"Un fluido barotropico \u00E8 un fluido in cui la pressione \u00E8 costante sulle superfici di uguale densit\u00E0. Anche se questa condizione difficilmente si realizza in condizioni di regime turbolento, si tratta di un'approssimazione largamente usata in fluidodinamica, in meteorologia e in climatologia, perch\u00E9 consente di semplificare la trattazione di molti fenomeni, restituendo risultati qualitativamente e quantitativamente accettabili. Spesso il suo significato \u00E8 esteso a indicare un fluido omogeneo con densit\u00E0 costante. Il concetto \u00E8 usato in contrasto col termine baroclino, che invece designa un fluido in cui la pressione dipende dalla densit\u00E0 e dalla temperatura. Un altro modo per definire questo particolare tipo di fluido \u00E8 dire che il gradiente di pressione e il gradiente di densit\u00E0 sono paralleli (possono anche non essere equiversi). Questa formulazione rende immediata l'importanza di tali fluidi: dalla equazione della vorticit\u00E0 si rileva infatti che sotto questa ipotesi la variazione di vorticit\u00E0 dipende esclusivamente dai gradienti di velocit\u00E0 nel flusso."@it . "La barotrop\u00EDa de un fluido es una caracter\u00EDstica por la cual las l\u00EDneas de presi\u00F3n constantes (isobara) coinciden con las de densidad constantes (isopicna). Ello permite una relaci\u00F3n en la que la presi\u00F3n solo depende de la densidad, no de otros campos; esto es P=P(\u03C1). En general, cualquier fluido isoentr\u00F3pico o isotermo ser\u00E1 un bar\u00F3tropo. Esto sucede en la atm\u00F3sfera terrestre en los tr\u00F3picos, ya que all\u00ED las diferencias de temperatura entre una zona y otra al mismo nivel son peque\u00F1as. Lo contrario de una atm\u00F3sfera barotr\u00F3pica es una atm\u00F3sfera baroclina. \n* Datos: Q739293"@es . "Barotropic fluid"@en . . "Barotropi"@sv . . "En m\u00E9canique des fluides, un fluide barotrope est celui dont les lignes d'\u00E9gale pression sont parall\u00E8les \u00E0 celles d'\u00E9gale densit\u00E9 (isopycne). Ce qualificatif est utilis\u00E9 dans plusieurs domaines dont la m\u00E9t\u00E9orologie, l'oc\u00E9anographie physique et l'astrophysique pour d\u00E9crire des gaz ou liquides dont les propri\u00E9t\u00E9s ne varient pas avec l'\u00E9paisseur."@fr . . "Barotropico"@it . . . . "\u0411\u0430\u0440\u043E\u0442\u0440\u043E\u043F\u043D\u0430 \u0440\u0456\u0434\u0438\u043D\u0430 \u2014 \u0440\u0456\u0434\u0438\u043D\u0430, \u0433\u0443\u0441\u0442\u0438\u043D\u0430 \u044F\u043A\u043E\u0457 \u0454 \u0444\u0443\u043D\u043A\u0446\u0456\u0454\u044E \u0442\u0456\u043B\u044C\u043A\u0438 \u0442\u0438\u0441\u043A\u0443 \u0456 \u043D\u0435 \u0437\u0430\u043B\u0435\u0436\u0438\u0442\u044C \u0432\u0456\u0434 \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u0438 \u0437\u0433\u0456\u0434\u043D\u043E \u0437 \u0440\u0456\u0432\u043D\u044F\u043D\u043D\u044F\u043C \u0441\u0442\u0430\u043D\u0443. \u0410\u043F\u0440\u043E\u043A\u0441\u0438\u043C\u0430\u0446\u0456\u044F \u0431\u0430\u0440\u043E\u0442\u0440\u043E\u043F\u043D\u043E\u0457 \u0440\u0456\u0434\u0438\u043D\u0438 \u0432\u0438\u043A\u043E\u0440\u0438\u0441\u0442\u043E\u0432\u0443\u0454\u0442\u044C\u0441\u044F \u0432 \u0444\u0456\u0437\u0438\u0446\u0456 \u0430\u0442\u043C\u043E\u0441\u0444\u0435\u0440\u0438, \u043E\u043A\u0435\u0430\u043D\u043E\u0433\u0440\u0430\u0444\u0456\u0457 \u0430\u0431\u043E \u0430\u0441\u0442\u0440\u043E\u0444\u0456\u0437\u0438\u0446\u0456[\u0434\u0436\u0435\u0440\u0435\u043B\u043E?]