. "Proiezione azimutale equivalente di Lambert"@it . . . "La proiezione azimutale equivalente di Lambert \u00E8 una proiezione cartografica mediante la quale una qualunque sfera viene rappresentata su di un disco. Essa conserva le aree in ogni parte della sfera, mentre non riproduce fedelmente gli angoli. Prende il nome dal matematico svizzero Johann Heinrich Lambert, che la formul\u00F2 nel 1772. La proiezione azimutale di Lambert \u00E8 utilizzata in cartografia. Per esempio l'Agenzia europea dell'ambiente ne raccomanda l'uso per le analisi statistiche."@it . . . . . . . "La proiezione azimutale equivalente di Lambert \u00E8 una proiezione cartografica mediante la quale una qualunque sfera viene rappresentata su di un disco. Essa conserva le aree in ogni parte della sfera, mentre non riproduce fedelmente gli angoli. Prende il nome dal matematico svizzero Johann Heinrich Lambert, che la formul\u00F2 nel 1772. La proiezione azimutale di Lambert \u00E8 utilizzata in cartografia. Per esempio l'Agenzia europea dell'ambiente ne raccomanda l'uso per le analisi statistiche."@it . "De oppervlaktegetrouwe azimutale projectie of azimutale projectie van Lambert is een van de projecties die is bedacht door Johann H. Lambert. Deze projectie is een speciaal geval van de (later ontwikkelde) projectie van Albers, waarbij beide standaardparallellen een punt op Aarde (vaak een van de beide polen) representeren, en de buitencirkel het tegenoverliggende punt."@nl . . . . "Die fl\u00E4chentreue Azimutalprojektion (auch Lambertsche Azimutalprojektion genannt, nach Johann Heinrich Lambert) ist ein Kartennetzentwurf, in dem die gesamte (Erd-)Kugeloberfl\u00E4che wiedergegeben werden kann. Lambert verk\u00FCndete sie 1772. Die Kartenabbildung ist weder l\u00E4ngen- noch winkeltreu. Das Kartenzentrum wird verzerrungsfrei dargestellt, jedoch nimmt die Verzerrung zum Rand hin so stark zu, dass diese Bereiche sehr unanschaulich werden. Deshalb wird meist nur maximal eine Halbkugeloberfl\u00E4che mit dieser Abbildung wiedergegeben. Diese ist in den unten dargestellten Grafiken jeweils durch eine rote Kreislinie markiert. Meridiane und Breitenkreise werden \u2013 besonders bei der schiefen Projektion erkennbar \u2013 zu komplexen Kurven verzerrt. Daher l\u00E4sst sich diese Kartenabbildung nicht mit Zirkel und Lineal konstruieren. \n* Transversale azimutale Lambert-Projektion \n* Polare azimutale Lambert-Projektion \n* Schiefe azimutale Lambert-Projektion (Wasserhalbkugel)"@de . . . . "3663384"^^ . . . . . . . "Proyecci\u00F3n acimutal de Lambert"@es . . "A proje\u00E7\u00E3o azimutal de Lambert \u00E9 uma forma de mapear uma esfera para um disco. Ela representa a \u00E1rea de forma precisa em todas as regi\u00F5es da esfera, mas n\u00E3o \u00E2ngulos. Recebe o nome do matem\u00E1tico Johann Heinrich Lambert que a prop\u00F4s em 1772."