u062A\u062C\u0627\u0647 \u0627\u0644\u062D\u0642\u0644 \u0627\u0644\u0645\u063A\u0646\u0627\u0637\u064A\u0633\u064A \u0627\u0644\u0623\u0631\u0636\u064A \u0639\u0645\u0648\u062F\u064A\u0627\u064B \u0628\u0627\u062A\u062C\u0627\u0647 \u0627\u0644\u0623\u0633\u0641\u0644\u060C \u0623\u064A \u0623\u0646\u0647 \u0625\u0630\u0627 \u0633\u0645\u062D \u0644\u0628\u0648\u0635\u0644\u0629 \u0623\u0646 \u062A\u062F\u0648\u0631 \u0628\u0634\u0643\u0644 \u062D\u0631 \u0641\u0625\u0646\u0647\u0627 \u0633\u062A\u062A\u062C\u0647 \u0646\u062D\u0648 \u0627\u0644\u0623\u0633\u0641\u0644. \u062A\u0642\u0639 \u0647\u0630\u0647 \u0627\u0644\u0645\u0646\u0637\u0642\u0629 \u0628\u0627\u0644\u0642\u0631\u0628 \u0645\u0646 \u0627\u0644\u0642\u0637\u0628 \u0627\u0644\u0634\u0645\u0627\u0644\u064A \u0627\u0644\u062C\u063A\u0631\u0627\u0641\u064A\u060C \u0648\u0647\u064A \u063A\u064A\u0631 \u062B\u0627\u0628\u062A\u0629 \u0641\u064A \u0645\u0643\u0627\u0646\u0647\u0627 \u0648\u062A\u062A\u062D\u0631\u0643 \u0645\u0639 \u0645\u0631\u0648\u0631 \u0627\u0644\u0648\u0642\u062A \u0628\u0633\u0628\u0628 \u062D\u062F\u0648\u062B \u062A\u063A\u064A\u0631\u0627\u062A \u0645\u063A\u0646\u0627\u0637\u064A\u0633\u064A\u0629 \u0641\u064A \u0627\u0644\u0644\u0628 \u0627\u0644\u062E\u0627\u0631\u062C\u064A \u0644\u0644\u0623\u0631\u0636."@ar . . . . "El Pol Nord magn\u00E8tic terrestre actualment est\u00E0 situat a uns 1.600 km del Pol Nord geogr\u00E0fic, prop de l'illa de Bathurst, a la part septentrional del Canad\u00E0, en el territori de Nunavut. Encara que magn\u00E8ticament parlant no \u00E9s exactament un Pol Nord sin\u00F3 un pol Sud usualment \u00E9s anomenat aix\u00ED per a no confondre's en parlar de temes relacionats amb la navegaci\u00F3, ja que es fa servir per ressaltar que es parla del Nord que marca la br\u00FAixola i no el \"real\" que normalment porten els mapes. Aquest lloc canvia cont\u00EDnuament al llarg del temps a una velocitat variable (actualment estimada en 40 km / any), i en altres ocasions ha estat situat en l'hemisferi sud a causa de les inversions peri\u00F2diques del camp magn\u00E8tic terrestre (la darrera, la inversi\u00F3 de Brunhes-Matuyama, va ser fa 780.000 anys). Una br\u00FAixola situada horitzontalment en aquest pol apuntaria a qualsevol direcci\u00F3 i si s'est\u00E0 prou a prop, tindria un error considerable, ja que en la majoria de les br\u00FAixoles l'agulla tendiria a apuntar cap avall. Les br\u00FAixoles no apunten al pol Nord geogr\u00E0fic sin\u00F3 al pol Nord magn\u00E8tic, definit com el lloc on el camp magn\u00E8tic \u00E9s perpendicular a la superf\u00EDcie, fet pel qual que en latituds altes s\u00F3n bastant imprecises."