. \u0420\u0456\u0434\u0438\u043D\u0430, \u044F\u043A\u0430 \u043D\u0435 \u0432\u0456\u0434\u043F\u043E\u0432\u0456\u0434\u0430\u0454 \u0443\u043C\u043E\u0432\u0430\u043C \u0431\u0430\u0440\u043E\u0442\u0440\u043E\u043F\u0456\u0457, \u043D\u0430\u0437\u0438\u0432\u0430\u0454\u0442\u044C\u0441\u044F \u0431\u0430\u0440\u043E\u043A\u043B\u0456\u043D\u0456\u0447\u043D\u043E\u044E \u0440\u0456\u0434\u0438\u043D\u043E\u044E[\u0434\u0436\u0435\u0440\u0435\u043B\u043E?]. \u0413\u0443\u0441\u0442\u0438\u043D\u0430 \u0431\u0430\u0433\u0430\u0442\u044C\u043E\u0445 \u0440\u0456\u0434\u0438\u043D, \u043D\u0430\u043F\u0440\u0438\u043A\u043B\u0430\u0434 \u0432\u043E\u0434\u0438, \u043C\u0430\u0439\u0436\u0435 \u043F\u043E\u0441\u0442\u0456\u0439\u043D\u0430 \u0456 \u0434\u0435\u0449\u043E \u0437\u0430\u043B\u0435\u0436\u0438\u0442\u044C \u0432\u0456\u0434 \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u0438 \u0442\u0430 \u0441\u043E\u043B\u043E\u043D\u043E\u0441\u0442\u0456. \u0413\u0443\u0441\u0442\u0438\u043D\u0430 \u0433\u0430\u0437\u0456\u0432, \u0432\u043A\u043B\u044E\u0447\u0430\u044E\u0447\u0438 \u043F\u043E\u0432\u0456\u0442\u0440\u044F, \u044F\u043A \u043F\u0440\u0430\u0432\u0438\u043B\u043E, \u043D\u0435 \u0432\u0456\u0434\u043F\u043E\u0432\u0456\u0434\u0430\u0454 \u0431\u0430\u0440\u043E\u0442\u0440\u043E\u043F\u043D\u0438\u043C \u0443\u043C\u043E\u0432\u0430\u043C, \u0430\u043B\u0435 \u044F\u043A\u0449\u043E \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u0456 \u0442\u0456\u0454\u0457 \u0436 \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u0438 \u0454 \u043F\u0430\u0440\u0430\u043B\u0435\u043B\u044C\u043D\u0438\u043C\u0438 \u0434\u043E \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u0456 \u0437 \u0442\u0430\u043A\u0438\u043C \u0436\u0435 \u0442\u0438\u0441\u043A\u043E\u043C, \u0442\u043E \u0430\u0442\u043C\u043E\u0441\u0444\u0435\u0440\u0430 \u0431\u0430\u0440\u043E\u0442\u0440\u043E\u043F\u043D\u0430. \u0423 \u0431\u0430\u0433\u0430\u0442\u044C\u043E\u0445 \u0442\u0438\u043F\u0430\u0445 \u043F\u043E\u0442\u043E\u043A\u0456\u0432 \u0446\u0435 \u043F\u0440\u0438\u043F\u0443\u0449\u0435\u043D\u043D\u044F \u0432\u0438\u043A\u043E\u043D\u0443\u0454\u0442\u044C\u0441\u044F \u0430\u0431\u043E \u043F\u0435\u0440\u0435\u0434\u0431\u0430\u0447\u0430\u0454\u0442\u044C\u0441\u044F \u044F\u043A \u043F\u0440\u0438\u043F\u0443\u0449\u0435\u043D\u043D\u044F \u043C\u043E\u0434\u0435\u043B\u0456. \u041F\u0440\u0438\u043A\u043B\u0430\u0434\u043E\u043C \u043C\u043E\u0436\u0435 \u0441\u043B\u0443\u0436\u0438\u0442\u0438 \u0437\u0430\u0441\u0442\u043E\u0441\u0443\u0432\u0430\u043D\u043D\u044F \u043F\u0440\u0438\u043D\u0446\u0438\u043F\u0443 \u043F\u043E\u0442\u0435\u043D\u0446\u0456\u0439\u043D\u043E\u0433\u043E \u0431\u0430\u0440\u043E\u0442\u0440\u043E\u043F\u043D\u043E\u0433\u043E \u0437\u0430\u0432\u0438\u0445\u043D\u0435\u043D\u043D\u044F \u0437 \u043D\u0430\u0431\u043B\u0438\u0436\u0435\u043D\u0438\u043C \u0431\u0430\u0440\u043E\u0442\u0440\u043E\u043F\u043D\u0438\u043C \u043E\u043F\u0438\u0441\u043E\u043C \u0445\u0432\u0438\u043B\u044C \u0420\u043E\u0441\u0441\u0431\u0456 \u0432 \u0430\u0442\u043C\u043E\u0441\u0444\u0435\u0440\u0456.."@uk . . . . . . "\u6D41\u4F53\u529B\u5B66\u306B\u304A\u3044\u3066\u3001\u6D41\u4F53\u304C\u9806\u5727\uFF08\u3058\u3085\u3093\u3042\u3064\uFF09\u3067\u3042\u308B\u3001\u3042\u308B\u3044\u306F\u30D0\u30ED\u30C8\u30ED\u30D4\u30C3\u30AF\uFF08\u82F1: barotropic\uFF09\u3067\u3042\u308B\u3068\u306F\u3001\u5727\u529B\u304C\u5BC6\u5EA6\u306E\u307F\u306B\u4F9D\u5B58\u3059\u308B\u3053\u3068\u3001\u3059\u306A\u308F\u3061\u3001\u7B49\u5727\u9762\u3068\u7B49\u5BC6\u5EA6\u9762\u304C\u4E00\u81F4\u3059\u308B\u3053\u3068\u3092\u3044\u3046\u3002 \u5929\u4F53\u529B\u5B66\u3067\u3001\u6052\u661F\u5185\u90E8\u306E\u6D41\u4F53\u306E\u30E2\u30C7\u30EB\u3068\u3057\u3066\u4F7F\u308F\u308C\u308B\u30DD\u30EA\u30C8\u30ED\u30D4\u30C3\u30AF\u6D41\u4F53\uFF08\u5727\u529B\u304C\u5BC6\u5EA6\u306E\u3079\u304D\u4E57\u3067\u8868\u305B\u308B\u6D41\u4F53\uFF09\u3082\u30D0\u30ED\u30C8\u30ED\u30D4\u30C3\u30AF\u6D41\u4F53\u306E\u3088\u304F\u77E5\u3089\u308C\u305F\u4F8B\u3067\u3042\u308B\u3002\u307E\u305F\u3001\u5BC6\u5EA6\u4E00\u5B9A\u306E\u6D41\u4F53\uFF08\u03C1=constant\uFF09\u3082\u30D0\u30ED\u30C8\u30ED\u30D4\u30C3\u30AF\u6D41\u4F53\u306E\u4E00\u3064\u3067\u3042\u308B\u3002"@ja . "Barotropi r\u00E5der i en v\u00E4tska, eller annan fluid, d\u00E5 ytskikt med lika tryck (isobarer) och ytskikt med lika temperatur (isotermer) \u00E4r parallella med varandra. I en s\u00E5dan idealiserad, barotrop fluid \u00E4r trycket enbart en funktion av densiteten och de horisontella str\u00F6mmarna f\u00F6rblir konstanta inom ett lager. Motsatsen till barotropi kallas baroklinitet."@sv . . "\u6B63\u58D3\u5927\u6C23\u662F\u7576\u5927\u6C23\u58D3\u529B\u50C5\u50C5\u53D6\u6C7A\u65BC\u5927\u6C23\u5BC6\u5EA6\u3001\u4EE5\u53CA\u5927\u6C23\u5BC6\u5EA6\u4EA6\u50C5\u53D6\u65BC\u5927\u6C23\u6C23\u58D3\u3002\u56E0\u6B64\uFF0C\u5728\u6B63\u58D3\u5927\u6C23\u5167\uFF0C\u4EA6\u5373\u70BA\u3002 \u82E5\u76F8\u95DC\u5927\u6C23\u4E43\u7406\u60F3\u6C23\u9AD4\uFF0C\u5247\u3001\u8207\u4EA6\u70BA\u540C\u4E00\u5E73\u9762\u3002\u56E0\u800C\uFF0C\u5730\u8F49\u98A8\u4E0D\u56E0\u5927\u6C23\u9AD8\u5EA6\u6539\u8B8A\u800C\u8B8A\u5316\uFF0C\u6545\u6B64\u5927\u5C3A\u5EA6\u74B0\u6D41\u4EA6\u4E0D\u96A8\u9AD8\u5EA6\u8B8A\u5316\u3002 \u7531\u65BC\u6B63\u58D3\u5927\u6C23\u5177\u6709\u9019\u7A2E\u7279\u6027\uFF0C\u56E0\u6B64\u6C23\u8C61\u7814\u7A76\u5E38\u5047\u8A2D\u6B63\u58D3\u5927\u6C23\u4EE5\u7C21\u5316\u8A08\u7B97\u3002"@zh . . . . "Barotrope"@fr . . . "Barotropia"@ca . . . "En m\u00E9canique des fluides, un fluide barotrope est celui dont les lignes d'\u00E9gale pression sont parall\u00E8les \u00E0 celles d'\u00E9gale densit\u00E9 (isopycne). Ce qualificatif est utilis\u00E9 dans plusieurs domaines dont la m\u00E9t\u00E9orologie, l'oc\u00E9anographie physique et l'astrophysique pour d\u00E9crire des gaz ou liquides dont les propri\u00E9t\u00E9s ne varient pas avec l'\u00E9paisseur."@fr . "Unter Barotropie (von griechisch baros \u201EDruck\u201C und tropos \u201EDrehung, Richtung\u201C) versteht man die Eigenschaft der Dichte eines Fluids, nur vom Druck abzuh\u00E4ngen: . Dies f\u00FChrt dazu, dass Fl\u00E4chen gleichen Druckes (Isobaren) und gleicher Temperatur (Isothermen) parallel zueinander verlaufen. Das Gegenst\u00FCck zur Barotropie ist die Baroklinit\u00E4t. Die Abbildungen zeigen extrem \u00FCbertriebene Neigungen, die in der Realit\u00E4t meist \u00E4u\u00DFerst klein und daher schwer messbar sind."@de . . "Barotropia"@pt . . . . . . "In fluid dynamics, a barotropic fluid is a fluid whose density is a function of pressure only. The barotropic fluid is a useful model of fluid behavior in a wide variety of scientific fields, from meteorology to astrophysics. In astrophysics, barotropic fluids are important in the study of stellar interiors or of the interstellar medium. One common class of barotropic model used in astrophysics is a polytropic fluid. Typically, the barotropic assumption is not very realistic."