@pt . "La projecci\u00F3 azimutal equivalent o projecci\u00F3 azimutal homologr\u00E0fica de Lambert\u00E9s una projecci\u00F3 cartogr\u00E0fica azimutalequivalent (mant\u00E9 les proporcions de les \u00E0rees) per\u00F2 no \u00E9s conforme (distorsiona les formes i els angles). Aquesta projecci\u00F3 \u00E9s un artefacte matem\u00E0tic, no una representaci\u00F3 d'una construcci\u00F3 geom\u00E8trica.Amb aquesta projecci\u00F3, un mapa del m\u00F3n sencer \u00E9s un cercle amb el centre de projecci\u00F3 al centre del mapa. La distorsi\u00F3 de formes i angles creix com m\u00E9s lluny del centre del mapa. Si el centre del mapa \u00E9s un dels pols, els meridians apareixen representats rectes i els paral\u00B7lels com cercles conc\u00E8ntrics amb dist\u00E0ncies decreixents. Si el centre del mapa \u00E9s qualsevol altre punt, els meridians i els paral\u00B7lels apareixen representats com corbes complexes. Les rectes que pasen pel centre del mapa s\u00F3n cercles m\u00E0xims de l'esfera. Com a cas particular, si el centre del mapa \u00E9s un punt de l'Equador, l'Equador, i el meridi\u00E0 del centre del mapa apareixen representats com a rectes, i la resta de meridians i de paral\u00B7lels apareixen representats com corbes complexes. Suposant una escala escala i un centre de projecci\u00F3 amb longitud long0 i latitud lat0, aquestes s\u00F3n les equacions generals per a obtenir les coordenades cartesianes x, y en el pla per al lloc amb longitud long i latitud lat: k = sqrt( 2 / (1 + sin(lat0) * sin(lat) + cos(lat0) * cos(lat) * cos(long - long0) ) )x = escala * k * cos(lat) * sin(long - long0)y = escala * k * ( cos(lat0) * sin(lat) - sin(lat0) * cos(lat) * cos(long - long0) )"@ca . "\uB78C\uBCA0\uB974\uD2B8 \uC815\uC801\uBC29\uC704\uB3C4\uBC95"@ko . . . . . . . . . "\u30E9\u30F3\u30D9\u30EB\u30C8\u6B63\u7A4D\u65B9\u4F4D\u56F3\u6CD5\uFF08\u30E9\u30F3\u30D9\u30EB\u30C8\u305B\u3044\u305B\u304D\u307B\u3046\u3044\u305A\u307B\u3046\uFF09\u3068\u306F\u3001\u5730\u56F3\u6295\u5F71\u6CD5\u306E\u4E00\u7A2E\u3067\u3042\u308A\u3001\u65B9\u4F4D\u56F3\u6CD5\uFF08\u5730\u56F3\u306E\u4E2D\u5FC3\u304B\u3089\u306E\u65B9\u4F4D\u304C\u6B63\u3057\u304F\u793A\u3055\u308C\u308B\uFF09\u304A\u3088\u3073\uFF08\u9762\u7A4D\u304C\u6B63\u3057\u304F\u793A\u3055\u308C\u308B\uFF09\u306E\u4E21\u65B9\u306E\u6027\u8CEA\u3092\u6301\u3064\u3002 \u5317\u6975\u70B9\u3082\u3057\u304F\u306F\u5357\u6975\u70B9\u3092\u57FA\u6E96\u70B9\uFF08\u4E2D\u5FC3\uFF09\u3068\u3057\u305F\u5834\u5408\u3001\u7D4C\u7DDA\u306F\u4E2D\u5FC3\u304B\u3089\u653E\u5C04\u72B6\u306B\u3001\u7DEF\u7DDA\u306F\u57FA\u6E96\u70B9\u3092\u4E2D\u5FC3\u3068\u3059\u308B\u540C\u5FC3\u5186\u306B\u63CF\u304B\u308C\u308B\u3002\u9762\u7A4D\u304C\u6B63\u3057\u304F\u8868\u3055\u308C\u308B\u3088\u3046\u3001\u7DEF\u7DDA\u306E\u9593\u9694\u306F\u7279\u306B\u56F3\u306E\u5916\u5074\uFF08\u57FA\u6E96\u70B9\u306B\u5BFE\u3057\u3066\u8D64\u9053\u3088\u308A\u9060\u3044\u5074\u306E\u534A\u7403\uFF09\u3067\u72ED\u304F\u306A\u3063\u3066\u3044\u308B\u3002\u4E2D\u5FC3\u4ED8\u8FD1\u306E\u6B6A\u307F\u306F\u6BD4\u8F03\u7684\u5C0F\u3055\u3044\u306E\u3067\u3001\u5927\u9678\u56F3\u3084\u5206\u5E03\u56F3\u306B\u7528\u3044\u3089\u308C\u308B\u3002 \u7DEF\u5EA6\u304C l\u00B0 \u3067\u3042\u308B\u7DEF\u570F\u3092\u6295\u5C04\u56F3\u4E0A\u306B\u63CF\u304F\u305F\u3081\u306E\u534A\u5F84 r \u306F\u3001r = 2 R sin((90\uFF0Dl)/2) \uFF08R\u306F\u5730\u7403\u306E\u534A\u5F84\uFF09\u3067\u4E0E\u3048\u3089\u308C\u308B\u3002 \u540C\u69D8\u306B\u4E16\u754C\u5168\u4F53\u304C\u5186\u5F62\u306B\u63CF\u304B\u308C\u308B\u56F3\u6CD5\u306B\u306F\u3001\u6B63\u8DDD\u65B9\u4F4D\u56F3\u6CD5\u306A\u3069\u304C\u3042\u308B\u3002"@ja . . "De oppervlaktegetrouwe azimutale projectie of azimutale projectie van Lambert is een van de projecties die is bedacht door Johann H. Lambert. Deze projectie is een speciaal geval van de (later ontwikkelde) projectie van Albers, waarbij beide standaardparallellen een punt op Aarde (vaak een van de beide polen) representeren, en de buitencirkel het tegenoverliggende punt."@nl . . . . . . . "Odwzorowanie azymutalne r\u00F3wnopowierzchniowe"@pl . . . . . "14439"^^ . "La proyecci\u00F3n acimutal equivalente de Lambert (LAEA, por sus siglas en ingl\u00E9s Lambert azimuthal equal-area) conserva deliberadamente las \u00E1reas. Es una proyecci\u00F3n particular de esfera a disco. No debe ser confundida con la Proyecci\u00F3n Conforme C\u00F3nica de Lambert que es muy utilizada en navegaci\u00F3n a\u00E9rea.La proyecci\u00F3n acimutal equivalente de Lambert no es conforme, es decir, no mantiene el valor real de los \u00E1ngulos tras realizar la proyecci\u00F3n. La escala disminuye a medida que nos acercamos al borde exterior, pero en menor medida que en la proyecci\u00F3n ortogr\u00E1fica. Este sistema es muy adecuado para trazar mapas de peque\u00F1a escala."@es . . . "Fl\u00E4chentreue Azimutalprojektion"@de . . . . "Proje\u00E7\u00E3o azimutal de Lambert"@pt . "Odwzorowanie azymutalne r\u00F3wnopowierzchniowe (azymutalne Lamberta) \u2013 odwzorowanie azymutalne, w kt\u00F3rym obszary o r\u00F3wnej powierzchni na kuli ziemskiej s\u0105 przedstawiane przez obszary o r\u00F3wnej powierzchni na mapie. Wzory przekszta\u0142caj\u0105ce to: gdzie: \u2013 d\u0142ugo\u015B\u0107 geograficzna \u2013 szeroko\u015B\u0107 geograficzna \u2013 d\u0142ugo\u015B\u0107 punktu centralnego mapy \u2013 szeroko\u015B\u0107 punktu centralnego mapy \u2013 sta\u0142a skalowania mapy Wzory odwrotne:"@pl . . . . . "\uB78C\uBCA0\uB974\uD2B8 \uC815\uC801\uBC29\uC704\uB3C4\uBC95(Rambert \u6B63\u7A4D\u65B9\u4F4D\u5716\u6CD5)\uC740 1772\uB144 \uB3C5\uC77C \uC0AC\uB78C \uAC00 \uACE0\uC548\uD55C \uAC83\uC774\uB2E4. \uC55E\uC5D0 \uC124\uBA85\uD55C \uBC29\uC704\uB3C4\uBC95\uACFC \uACF5\uD1B5\uC801\uC778 \uD2B9\uC0C9\uC744 \uC9C0\uB2C8\uACE0 \uC788\uC73C\uBA70, \uBA74\uC801\uB3C4 \uBC14\uB974\uAC8C \uD45C\uC2DC\uB418\uBBC0\uB85C \uC815\uC801\uB3C4\uBC95\uC758 \uC77C\uC885\uC778 \uC148\uC774\uB2E4. \uB78C\uBCA0\uB974\uD2B8 \uC815\uC801 \uBC29\uC704\uB3C4\uBC95\uC758 \uC815\uCD95\uBC95\uC5D0\uC11C\uB294 \uACBD\uC120\uC774 \uADF9\uC5D0\uC11C \uBC29\uC0AC\uD558\uB294 \uC9C1\uC120, \uC704\uC120\uC740 \uADF9\uC744 \uC911\uC2EC\uC73C\uB85C \uD558\uB294 \uB3D9\uC2EC\uC6D0\uC744 \uC774\uB8E8\uC9C0\uB9CC \uC704\uC120\uACFC \uC704\uC120\uC758 \uAC04\uACA9\uC740 \uADF9\uC5D0\uC11C \uBA40\uC5B4\uC9C8\uC218\uB85D \uC791\uC544\uC9C4\uB2E4. \uAE38\uC774\uB294 \uACBD\uC120\uC0C1\uC5D0\uC11C\uB294 \uCD95\uC18C, \uC704\uC120\uC0C1\uC5D0\uC11C\uB294 \uD655\uB300\uB418\uC5B4 \uC788\uB2E4. \uC774 \uBB38\uC11C\uC5D0\uB294 \uB2E4\uC74C\uCEE4\uBBA4\uB2C8\uCF00\uC774\uC158(\uD604 \uCE74\uCE74\uC624)\uC5D0\uC11C GFDL \uB610\uB294 CC-SA \uB77C\uC774\uC120\uC2A4\uB85C \uBC30\uD3EC\uD55C \uAE00\uB85C\uBC8C \uC138\uACC4\uB300\uBC31\uACFC\uC0AC\uC804\uC758 \uB0B4\uC6A9\uC744 \uAE30\uCD08\uB85C \uC791\uC131\uB41C \uAE00\uC774 \uD3EC\uD568\uB418\uC5B4 \uC788\uC2B5\uB2C8\uB2E4."@ko . "La projection azimutale \u00E9quivalente de Lambert est une mani\u00E8re de projeter une sph\u00E8re sur un plan, et en particulier, une fa\u00E7on de repr\u00E9senter enti\u00E8rement la surface de la Terre sous la forme d'un disque. C'est donc une projection cartographique azimutale con\u00E7ue (parmi d'autres) en 1772 par le math\u00E9maticien alsacien Johann Heinrich Lambert."@fr . . . . . . . "1098502475"^^ . . . . "\u30E9\u30F3\u30D9\u30EB\u30C8\u6B63\u7A4D\u65B9\u4F4D\u56F3\u6CD5"@ja . "\u0420\u0430\u0432\u043D\u043E\u0432\u0435\u043B\u0438\u043A\u0430\u044F \u0430\u0437\u0438\u043C\u0443\u0442\u0430\u043B\u044C\u043D\u0430\u044F \u043F\u0440\u043E\u0435\u043A\u0446\u0438\u044F \u041B\u0430\u043C\u0431\u0435\u0440\u0442\u0430 \u2014 \u044D\u0442\u043E \u0441\u043F\u043E\u0441\u043E\u0431 \u043F\u0440\u043E\u0435\u043A\u0446\u0438\u0438 \u0441 \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u043E\u0441\u0442\u0438 \u0441\u0444\u0435\u0440\u044B \u043D\u0430 \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u043E\u0441\u0442\u044C \u043A\u0440\u0443\u0433\u0430. \u042D\u0442\u0430 \u043F\u0440\u043E\u0435\u043A\u0446\u0438\u044F \u0441\u043E\u0445\u0440\u0430\u043D\u044F\u0435\u0442 \u043F\u043B\u043E\u0449\u0430\u0434\u0438, \u043D\u043E \u043D\u0435 \u0441\u043E\u0445\u0440\u0430\u043D\u044F\u0435\u0442 \u0443\u0433\u043B\u044B. \u041F\u0440\u043E\u0435\u043A\u0446\u0438\u044F \u043D\u043E\u0441\u0438\u0442 \u0438\u043C\u044F \u0448\u0432\u0435\u0439\u0446\u0430\u0440\u0441\u043A\u043E\u0433\u043E \u043C\u0430\u0442\u0435\u043C\u0430\u0442\u0438\u043A\u0430 \u0418\u043E\u0433\u0430\u043D\u043D\u0430 \u0413\u0435\u043D\u0440\u0438\u0445\u0430 \u041B\u0430\u043C\u0431\u0435\u0440\u0442\u0430, \u043A\u043E\u0442\u043E\u0440\u044B\u0439 \u043F\u0440\u0435\u0434\u0441\u0442\u0430\u0432\u0438\u043B \u0435\u0451 \u0432 1772 \u0433\u043E\u0434\u0443. \u0420\u0430\u0432\u043D\u043E\u0432\u0435\u043B\u0438\u043A\u0430\u044F \u0430\u0437\u0438\u043C\u0443\u0442\u0430\u043B\u044C\u043D\u0430\u044F \u043F\u0440\u043E\u0435\u043A\u0446\u0438\u044F \u041B\u0430\u043C\u0431\u0435\u0440\u0442\u0430 \u0438\u0441\u043F\u043E\u043B\u044C\u0437\u0443\u0435\u0442\u0441\u044F \u0432 \u043A\u0430\u0447\u0435\u0441\u0442\u0432\u0435 \u043A\u0430\u0440\u0442\u043E\u0433\u0440\u0430\u0444\u0438\u0447\u0435\u0441\u043A\u043E\u0439 \u043F\u0440\u043E\u0435\u043A\u0446\u0438\u0438 \u0432 \u043A\u0430\u0440\u0442\u043E\u0433\u0440\u0430\u0444\u0438\u0438."