@ca . . "\u041F\u0456\u0432\u043D\u0456\u0447\u043D\u0438\u0439 \u043C\u0430\u0433\u043D\u0456\u0442\u043D\u0438\u0439 \u043F\u043E\u043B\u044E\u0441 \u2014 \u0443\u043C\u043E\u0432\u043D\u0430 \u0442\u043E\u0447\u043A\u0430 \u043D\u0430 \u0437\u0435\u043C\u043D\u0456\u0439 \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u0456, \u0432 \u044F\u043A\u0456\u0439 \u043C\u0430\u0433\u043D\u0456\u0442\u043D\u0435 \u043F\u043E\u043B\u0435 \u0417\u0435\u043C\u043B\u0456 \u0441\u043F\u0440\u044F\u043C\u043E\u0432\u0430\u043D\u043E \u043F\u0440\u044F\u043C\u043E\u0432\u0438\u0441\u043D\u043E (\u043F\u0456\u0434 \u043A\u0443\u0442\u043E\u043C 90 \u00B0 \u0434\u043E \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u0456). \u0421\u043B\u0456\u0434 \u0437\u0430\u0437\u043D\u0430\u0447\u0438\u0442\u0438, \u0449\u043E \u0437 \u0444\u0456\u0437\u0438\u0447\u043D\u043E\u0433\u043E \u043F\u043E\u0433\u043B\u044F\u0434\u0443 \u0446\u0435\u0439 \u043F\u043E\u043B\u044E\u0441 \u0454 \u00AB\u043F\u0456\u0432\u0434\u0435\u043D\u043D\u0438\u043C\u00BB, \u043E\u0441\u043A\u0456\u043B\u044C\u043A\u0438 \u043F\u0440\u0438\u0442\u044F\u0433\u0443\u0454 \u043F\u0456\u0432\u043D\u0456\u0447\u043D\u0438\u0439 \u043F\u043E\u043B\u044E\u0441 \u0441\u0442\u0440\u0456\u043B\u043A\u0438 \u043A\u043E\u043C\u043F\u0430\u0441\u0430."@uk . . . . . . . . . . . . . "El Pol Nord magn\u00E8tic terrestre actualment est\u00E0 situat a uns 1.600 km del Pol Nord geogr\u00E0fic, prop de l'illa de Bathurst, a la part septentrional del Canad\u00E0, en el territori de Nunavut. Encara que magn\u00E8ticament parlant no \u00E9s exactament un Pol Nord sin\u00F3 un pol Sud usualment \u00E9s anomenat aix\u00ED per a no confondre's en parlar de temes relacionats amb la navegaci\u00F3, ja que es fa servir per ressaltar que es parla del Nord que marca la br\u00FAixola i no el \"real\" que normalment porten els mapes."@ca . . . "\u5730\u78C1\u5317\u6781"@zh . "Polo norte magn\u00E9tico"@pt . . . "Arkta magnetpoluso"@eo . . . . . . . . . "P\u00F4le Nord magn\u00E9tique"@fr . . . "La arkta magneta poluso a\u016D norda magnetpoluso estas tiu punkto sur la tersurfaco de la norda hemisfero en kiu la tera magnetkampo direkti\u011Das vertikale suben. Tiu punkto varias depende de la tempo. \u011Cia kontra\u016Dparto en la suda hemisfero estas la Antarkta magneta poluso. \u0108ar la tera magnetkampo ne estas ekzakte simetria Arkta kaj Antarkta magnetpolusoj ne estas antipodaj (spegulsimetriaj tra la tercentro): linio inter amba\u016D magnetpolusoj preteriras la tercentron en distanco de 530 km. La plej okulfrapa fenomeno \u0109irka\u016D la magnetpolusoj estas la \"Polaraj lumoj\" (\"norda brilo\")."@eo . . "24238"^^ . "\uC790\uBD81\uADF9(\u78C1\u5317\u6975) \uB610\uB294 \uC790\uBD81(\u78C1\u5317)\uC740 \uC9C0\uAD6C\uC758 \uC790\uAE30\uC7A5\uC774 \uC218\uC9C1\uC758 \uC544\uB798 \uBC29\uD5A5\uC73C\uB85C \uAC00\uB9AC\uD0A4\uB294 \uC9C0\uAD6C \uD45C\uBA74\uC758 \uC9C0\uC810\uC73C\uB85C, \uC2DC\uAC04\uC774 \uC9C0\uB0A8\uC5D0 \uB530\uB77C \uC810\uC810 \uC774\uB3D9\uD55C\uB2E4. \uC790\uBD81\uC740 \uD754\uD788 '\uC9C0\uC790\uAE30 \uBD81\uADF9(Geomagnetic pole)'\uACFC \uD63C\uB3D9\uB418\uAE30\uB3C4 \uD55C\uB2E4. 