@en . . "\uC21C\uC555(\u9806\u58D3, barotropic)\uD558\uB2E4 \uD568\uC740 \uC720\uCCB4\uC5ED\uD559\uC5D0\uC11C \uBC00\uB3C4\uAC00 \uC555\uB825\uC758 \uD568\uC218\uB85C\uB9CC \uC815\uD574\uC9C0\uB294 \uAC83\uC744 \uB9D0\uD55C\uB2E4. \uC720\uCCB4\uB97C \uC21C\uC555\uD558\uB2E4\uACE0 \uADFC\uC0AC\uD558\uB294 \uAC83\uC740 \uAE30\uC0C1\uD559\uC5D0\uC11C \uCC9C\uCCB4\uBB3C\uB9AC\uD559\uAE4C\uC9C0 \uB2E4\uC591\uD55C \uBD84\uC57C\uC5D0\uC11C \uC720\uC6A9\uD558\uAC8C \uC0AC\uC6A9\uB41C\uB2E4. \uB300\uBD80\uBD84\uC758 \uC720\uCCB4\uB294 \uBC00\uB3C4\uAC00 \uC77C\uC815\uD558\uBA70, \uC555\uB825\uACFC \uC628\uB3C4\uC5D0 \uB530\uB77C \uB9E4\uC6B0 \uACBD\uBBF8\uD558\uAC8C \uBC00\uB3C4\uAC00 \uBCC0\uD55C\uB2E4\uACE0 \uB9D0\uD560 \uC218 \uC788\uB2E4. \uC628\uB3C4\uC640 \uC5FC\uB3C4\uC5D0 \uBC00\uB3C4\uAC00 \uBCC0\uD558\uB294 \uC815\uB3C4\uAC00 \uC218 \uD37C\uC13C\uD2B8\uC5D0 \uBD88\uACFC\uD55C \uBB3C\uC740 \uB300\uCDA9 \uC21C\uC555\uD558\uB2E4\uACE0 \uB9D0\uD560 \uC218 \uC788\uB2E4. \uD558\uC9C0\uB9CC \uC628\uB3C4\uC640 \uC555\uB825\uC5D0 \uC758\uD574 \uB3D9\uC2DC\uC5D0 \uBC00\uB3C4\uAC00 \uD06C\uAC8C \uBCC0\uD558\uB294 \uACF5\uAE30 \uAC19\uC740 \uAC83\uC740 \uC77C\uBC18\uC801\uC73C\uB85C \uC21C\uC555\uD558\uC9C0 \uC544\uB2C8\uD558\uB2E4. \uCC9C\uCCB4\uBB3C\uB9AC\uD559\uC5D0\uC11C\uB294 \uD56D\uC131 \uB0B4\uBD80\uAD6C\uC870\uB098 \uC131\uAC04\uB9E4\uC9C8\uC744 \uC5F0\uAD6C\uD560 \uB54C \uC774\uAC83\uB4E4\uC774 \uC21C\uC555\uC720\uCCB4\uB77C\uACE0 \uAC00\uC815\uD55C\uB2E4. \uCC9C\uCCB4\uBB3C\uB9AC\uD559\uC5D0\uC11C \uC0AC\uC6A9\uD558\uB294 \uB300\uD45C\uC801\uC778 \uC21C\uC555 \uBAA8\uD615\uC774 \uB2E4\uBC29\uC720\uCCB4 \uBAA8\uD615\uC774\uB2E4. \uAE30\uC0C1\uD559\uC5D0\uC11C\uB294 \uC555\uB825\uC5D0 \uC758\uD574\uC11C\uB9CC \uBC00\uB3C4\uAC00 \uACB0\uC815\uB418\uB294 \uACF5\uAE30\uB97C \uC21C\uC555\uB300\uAE30(barotropic atmosphere)\uB77C\uACE0 \uD55C\uB2E4. \uC21C\uC555\uB300\uAE30\uB294 \uB4F1\uC555\uBA74 \uBC0F \uB4F1\uBC00\uB3C4\uBA74\uC758 \uACB0\uACFC \uBC1C\uC0DD\uD558\uBA70, \uC774\uB7F0 \uB4F1\uC555\uBA74\uB4E4\uC740 \uB610\uD55C \uB4F1\uC628\uBA74\uC774\uAE30\uB3C4 \uD558\uB2E4. \uADF8\uB798\uC11C \uC9C0\uADE0\uD48D\uC740 \uAE4A\uC774\uC5D0 \uB530\uB77C \uD48D\uC18D\uC774 \uD06C\uAC8C \uBCC0\uD558\uC9C0 \uC54A\uB294\uB2E4. \uC21C\uC555\uD558\uC9C0 \uC54A\uC740 \uC720\uCCB4\uB294 \uD558\uB2E4\uACE0 \uD55C\uB2E4. \uC21C\uC555\uC720\uCCB4 \uBC0F \uC21C\uC555\uC720\uB3D9\uC5D0\uC11C\uB294 \uAC00 0\uC774\uB2E4."@ko . . "La barotrop\u00EDa de un fluido es una caracter\u00EDstica por la cual las l\u00EDneas de presi\u00F3n constantes (isobara) coinciden con las de densidad constantes (isopicna). Ello permite una relaci\u00F3n en la que la presi\u00F3n solo depende de la densidad, no de otros campos; esto es P=P(\u03C1). En general, cualquier fluido isoentr\u00F3pico o isotermo ser\u00E1 un bar\u00F3tropo. Esto sucede en la atm\u00F3sfera terrestre en los tr\u00F3picos, ya que all\u00ED las diferencias de temperatura entre una zona y otra al mismo nivel son peque\u00F1as. Lo contrario de una atm\u00F3sfera barotr\u00F3pica es una atm\u00F3sfera baroclina. \n* Datos: Q739293"@es . "\uC21C\uC555(\u9806\u58D3, barotropic)\uD558\uB2E4 \uD568\uC740 \uC720\uCCB4\uC5ED\uD559\uC5D0\uC11C \uBC00\uB3C4\uAC00 \uC555\uB825\uC758 \uD568\uC218\uB85C\uB9CC \uC815\uD574\uC9C0\uB294 \uAC83\uC744 \uB9D0\uD55C\uB2E4. \uC720\uCCB4\uB97C \uC21C\uC555\uD558\uB2E4\uACE0 \uADFC\uC0AC\uD558\uB294 \uAC83\uC740 \uAE30\uC0C1\uD559\uC5D0\uC11C \uCC9C\uCCB4\uBB3C\uB9AC\uD559\uAE4C\uC9C0 \uB2E4\uC591\uD55C \uBD84\uC57C\uC5D0\uC11C \uC720\uC6A9\uD558\uAC8C \uC0AC\uC6A9\uB41C\uB2E4. \uB300\uBD80\uBD84\uC758 \uC720\uCCB4\uB294 \uBC00\uB3C4\uAC00 \uC77C\uC815\uD558\uBA70, \uC555\uB825\uACFC \uC628\uB3C4\uC5D0 \uB530\uB77C \uB9E4\uC6B0 \uACBD\uBBF8\uD558\uAC8C \uBC00\uB3C4\uAC00 \uBCC0\uD55C\uB2E4\uACE0 \uB9D0\uD560 \uC218 \uC788\uB2E4. \uC628\uB3C4\uC640 \uC5FC\uB3C4\uC5D0 \uBC00\uB3C4\uAC00 \uBCC0\uD558\uB294 \uC815\uB3C4\uAC00 \uC218 \uD37C\uC13C\uD2B8\uC5D0 \uBD88\uACFC\uD55C \uBB3C\uC740 \uB300\uCDA9 \uC21C\uC555\uD558\uB2E4\uACE0 \uB9D0\uD560 \uC218 \uC788\uB2E4. \uD558\uC9C0\uB9CC \uC628\uB3C4\uC640 \uC555\uB825\uC5D0 \uC758\uD574 \uB3D9\uC2DC\uC5D0 \uBC00\uB3C4\uAC00 \uD06C\uAC8C \uBCC0\uD558\uB294 \uACF5\uAE30 \uAC19\uC740 \uAC83\uC740 \uC77C\uBC18\uC801\uC73C\uB85C \uC21C\uC555\uD558\uC9C0 \uC544\uB2C8\uD558\uB2E4. \uCC9C\uCCB4\uBB3C\uB9AC\uD559\uC5D0\uC11C\uB294 \uD56D\uC131 \uB0B4\uBD80\uAD6C\uC870\uB098 \uC131\uAC04\uB9E4\uC9C8\uC744 \uC5F0\uAD6C\uD560 \uB54C \uC774\uAC83\uB4E4\uC774 \uC21C\uC555\uC720\uCCB4\uB77C\uACE0 \uAC00\uC815\uD55C\uB2E4. \uCC9C\uCCB4\uBB3C\uB9AC\uD559\uC5D0\uC11C \uC0AC\uC6A9\uD558\uB294 \uB300\uD45C\uC801\uC778 \uC21C\uC555 \uBAA8\uD615\uC774 \uB2E4\uBC29\uC720\uCCB4 \uBAA8\uD615\uC774\uB2E4. \uAE30\uC0C1\uD559\uC5D0\uC11C\uB294 \uC555\uB825\uC5D0 \uC758\uD574\uC11C\uB9CC \uBC00\uB3C4\uAC00 \uACB0\uC815\uB418\uB294 \uACF5\uAE30\uB97C \uC21C\uC555\uB300\uAE30(barotropic atmosphere)\uB77C\uACE0 \uD55C\uB2E4. \uC21C\uC555\uB300\uAE30\uB294 \uB4F1\uC555\uBA74 \uBC0F \uB4F1\uBC00\uB3C4\uBA74\uC758 \uACB0\uACFC \uBC1C\uC0DD\uD558\uBA70, \uC774\uB7F0 \uB4F1\uC555\uBA74\uB4E4\uC740 \uB610\uD55C \uB4F1\uC628\uBA74\uC774\uAE30\uB3C4 \uD558\uB2E4. \uADF8\uB798\uC11C \uC9C0\uADE0\uD48D\uC740 \uAE4A\uC774\uC5D0 \uB530\uB77C \uD48D\uC18D\uC774 \uD06C\uAC8C \uBCC0\uD558\uC9C0 \uC54A\uB294\uB2E4. \uC21C\uC555\uB300\uAE30\uB97C \uC77C\uBC18\uD654\uD55C \uAC83\uC744 \uC21C\uC555\uC720\uB3D9(barotropic flow)\uC774\uB77C \uD55C\uB2E4. \uC21C\uC555\uC720\uB3D9\uC740 \uC555\uB825\uC774 \uBC00\uB3C4\uC758 \uD568\uC218\uB85C\uB9CC \uACB0\uC815\uB418\uACE0 \uB610\uD55C \uBC00\uB3C4\uAC00 \uC555\uB825\uC758 \uD568\uC218\uB85C\uB9CC \uACB0\uC815\uB418\uB294 \uD750\uB984\uC774\uB2E4. \uB2E4\uC2DC \uB9D0\uD558\uBA74 \uB4F1\uC555\uBA74\uC774 \uB4F1\uBC00\uB3C4\uBA74\uC774\uACE0 \uB4F1\uBC00\uB3C4\uBA74\uC774 \uB4F1\uC555\uBA74\uC778 \uD750\uB984\uC774\uB2E4. \uBE44\uC21C\uC555\uC720\uCCB4\uAC00 \uC21C\uC555\uC720\uB3D9\uC744 \uD560 \uC218\uB3C4 \uC788\uC9C0\uB9CC, \uC21C\uC555\uC720\uCCB4\uB294 \uC5B8\uC81C\uB098 \uC21C\uC555\uC720\uB3D9\uC744 \uD55C\uB2E4. \uC21C\uC555\uC720\uB3D9\uC758 \uC608\uB85C\uB294 \uBC14\uB2E4\uC758 \uC21C\uC555\uCE35, \uB4F1\uC628\uC774\uC0C1\uAE30\uCCB4, \uB4F1\uBC00\uB3C4\uC774\uC0C1\uAE30\uCCB4 \uB4F1\uC774 \uC788\uB2E4. \uC21C\uC555\uD558\uC9C0 \uC54A\uC740 \uC720\uCCB4\uB294 \uD558\uB2E4\uACE0 \uD55C\uB2E4. \uC21C\uC555\uC720\uCCB4 \uBC0F \uC21C\uC555\uC720\uB3D9\uC5D0\uC11C\uB294 \uAC00 0\uC774\uB2E4."@ko . . "P\u0142yn barotropowy - p\u0142yn, kt\u00F3rego g\u0119sto\u015B\u0107 jest sta\u0142a lub zale\u017Cna tylko od ci\u015Bnienia. Przybli\u017Cenie p\u0142ynu barotropowego jest u\u017Cywane w fizyce atmosfery, oceanografii czy te\u017C w astrofizyce. P\u0142yn niespe\u0142niaj\u0105cy warunku barotropowo\u015Bci nazywa si\u0119 p\u0142ynem baroklinowym."@pl . . . . "En meteorologia, la barotropia d'un fluid \u00E9s una caracter\u00EDstica per la qual les l\u00EDnies de pressi\u00F3 constants (is\u00F2bares) coincideixen amb les de densitat constants. Aix\u00F2 permet una relaci\u00F3 en qu\u00E8 la pressi\u00F3 nom\u00E9s dep\u00E8n de la densitat, no d'altres camps, \u00E9s a dir:. Els fluids barotr\u00F2pics s\u00F3n tamb\u00E9 fluids idealitzats importants en astrof\u00EDsica, com l'estudi de l'interior estel\u00B7lar o del medi interestel\u00B7lar."@ca . "Barotropi r\u00E5der i en v\u00E4tska, eller annan fluid, d\u00E5 ytskikt med lika tryck (isobarer) och ytskikt med lika temperatur (isotermer) \u00E4r parallella med varandra. I en s\u00E5dan idealiserad, barotrop fluid \u00E4r trycket enbart en funktion av densiteten och de horisontella str\u00F6mmarna f\u00F6rblir konstanta inom ett lager. Motsatsen till barotropi kallas baroklinitet."