@ru . . "Odwzorowanie azymutalne r\u00F3wnopowierzchniowe (azymutalne Lamberta) \u2013 odwzorowanie azymutalne, w kt\u00F3rym obszary o r\u00F3wnej powierzchni na kuli ziemskiej s\u0105 przedstawiane przez obszary o r\u00F3wnej powierzchni na mapie. Wzory przekszta\u0142caj\u0105ce to: gdzie: \u2013 d\u0142ugo\u015B\u0107 geograficzna \u2013 szeroko\u015B\u0107 geograficzna \u2013 d\u0142ugo\u015B\u0107 punktu centralnego mapy \u2013 szeroko\u015B\u0107 punktu centralnego mapy \u2013 sta\u0142a skalowania mapy Wzory odwrotne:"@pl . . "\uB78C\uBCA0\uB974\uD2B8 \uC815\uC801\uBC29\uC704\uB3C4\uBC95(Rambert \u6B63\u7A4D\u65B9\u4F4D\u5716\u6CD5)\uC740 1772\uB144 \uB3C5\uC77C \uC0AC\uB78C \uAC00 \uACE0\uC548\uD55C \uAC83\uC774\uB2E4. \uC55E\uC5D0 \uC124\uBA85\uD55C \uBC29\uC704\uB3C4\uBC95\uACFC \uACF5\uD1B5\uC801\uC778 \uD2B9\uC0C9\uC744 \uC9C0\uB2C8\uACE0 \uC788\uC73C\uBA70, \uBA74\uC801\uB3C4 \uBC14\uB974\uAC8C \uD45C\uC2DC\uB418\uBBC0\uB85C \uC815\uC801\uB3C4\uBC95\uC758 \uC77C\uC885\uC778 \uC148\uC774\uB2E4. \uB78C\uBCA0\uB974\uD2B8 \uC815\uC801 \uBC29\uC704\uB3C4\uBC95\uC758 \uC815\uCD95\uBC95\uC5D0\uC11C\uB294 \uACBD\uC120\uC774 \uADF9\uC5D0\uC11C \uBC29\uC0AC\uD558\uB294 \uC9C1\uC120, \uC704\uC120\uC740 \uADF9\uC744 \uC911\uC2EC\uC73C\uB85C \uD558\uB294 \uB3D9\uC2EC\uC6D0\uC744 \uC774\uB8E8\uC9C0\uB9CC \uC704\uC120\uACFC \uC704\uC120\uC758 \uAC04\uACA9\uC740 \uADF9\uC5D0\uC11C \uBA40\uC5B4\uC9C8\uC218\uB85D \uC791\uC544\uC9C4\uB2E4. \uAE38\uC774\uB294 \uACBD\uC120\uC0C1\uC5D0\uC11C\uB294 \uCD95\uC18C, \uC704\uC120\uC0C1\uC5D0\uC11C\uB294 \uD655\uB300\uB418\uC5B4 \uC788\uB2E4. \uC774 \uBB38\uC11C\uC5D0\uB294 \uB2E4\uC74C\uCEE4\uBBA4\uB2C8\uCF00\uC774\uC158(\uD604 \uCE74\uCE74\uC624)\uC5D0\uC11C GFDL \uB610\uB294 CC-SA \uB77C\uC774\uC120\uC2A4\uB85C \uBC30\uD3EC\uD55C \uAE00\uB85C\uBC8C \uC138\uACC4\uB300\uBC31\uACFC\uC0AC\uC804\uC758 \uB0B4\uC6A9\uC744 \uAE30\uCD08\uB85C \uC791\uC131\uB41C \uAE00\uC774 \uD3EC\uD568\uB418\uC5B4 \uC788\uC2B5\uB2C8\uB2E4."@ko . . "Projection azimutale \u00E9quivalente de Lambert"@fr . . . . . . . "Oppervlaktegetrouwe azimutale projectie"@nl . . . . . . . . . "The Lambert azimuthal equal-area projection is a particular mapping from a sphere to a disk. It accurately represents area in all regions of the sphere, but it does not accurately represent angles. It is named for the Swiss mathematician Johann Heinrich Lambert, who announced it in 1772. \"Zenithal\" being synonymous with \"azimuthal\", the projection is also known as the Lambert zenithal equal-area projection."