2005\uB144\uC758 \uC790\uBD81\uC740 \uCE90\uB098\uB2E4 \uBD81\uBD80\uC758 \uC5D8\uC988\uBBF8\uC5B4\uC12C \uBD80\uADFC(\uBD81\uC704 82.7\u00B0, \uC11C\uACBD 114.4\u00B0)\uC5D0 \uB193\uC5EC \uC788\uC5C8\uB2E4. \uC9C0\uAD6C \uC790\uAE30\uB294 \uC644\uBCBD\uD55C \uB300\uCE6D\uC774 \uC544\uB2C8\uBBC0\uB85C, \uC790\uBD81\uACFC \uADF8 \uBC18\uB300 \uC9C0\uC810\uC778 \uC790\uB0A8\uC740 \uC9C0\uB9AC\uC0C1 \uC815\uBC18\uB300\uC5D0 \uC788\uC9C0 \uC54A\uB2E4. \uC790\uBD81\uC5D0\uC11C \uC790\uB0A8\uC744 \uC9C0\uB098\uB294 \uC120\uC740 \uC9C0\uAD6C\uC758 \uC911\uC2EC\uC744 \uC9C0\uB098\uC9C0 \uC54A\uC73C\uBA70, \uC2E4\uC81C\uB85C\uB294 \uC57D 530km \uB5A8\uC5B4\uC9C4 \uACF3\uC744 \uC9C0\uB098\uAC04\uB2E4."@ko . "The north magnetic pole is a point on the surface of Earth's Northern Hemisphere at which the planet's magnetic field points vertically downward (in other words, if a magnetic compass needle is allowed to rotate in three dimensions, it will point straight down). There is only one location where this occurs, near (but distinct from) the geographic north pole. The geomagnetic north pole is the northern antipodal pole of an ideal dipole model of the Earth's magnetic field, which is the most closely fitting model of Earth's actual magnetic field."@en . "\u039F \u03BC\u03B1\u03B3\u03BD\u03B7\u03C4\u03B9\u03BA\u03CC\u03C2 \u03B2\u03CC\u03C1\u03B5\u03B9\u03BF\u03C2 \u03C0\u03CC\u03BB\u03BF\u03C2 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03C4\u03BF \u03C3\u03B7\u03BC\u03B5\u03AF\u03BF \u03C0\u03BF\u03C5 \u03B4\u03B5\u03AF\u03C7\u03BD\u03BF\u03C5\u03BD \u03CC\u03BB\u03B5\u03C2 \u03BF\u03B9 \u03BC\u03B1\u03B3\u03BD\u03B7\u03C4\u03B9\u03BA\u03AD\u03C2 \u03B2\u03B5\u03BB\u03CC\u03BD\u03B5\u03C2 \u03C4\u03C9\u03BD \u03C0\u03C5\u03BE\u03AF\u03B4\u03C9\u03BD, \u03C0\u03BF\u03C5 \u03CC\u03BC\u03C9\u03C2 \u03B4\u03B5\u03BD \u03C4\u03B1\u03C5\u03C4\u03AF\u03B6\u03B5\u03C4\u03B1\u03B9 \u03BC\u03B5 \u03C4\u03BF\u03BD \u03B3\u03B5\u03C9\u03B3\u03C1\u03B1\u03C6\u03B9\u03BA\u03CC \u03B2\u03CC\u03C1\u03B5\u03B9\u03BF \u03C0\u03CC\u03BB\u03BF (\u03B4\u03B5\u03AF\u03C4\u03B5 \u03C3\u03C7\u03B5\u03C4\u03B9\u03BA\u03AC \u03BC\u03B1\u03B3\u03BD\u03B7\u03C4\u03B9\u03BA\u03CC\u03C2 \u03B2\u03BF\u03C1\u03C1\u03AC\u03C2). \u038C\u03C0\u03C9\u03C2 \u03BF\u03B9 \u03BC\u03B1\u03B3\u03BD\u03B7\u03C4\u03B9\u03BA\u03BF\u03AF \u03C0\u03CC\u03BB\u03BF\u03B9 \u03CC\u03BB\u03C9\u03BD \u03C4\u03C9\u03BD \u03C0\u03BB\u03B1\u03BD\u03B7\u03C4\u03CE\u03BD, \u03AD\u03C4\u03C3\u03B9 \u03BA\u03B1\u03B9 \u03C4\u03B7\u03C2 \u0393\u03B7\u03C2 \u03BC\u03B5\u03C4\u03B1\u03C4\u03BF\u03C0\u03AF\u03B6\u03B5\u03C4\u03B1\u03B9 \u03B5\u03BB\u03B1\u03C6\u03C1\u03AC, \u03B1\u03BB\u03BB\u03AC\u03B6\u03BF\u03BD\u03C4\u03B1\u03C2 \u03C3\u03C5\u03BD\u03B5\u03C7\u03CE\u03C2 \u03B8\u03AD\u03C3\u03B7 \u03B3\u03CD\u03C1\u03C9 \u03B1\u03C0\u03CC \u03C4\u03BF\u03BD \u03B3\u03B5\u03C9\u03B3\u03C1\u03B1\u03C6\u03B9\u03BA\u03CC \u03C0\u03CC\u03BB\u03BF. \u0391\u03C5\u03C4\u03CC \u03C3\u03C5\u03BC\u03B2\u03B1\u03AF\u03BD\u03B5\u03B9 \u03BB\u03CC\u03B3\u03C9 \u03C4\u03C9\u03BD \u03BA\u03B9\u03BD\u03AE\u03C3\u03B5\u03C9\u03BD \u03C3\u03C4\u03BF \u03B5\u03C3\u03C9\u03C4\u03B5\u03C1\u03B9\u03BA\u03CC \u03C4\u03B7\u03C2 \u03C4\u03BF \u03C1\u03B5\u03C5\u03C3\u03C4\u03BF\u03CD \u03C5\u03BB\u03B9\u03BA\u03BF\u03CD \u03C0\u03BF\u03C5 \u03B5\u03AF\u03BD\u03B1\u03B9 \u03BA\u03C5\u03C1\u03AF\u03C9\u03C2 \u03C5\u03C0\u03B5\u03CD\u03B8\u03C5\u03BD\u03BF \u03B3\u03B9\u03B1 \u03C4\u03B7 \u03B4\u03B7\u03BC\u03B9\u03BF\u03C5\u03C1\u03B3\u03AF\u03B1 \u03BA\u03B1\u03B9 \u03C3\u03C5\u03BD\u03C4\u03AE\u03C1\u03B7\u03C3\u03B7 \u03C4\u03BF\u03C5 \u03BC\u03B1\u03B3\u03BD\u03B7\u03C4\u03B9\u03BA\u03BF\u03CD \u03C0\u03B5\u03B4\u03AF\u03BF\u03C5. \u03A3\u03CD\u03BC\u03C6\u03C9\u03BD\u03B1 \u03BC\u03B5 \u03BC\u03B5\u03C4\u03C1\u03AE\u03C3\u03B5\u03B9\u03C2 \u03C4\u03B7\u03C2 \u039A\u03B1\u03BD\u03B1\u03B4\u03B9\u03BA\u03AE\u03C2 \u039A\u03C5\u03B2\u03AD\u03C1\u03BD\u03B7\u03C3\u03B7\u03C2, \u03BF \u03BC\u03B1\u03B3\u03BD\u03B7\u03C4\u03B9\u03BA\u03CC\u03C2 \u03B2\u03CC\u03C1\u03B5\u03B9\u03BF\u03C2 \u03C0\u03CC\u03BB\u03BF\u03C2 \u03C3\u03C5\u03BD\u03B5\u03C7\u03AF\u03B6\u03B5\u03B9 \u03BD\u03B1 \u03BC\u03B5\u03C4\u03B1\u03BA\u03B9\u03BD\u03B5\u03AF\u03C4\u03B1\u03B9 \u03B2\u03CC\u03C1\u03B5\u03B9\u03B1. \u03A4\u03BF 1996 \u03C4\u03BF \u03C3\u03B7\u03BC\u03B5\u03AF\u03BF \u03C4\u03BF\u03C5 \u03B2\u03C1\u03AD\u03B8\u03B7\u03BA\u03B5 \u03C3\u03C4\u03BF \u03B3\u03B5\u03C9\u03B3\u03C1\u03B1\u03C6\u03B9\u03BA\u03CC \u03C3\u03C4\u03AF\u03B3\u03BC\u03B1 78\u00B035.7\u2032 N, 104\u00B011.9\u2032 W. \u03A4\u03BF 2005 \u03B2\u03C1\u03AD\u03B8\u03B7\u03BA\u03B5 \u03C3\u03C4\u03BF 82\u00B007\u2032 N, 114\u00B004\u2032 W. \u039A\u03B1\u03C4\u03AC \u03C4\u03B7 \u03B4\u03B9\u03AC\u03C1\u03BA\u03B5\u03B9\u03B1 \u03C4\u03BF\u03C5 20\u03BF\u03C5 \u03B1\u03B9\u03CE\u03BD\u03B1 \u03BC\u03B5\u03C4\u03B1\u03BA\u03B9\u03BD\u03AE\u03B8\u03B7\u03BA\u03B5 1100 \u03C7\u03B9\u03BB\u03B9\u03CC\u03BC\u03B5\u03C4\u03C1\u03B1, \u03BA\u03B1\u03B9 \u03BC\u03B5\u03C4\u03AC \u03C4\u03BF 1970 \u03B7 \u03BC\u03B5\u03C4\u03B1\u03BA\u03AF\u03BD\u03B7\u03C3\u03AE \u03C4\u03BF\u03C5 \u03B5\u03C0\u03B9\u03C4\u03B1\u03C7"@el . "Iparburu magnetikoa"@eu . . "December 2019"@en . "Does 'foci' mean foci of the aforementioned ellipse? Why are the foci important?"@en . . . . "The north magnetic pole is a point on the surface of Earth's Northern Hemisphere at which the planet's magnetic field points vertically downward (in other words, if a magnetic compass needle is allowed to rotate in three dimensions, it will point straight down). There is only one location where this occurs, near (but distinct from) the geographic north pole. The geomagnetic north pole is the northern antipodal pole of an ideal dipole model of the Earth's magnetic field, which is the most closely fitting model of Earth's actual magnetic field. The north magnetic pole moves over time according to magnetic changes and flux lobe elongation in the Earth's outer core. In 2001, it was determined by the Geological Survey of Canada to lie west of Ellesmere Island in northern Canada at 81\u00B018\u2032N 110\u00B048\u2032W\uFEFF / \uFEFF81.300\u00B0N 110.800\u00B0W. It was situated at 83\u00B006\u2032N 117\u00B048\u2032W\uFEFF / \uFEFF83.100\u00B0N 117.800\u00B0W in 2005. In 2009, while still