@sv . . "\uC21C\uC555"@ko . "P\u0142yn barotropowy"@pl . . "\u0411\u0430\u0440\u043E\u0442\u0440\u043E\u043F\u043D\u0430 \u0440\u0456\u0434\u0438\u043D\u0430 \u2014 \u0440\u0456\u0434\u0438\u043D\u0430, \u0433\u0443\u0441\u0442\u0438\u043D\u0430 \u044F\u043A\u043E\u0457 \u0454 \u0444\u0443\u043D\u043A\u0446\u0456\u0454\u044E \u0442\u0456\u043B\u044C\u043A\u0438 \u0442\u0438\u0441\u043A\u0443 \u0456 \u043D\u0435 \u0437\u0430\u043B\u0435\u0436\u0438\u0442\u044C \u0432\u0456\u0434 \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u0438 \u0437\u0433\u0456\u0434\u043D\u043E \u0437 \u0440\u0456\u0432\u043D\u044F\u043D\u043D\u044F\u043C \u0441\u0442\u0430\u043D\u0443. \u0410\u043F\u0440\u043E\u043A\u0441\u0438\u043C\u0430\u0446\u0456\u044F \u0431\u0430\u0440\u043E\u0442\u0440\u043E\u043F\u043D\u043E\u0457 \u0440\u0456\u0434\u0438\u043D\u0438 \u0432\u0438\u043A\u043E\u0440\u0438\u0441\u0442\u043E\u0432\u0443\u0454\u0442\u044C\u0441\u044F \u0432 \u0444\u0456\u0437\u0438\u0446\u0456 \u0430\u0442\u043C\u043E\u0441\u0444\u0435\u0440\u0438, \u043E\u043A\u0435\u0430\u043D\u043E\u0433\u0440\u0430\u0444\u0456\u0457 \u0430\u0431\u043E \u0430\u0441\u0442\u0440\u043E\u0444\u0456\u0437\u0438\u0446\u0456[\u0434\u0436\u0435\u0440\u0435\u043B\u043E?]. \u0420\u0456\u0434\u0438\u043D\u0430, \u044F\u043A\u0430 \u043D\u0435 \u0432\u0456\u0434\u043F\u043E\u0432\u0456\u0434\u0430\u0454 \u0443\u043C\u043E\u0432\u0430\u043C \u0431\u0430\u0440\u043E\u0442\u0440\u043E\u043F\u0456\u0457, \u043D\u0430\u0437\u0438\u0432\u0430\u0454\u0442\u044C\u0441\u044F \u0431\u0430\u0440\u043E\u043A\u043B\u0456\u043D\u0456\u0447\u043D\u043E\u044E \u0440\u0456\u0434\u0438\u043D\u043E\u044E[\u0434\u0436\u0435\u0440\u0435\u043B\u043E?]."@uk . "Un fluido barotropico \u00E8 un fluido in cui la pressione \u00E8 costante sulle superfici di uguale densit\u00E0. Anche se questa condizione difficilmente si realizza in condizioni di regime turbolento, si tratta di un'approssimazione largamente usata in fluidodinamica, in meteorologia e in climatologia, perch\u00E9 consente di semplificare la trattazione di molti fenomeni, restituendo risultati qualitativamente e quantitativamente accettabili. Spesso il suo significato \u00E8 esteso a indicare un fluido omogeneo con densit\u00E0 costante. Il concetto \u00E8 usato in contrasto col termine baroclino, che invece designa un fluido in cui la pressione dipende dalla densit\u00E0 e dalla temperatura."@it . . "1031851181"^^ . . "3442"^^ . . "Unter Barotropie (von griechisch baros \u201EDruck\u201C und tropos \u201EDrehung, Richtung\u201C) versteht man die Eigenschaft der Dichte eines Fluids, nur vom Druck abzuh\u00E4ngen: . Dies f\u00FChrt dazu, dass Fl\u00E4chen gleichen Druckes (Isobaren) und gleicher Temperatur (Isothermen) parallel zueinander verlaufen. Das Gegenst\u00FCck zur Barotropie ist die Baroklinit\u00E4t. Die Abbildungen zeigen extrem \u00FCbertriebene Neigungen, die in der Realit\u00E4t meist \u00E4u\u00DFerst klein und daher schwer messbar sind."@de . "A barotropia de um fluido \u00E9 uma caracter\u00EDstica pela qual a densidade do fluido s\u00F3 depende da press\u00E3o, j\u00E1 que a temperatura \u00E9 constante. Isto sucede na atmosfera terrestre nos tr\u00F3picos, j\u00E1 que a\u00ED as diferen\u00E7as de temperatura entre uma zona e outra ao mesmo n\u00EDvel s\u00E3o pequenas. Quando a atmosfera n\u00E3o \u00E9 barotr\u00F3pica \u00E9 uma atmosfera bar\u00F3clina."