@en . . . . "La projecci\u00F3 azimutal equivalent o projecci\u00F3 azimutal homologr\u00E0fica de Lambert\u00E9s una projecci\u00F3 cartogr\u00E0fica azimutalequivalent (mant\u00E9 les proporcions de les \u00E0rees) per\u00F2 no \u00E9s conforme (distorsiona les formes i els angles). Aquesta projecci\u00F3 \u00E9s un artefacte matem\u00E0tic, no una representaci\u00F3 d'una construcci\u00F3 geom\u00E8trica.Amb aquesta projecci\u00F3, un mapa del m\u00F3n sencer \u00E9s un cercle amb el centre de projecci\u00F3 al centre del mapa. La distorsi\u00F3 de formes i angles creix com m\u00E9s lluny del centre del mapa."@ca . 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"La projection azimutale \u00E9quivalente de Lambert est une mani\u00E8re de projeter une sph\u00E8re sur un plan, et en particulier, une fa\u00E7on de repr\u00E9senter enti\u00E8rement la surface de la Terre sous la forme d'un disque. C'est donc une projection cartographique azimutale con\u00E7ue (parmi d'autres) en 1772 par le math\u00E9maticien alsacien Johann Heinrich Lambert."@fr . "A proje\u00E7\u00E3o azimutal de Lambert \u00E9 uma forma de mapear uma esfera para um disco. Ela representa a \u00E1rea de forma precisa em todas as regi\u00F5es da esfera, mas n\u00E3o \u00E2ngulos. Recebe o nome do matem\u00E1tico Johann Heinrich Lambert que a prop\u00F4s em 1772."@pt . . . . . . . . . . "Projecci\u00F3 azimutal equivalent"@ca . . "\u0420\u0430\u0432\u043D\u043E\u0432\u0435\u043B\u0438\u043A\u0430\u044F \u0430\u0437\u0438\u043C\u0443\u0442\u0430\u043B\u044C\u043D\u0430\u044F \u043F\u0440\u043E\u0435\u043A\u0446\u0438\u044F \u041B\u0430\u043C\u0431\u0435\u0440\u0442\u0430 \u2014 \u044D\u0442\u043E \u0441\u043F\u043E\u0441\u043E\u0431 \u043F\u0440\u043E\u0435\u043A\u0446\u0438\u0438 \u0441 \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u043E\u0441\u0442\u0438 \u0441\u0444\u0435\u0440\u044B \u043D\u0430 \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u043E\u0441\u0442\u044C \u043A\u0440\u0443\u0433\u0430. \u042D\u0442\u0430 \u043F\u0440\u043E\u0435\u043A\u0446\u0438\u044F \u0441\u043E\u0445\u0440\u0430\u043D\u044F\u0435\u0442 \u043F\u043B\u043E\u0449\u0430\u0434\u0438, \u043D\u043E \u043D\u0435 \u0441\u043E\u0445\u0440\u0430\u043D\u044F\u0435\u0442 \u0443\u0433\u043B\u044B. \u041F\u0440\u043E\u0435\u043A\u0446\u0438\u044F \u043D\u043E\u0441\u0438\u0442 \u0438\u043C\u044F \u0448\u0432\u0435\u0439\u0446\u0430\u0440\u0441\u043A\u043E\u0433\u043E \u043C\u0430\u0442\u0435\u043C\u0430\u0442\u0438\u043A\u0430 \u0418\u043E\u0433\u0430\u043D\u043D\u0430 \u0413\u0435\u043D\u0440\u0438\u0445\u0430 \u041B\u0430\u043C\u0431\u0435\u0440\u0442\u0430, \u043A\u043E\u0442\u043E\u0440\u044B\u0439 \u043F\u0440\u0435\u0434\u0441\u0442\u0430\u0432\u0438\u043B \u0435\u0451 \u0432 1772 \u0433\u043E\u0434\u0443. \u0420\u0430\u0432\u043D\u043E\u0432\u0435\u043B\u0438\u043A\u0430\u044F \u0430\u0437\u0438\u043C\u0443\u0442\u0430\u043B\u044C\u043D\u0430\u044F \u043F\u0440\u043E\u0435\u043A\u0446\u0438\u044F \u041B\u0430\u043C\u0431\u0435\u0440\u0442\u0430 \u0438\u0441\u043F\u043E\u043B\u044C\u0437\u0443\u0435\u0442\u0441\u044F \u0432 \u043A\u0430\u0447\u0435\u0441\u0442\u0432\u0435 \u043A\u0430\u0440\u0442\u043E\u0433\u0440\u0430\u0444\u0438\u0447\u0435\u0441\u043A\u043E\u0439 \u043F\u0440\u043E\u0435\u043A\u0446\u0438\u0438 \u0432 \u043A\u0430\u0440\u0442\u043E\u0433\u0440\u0430\u0444\u0438\u0438."