situated within the Canadian Arctic at 84\u00B054\u2032N 131\u00B000\u2032W\uFEFF / \uFEFF84.900\u00B0N 131.000\u00B0W, it was moving toward Russia at between 55 and 60 km (34 and 37 mi) per year. As of 2021, the pole is projected to have moved beyond the Canadian Arctic to 86\u00B024\u203200\u2033N 156\u00B047\u203210\u2033E\uFEFF / \uFEFF86.400\u00B0N 156.786\u00B0E. Its southern hemisphere counterpart is the south magnetic pole. Since Earth's magnetic field is not exactly symmetric, the north and south magnetic poles are not antipodal, meaning that a straight line drawn from one to the other does not pass through the geometric center of Earth. Earth's north and south magnetic poles are also known as magnetic dip poles, with reference to the vertical \"dip\" of the magnetic field lines at those points."@en . . "El polo norte magn\u00E9tico es la direcci\u00F3n que se\u00F1ala la aguja imantada de una br\u00FAjula, direcci\u00F3n que no coincide con la del polo norte geogr\u00E1fico, excepto en los puntos del hemisferio norte, situados en el mismo meridiano que el norte magn\u00E9tico. Actualmente est\u00E1 situado a unos 1600 km del polo norte geogr\u00E1fico, cerca de la isla de Bathurst, en la parte septentrional de Canad\u00E1, en el territorio de Nunavut. La Tierra genera un campo magn\u00E9tico que se llama campo geomagn\u00E9tico o campo magn\u00E9tico terrestre. El estudio de este campo geomagn\u00E9tico se remonta al siglo XVI, cuando el ingl\u00E9s William Gilbert public\u00F3 el libro De Magnete, en 1600.Las br\u00FAjulas no apuntan al polo norte geogr\u00E1fico sino al polo norte magn\u00E9tico, definido como el lugar donde el campo magn\u00E9tico es perpendicular a la superficie, por lo que en latitudes altas son bastante imprecisas.El norte magn\u00E9tico se desplaza paulatinamente, por lo que su posici\u00F3n marcada para un a\u00F1o es solo un promedio. Actualmente se desplaza unos cien metros diarios (40 km/a\u00F1o), el campo magn\u00E9tico crece y decrece en intensidad a lo largo de los a\u00F1os y, peri\u00F3dicamente, se invierte la polaridad, en ciclos de miles de a\u00F1os. La fase actual es decreciente.Magn\u00E9ticamente hablando no es exactamente un polo norte sino un polo sur, usualmente es llamado as\u00ED para no confundirse al hablar de temas relacionados con la navegaci\u00F3n, ya que se usa para resaltar que se habla del norte que marca la br\u00FAjula y no el \"real\" que normalmente llevan los mapas. Este lugar cambia continuamente a lo largo del tiempo a una velocidad variable (actualmente estimada en 40 km/a\u00F1o), y en otras ocasiones ha estado situado en el hemisferio sur debido a las inversiones peri\u00F3dicas del campo magn\u00E9tico terrestre (la \u00FAltima fue hace 780 000 a\u00F1os). Una br\u00FAjula situada horizontalmente en este polo apuntar\u00EDa a cualquier direcci\u00F3n y si se est\u00E1 lo suficientemente cerca tendr\u00EDa un error considerable ya que en la mayor\u00EDa de las br\u00FAjulas la aguja tender\u00EDa a apuntar hacia abajo."@es . .