@pt . "\u6D41\u4F53\u529B\u5B66\u306B\u304A\u3044\u3066\u3001\u6D41\u4F53\u304C\u9806\u5727\uFF08\u3058\u3085\u3093\u3042\u3064\uFF09\u3067\u3042\u308B\u3001\u3042\u308B\u3044\u306F\u30D0\u30ED\u30C8\u30ED\u30D4\u30C3\u30AF\uFF08\u82F1: barotropic\uFF09\u3067\u3042\u308B\u3068\u306F\u3001\u5727\u529B\u304C\u5BC6\u5EA6\u306E\u307F\u306B\u4F9D\u5B58\u3059\u308B\u3053\u3068\u3001\u3059\u306A\u308F\u3061\u3001\u7B49\u5727\u9762\u3068\u7B49\u5BC6\u5EA6\u9762\u304C\u4E00\u81F4\u3059\u308B\u3053\u3068\u3092\u3044\u3046\u3002 \u5929\u4F53\u529B\u5B66\u3067\u3001\u6052\u661F\u5185\u90E8\u306E\u6D41\u4F53\u306E\u30E2\u30C7\u30EB\u3068\u3057\u3066\u4F7F\u308F\u308C\u308B\u30DD\u30EA\u30C8\u30ED\u30D4\u30C3\u30AF\u6D41\u4F53\uFF08\u5727\u529B\u304C\u5BC6\u5EA6\u306E\u3079\u304D\u4E57\u3067\u8868\u305B\u308B\u6D41\u4F53\uFF09\u3082\u30D0\u30ED\u30C8\u30ED\u30D4\u30C3\u30AF\u6D41\u4F53\u306E\u3088\u304F\u77E5\u3089\u308C\u305F\u4F8B\u3067\u3042\u308B\u3002\u307E\u305F\u3001\u5BC6\u5EA6\u4E00\u5B9A\u306E\u6D41\u4F53\uFF08\u03C1=constant\uFF09\u3082\u30D0\u30ED\u30C8\u30ED\u30D4\u30C3\u30AF\u6D41\u4F53\u306E\u4E00\u3064\u3067\u3042\u308B\u3002"@ja . "\u9806\u5727"@ja . "A barotropia de um fluido \u00E9 uma caracter\u00EDstica pela qual a densidade do fluido s\u00F3 depende da press\u00E3o, j\u00E1 que a temperatura \u00E9 constante. Isto sucede na atmosfera terrestre nos tr\u00F3picos, j\u00E1 que a\u00ED as diferen\u00E7as de temperatura entre uma zona e outra ao mesmo n\u00EDvel s\u00E3o pequenas. Quando a atmosfera n\u00E3o \u00E9 barotr\u00F3pica \u00E9 uma atmosfera bar\u00F3clina."@pt . "\u6B63\u58D3\u5927\u6C23\u662F\u7576\u5927\u6C23\u58D3\u529B\u50C5\u50C5\u53D6\u6C7A\u65BC\u5927\u6C23\u5BC6\u5EA6\u3001\u4EE5\u53CA\u5927\u6C23\u5BC6\u5EA6\u4EA6\u50C5\u53D6\u65BC\u5927\u6C23\u6C23\u58D3\u3002\u56E0\u6B64\uFF0C\u5728\u6B63\u58D3\u5927\u6C23\u5167\uFF0C\u4EA6\u5373\u70BA\u3002 \u82E5\u76F8\u95DC\u5927\u6C23\u4E43\u7406\u60F3\u6C23\u9AD4\uFF0C\u5247\u3001\u8207\u4EA6\u70BA\u540C\u4E00\u5E73\u9762\u3002\u56E0\u800C\uFF0C\u5730\u8F49\u98A8\u4E0D\u56E0\u5927\u6C23\u9AD8\u5EA6\u6539\u8B8A\u800C\u8B8A\u5316\uFF0C\u6545\u6B64\u5927\u5C3A\u5EA6\u74B0\u6D41\u4EA6\u4E0D\u96A8\u9AD8\u5EA6\u8B8A\u5316\u3002 \u7531\u65BC\u6B63\u58D3\u5927\u6C23\u5177\u6709\u9019\u7A2E\u7279\u6027\uFF0C\u56E0\u6B64\u6C23\u8C61\u7814\u7A76\u5E38\u5047\u8A2D\u6B63\u58D3\u5927\u6C23\u4EE5\u7C21\u5316\u8A08\u7B97\u3002"@zh . . "En meteorologia, la barotropia d'un fluid \u00E9s una caracter\u00EDstica per la qual les l\u00EDnies de pressi\u00F3 constants (is\u00F2bares) coincideixen amb les de densitat constants. Aix\u00F2 permet una relaci\u00F3 en qu\u00E8 la pressi\u00F3 nom\u00E9s dep\u00E8n de la densitat, no d'altres camps, \u00E9s a dir:. Una atmosfera barotr\u00F2pica \u00E9s aquella atmosfera en la qual la pressi\u00F3 dep\u00E8n tan sols en la densitat i viceversa.En general, qualsevol fluid isoentr\u00F2pic o isoterm ser\u00E0 un barotr\u00F2pic. Aix\u00F2 succeeix a l'atmosfera terrestre en els tr\u00F2pics, ja que all\u00E0 les difer\u00E8ncies de temperatura entre una zona i una altra al mateix nivell s\u00F3n petites. El contrari d'una atmosfera barotr\u00F2pica \u00E9s una atmosfera . Un flux barotr\u00F2pic \u00E9s una generalitzaci\u00F3 d'una atmosfera barotr\u00F2pica: es tracta d'un flux en el qual la pressi\u00F3 \u00E9s una funci\u00F3 de la densitat i vice versa. \u00C9s a dir, \u00E9s un flux en el qual les superf\u00EDcies isob\u00E0riques s\u00F3n superf\u00EDcies isop\u00EDcniques i a l'inrev\u00E9s. Es pot donar el cas d'un flux barotr\u00F2pic amb un fluid no barotr\u00F2pic, per\u00F2 un fluid barotr\u00F2pic ha de seguir sempre un flux barotr\u00F2pic. Exemples inclourien les capes barotr\u00F2piques dels oceans, un gas ideal isotermal o un gas ideal isentr\u00F2pic. Els fluids barotr\u00F2pics s\u00F3n tamb\u00E9 fluids idealitzats importants en astrof\u00EDsica, com l'estudi de l'interior estel\u00B7lar o del medi interestel\u00B7lar."