@ru . "Die fl\u00E4chentreue Azimutalprojektion (auch Lambertsche Azimutalprojektion genannt, nach Johann Heinrich Lambert) ist ein Kartennetzentwurf, in dem die gesamte (Erd-)Kugeloberfl\u00E4che wiedergegeben werden kann. Lambert verk\u00FCndete sie 1772. Meridiane und Breitenkreise werden \u2013 besonders bei der schiefen Projektion erkennbar \u2013 zu komplexen Kurven verzerrt. Daher l\u00E4sst sich diese Kartenabbildung nicht mit Zirkel und Lineal konstruieren. \n* Transversale azimutale Lambert-Projektion \n* Polare azimutale Lambert-Projektion \n* Schiefe azimutale Lambert-Projektion (Wasserhalbkugel)"@de . . . . "Lambert azimuthal equal-area projection"@en . . "The Lambert azimuthal equal-area projection is a particular mapping from a sphere to a disk. It accurately represents area in all regions of the sphere, but it does not accurately represent angles. It is named for the Swiss mathematician Johann Heinrich Lambert, who announced it in 1772. \"Zenithal\" being synonymous with \"azimuthal\", the projection is also known as the Lambert zenithal equal-area projection. The Lambert azimuthal projection is used as a map projection in cartography. For example, the National Atlas of the US uses a Lambert azimuthal equal-area projection to display information in the online Map Maker application, and the European Environment Agency recommends its usage for European mapping for statistical analysis and display. It is also used in scientific disciplines such as geology for plotting the orientations of lines in three-dimensional space. This plotting is aided by a special kind of graph paper called a Schmidt net."@en . "\u0420\u0430\u0432\u043D\u043E\u0432\u0435\u043B\u0438\u043A\u0430\u044F \u0430\u0437\u0438\u043C\u0443\u0442\u0430\u043B\u044C\u043D\u0430\u044F \u043F\u0440\u043E\u0435\u043A\u0446\u0438\u044F \u041B\u0430\u043C\u0431\u0435\u0440\u0442\u0430"@ru . . . . . "La proyecci\u00F3n acimutal equivalente de Lambert (LAEA, por sus siglas en ingl\u00E9s Lambert azimuthal equal-area) conserva deliberadamente las \u00E1reas. Es una proyecci\u00F3n particular de esfera a disco. No debe ser confundida con la Proyecci\u00F3n Conforme C\u00F3nica de Lambert que es muy utilizada en navegaci\u00F3n a\u00E9rea.La proyecci\u00F3n acimutal equivalente de Lambert no es conforme, es decir, no mantiene el valor real de los \u00E1ngulos tras realizar la proyecci\u00F3n. La escala disminuye a medida que nos acercamos al borde exterior, pero en menor medida que en la proyecci\u00F3n ortogr\u00E1fica. Este sistema es muy adecuado para trazar mapas de peque\u00F1a escala."@es . .