@ca . "\u6B63\u58D3\u5927\u6C23"@zh . . "\u0411\u0430\u0440\u043E\u0442\u0440\u043E\u043F\u043D\u0430 \u0440\u0456\u0434\u0438\u043D\u0430"@uk . . . . . "Barotropie"@de . . . "1614121"^^ . "P\u0142yn barotropowy - p\u0142yn, kt\u00F3rego g\u0119sto\u015B\u0107 jest sta\u0142a lub zale\u017Cna tylko od ci\u015Bnienia. Przybli\u017Cenie p\u0142ynu barotropowego jest u\u017Cywane w fizyce atmosfery, oceanografii czy te\u017C w astrofizyce. P\u0142yn niespe\u0142niaj\u0105cy warunku barotropowo\u015Bci nazywa si\u0119 p\u0142ynem baroklinowym. G\u0119sto\u015B\u0107 wielu cieczy, dla przyk\u0142adu wody jest prawie sta\u0142a i stosunkowo nieznacznie zale\u017Cy od temperatury i zasolenia. G\u0119sto\u015B\u0107 gaz\u00F3w w tym i powietrza, og\u00F3lnie nie spe\u0142nia warunk\u00F3w barotropowo\u015Bci, ale je\u017Celi powierzchnie o jednakowej temperaturze s\u0105 r\u00F3wnoleg\u0142e do powierzchni o jednakowym ci\u015Bnieniu, to atmosfera jest barotropowa. W wielu rodzajach przep\u0142yw\u00F3w za\u0142o\u017Cenie to jest spe\u0142nione lub przyjmowane jako za\u0142o\u017Cenie modelu. Przyk\u0142adem jest zastosowanie zasady wirowo\u015Bci potencjalnej w przybli\u017Ceniu barotropowym opisuj\u0105cym fale Rossby\u2019ego w atmosferze."@pl . "Barotrop\u00EDa"@es . "In fluid dynamics, a barotropic fluid is a fluid whose density is a function of pressure only. The barotropic fluid is a useful model of fluid behavior in a wide variety of scientific fields, from meteorology to astrophysics. The density of most liquids is nearly constant (isopycnic), so it can be stated that their densities vary only weakly with pressure and temperature. Water, which varies only a few percent with temperature and salinity, may be approximated as barotropic. In general, air is not barotropic, as it is a function of temperature and pressure; but, under certain circumstances, the barotropic assumption can be useful. In astrophysics, barotropic fluids are important in the study of stellar interiors or of the interstellar medium. One common class of barotropic model used in astrophysics is a polytropic fluid. Typically, the barotropic assumption is not very realistic. In meteorology, a barotropic atmosphere is one that for which the density of the air depends only on pressure, as a result isobaric surfaces (constant-pressure surfaces) are also constant-density surfaces. Such isobaric surfaces will also be isothermal surfaces, hence (from the thermal wind equation) the geostrophic wind will not vary with depth. Hence, the motions of a rotating barotropic air mass is strongly constrained. The tropics are more nearly barotropic than mid-latitudes because temperature is more nearly horizontally uniform in the tropics. A barotropic flow is a generalization of a barotropic atmosphere. It is a flow in which the pressure is a function of the density only and vice versa. In other words, it is a flow in which isobaric surfaces are isopycnic surfaces and vice versa. One may have a barotropic flow of a non-barotropic fluid, but a barotropic fluid will always follow a barotropic flow. Examples include barotropic layers of the oceans, an isothermal ideal gas or an isentropic ideal gas. A fluid which is not barotropic is baroclinic, i. e., pressure is not the only factor to determine density. For a barotropic fluid or a barotropic flow (such as a barotropic atmosphere), the baroclinic vector is zero."@en .