. . . . "\u0422\u0435\u0440\u043C\u0430\u043B\u044C\u043D\u0438\u0439 \u0432\u0456\u0442\u0435\u0440 \u2014 \u0432\u0435\u0440\u0442\u0438\u043A\u0430\u043B\u044C\u043D\u0438\u0439 \u0433\u0440\u0430\u0434\u0456\u0454\u043D\u0442 \u0433\u0435\u043E\u0441\u0442\u0440\u043E\u0444\u0456\u0447\u043D\u043E\u0433\u043E \u0432\u0456\u0442\u0440\u0443, \u0432\u0438\u043A\u043B\u0438\u043A\u0430\u043D\u0438\u0439 \u0433\u043E\u0440\u0438\u0437\u043E\u043D\u0442\u0430\u043B\u044C\u043D\u0438\u043C \u0433\u0440\u0430\u0434\u0456\u0454\u043D\u0442\u043E\u043C \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u0438 \u0430\u0442\u043C\u043E\u0441\u0444\u0435\u0440\u0438. \u0422\u0435\u0440\u043C\u0430\u043B\u044C\u043D\u0438\u0439 \u0432\u0456\u0442\u0435\u0440 \u0444\u0430\u043A\u0442\u0438\u0447\u043D\u043E \u0454 \u043D\u0435 \u0432\u0456\u0442\u0440\u043E\u043C, \u0430 \u0433\u0440\u0430\u0434\u0456\u0454\u043D\u0442\u043E\u043C \u0432\u0456\u0442\u0440\u0443."@uk . . . . . "The thermal wind is the vector difference between the geostrophic wind at upper altitudes minus that at lower altitudes in the atmosphere. It is the hypothetical vertical wind shear that would exist if the winds obey geostrophic balance in the horizontal, while pressure obeys hydrostatic balance in the vertical. The combination of these two force balances is called thermal wind balance, a term generalizable also to more complicated horizontal flow balances such as gradient wind balance. Since the geostrophic wind at a given pressure level flows along geopotential height contours on a map, and the geopotential thickness of a pressure layer is proportional to virtual temperature, it follows that the thermal wind flows along thickness or temperature contours. For instance, the thermal wind associated with pole-to-equator temperature gradients is the primary physical explanation for the jet stream in the upper half of the troposphere, which is the atmospheric layer extending from the surface of the planet up to altitudes of about 12\u201315 km. Mathematically, the thermal wind relation defines a vertical wind shear \u2013 a variation in wind speed or direction with height. The wind shear in this case is a function of a horizontal temperature gradient, which is a variation in temperature over some horizontal distance. Also called baroclinic flow, the thermal wind varies with height in proportion to the horizontal temperature gradient. The thermal wind relation results from hydrostatic balance and geostrophic balance in the presence of a temperature gradient along constant pressure surfaces, or isobars. The term thermal wind is often considered a misnomer, since it really describes the change in wind with height, rather than the wind itself. However, one can view the thermal wind as a geostrophic wind that varies with height, so that the term wind seems appropriate. In the early years of meteorology, when data was scarce, the wind field could be estimated using the thermal wind relation and knowledge of a surface wind speed and direction as well as thermodynamic soundings aloft. In this way, the thermal wind relation acts to define the wind itself, rather than just its shear. Many authors retain the thermal wind moniker, even though it describes a wind gradient, sometimes offering a clarification to that effect."@en . . "Vento t\u00E9rmico"@pt . . . "Vento termico"@it . . . . "Wiatr termiczny"@pl . . . . . . . "Termisk vind \u00E4r en vind som g\u00E5r mellan omr\u00E5den i atmosf\u00E4ren med . Den existerar bara i atmosf\u00E4rer med horisontella temperaturgradienter, det vill s\u00E4ga baroklinitet. I en barotropisk atmosf\u00E4r \u00E4r den geotrofiska vinden oberoende av h\u00F6jd. Som namnet antyder bl\u00E5ser en geotermisk vind kring omr\u00E5den med l\u00E5g respektive h\u00F6g temperatur p\u00E5 samma vis som en geostrofisk vind bl\u00E5ser kring omr\u00E5den med l\u00E5gt respektive h\u00F6gt tryck."@sv . . . . . . . . . . . . . "Wiatr termiczny \u2013 r\u00F3\u017Cnica wektor\u00F3w pr\u0119dko\u015Bci wiatr\u00F3w geostroficznych mi\u0119dzy dwoma poziomami ci\u015Bnienia (wysoko\u015Bci) wynikaj\u0105ca z poziomej r\u00F3\u017Cnicy temperatury powietrza. Nie jest to faktyczny wiatr, ale jest to u\u017Cyteczna konstrukcja, kt\u00F3ra pozwala wyznaczy\u0107 w przestrzeni w kt\u00F3rej zachodz\u0105 poziome zmiany ci\u015Bnienia i temperatury."@pl . . . . . "Thermal wind"@en . "Le vent thermique est un concept pratique en m\u00E9t\u00E9orologie pour calculer la variation du vent entre deux altitudes quand on conna\u00EEt la structure thermique de la masse d'air."@fr . . . "11258"^^ . . . "\u6E29\u5EA6\u98A8"@ja . . . . . "\u0422\u0435\u0440\u043C\u0438\u0447\u0435\u0441\u043A\u0438\u0439 \u0432\u0435\u0442\u0435\u0440 \u0438\u043B\u0438 \u0442\u0435\u0440\u043C\u0438\u0447\u0435\u0441\u043A\u0430\u044F \u0441\u043E\u0441\u0442\u0430\u0432\u043B\u044F\u044E\u0449\u0430\u044F \u0432\u0435\u0442\u0440\u0430 \u2014 \u0432\u0435\u043A\u0442\u043E\u0440\u043D\u044B\u0439 \u0441\u0434\u0432\u0438\u0433 \u0433\u0435\u043E\u0441\u0442\u0440\u043E\u0444\u0438\u0447\u0435\u0441\u043A\u043E\u0433\u043E \u0432\u0435\u0442\u0440\u0430 \u043F\u043E \u0432\u0435\u0440\u0442\u0438\u043A\u0430\u043B\u0438 \u043E\u0442 \u043E\u0434\u043D\u043E\u0433\u043E \u0433\u043E\u0440\u0438\u0437\u043E\u043D\u0442\u0430\u043B\u044C\u043D\u043E\u0433\u043E \u0441\u043B\u043E\u044F \u043A \u0434\u0440\u0443\u0433\u043E\u043C\u0443, \u043A\u043E\u0442\u043E\u0440\u044B\u0439 \u043E\u043F\u0440\u0435\u0434\u0435\u043B\u044F\u0435\u0442\u0441\u044F \u0443\u0441\u0440\u0435\u0434\u043D\u0451\u043D\u043D\u044B\u043C \u0437\u043D\u0430\u0447\u0435\u043D\u0438\u0435\u043C \u0433\u0440\u0430\u0434\u0438\u0435\u043D\u0442\u0430 \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u044B \u043C\u0435\u0436\u0434\u0443 \u044D\u0442\u0438\u043C\u0438 \u0432\u044B\u0441\u043E\u0442\u0430\u043C\u0438."@ru . . . "\u0422\u0435\u0440\u043C\u0430\u043B\u044C\u043D\u0438\u0439 \u0432\u0456\u0442\u0435\u0440 \u2014 \u0432\u0435\u0440\u0442\u0438\u043A\u0430\u043B\u044C\u043D\u0438\u0439 \u0433\u0440\u0430\u0434\u0456\u0454\u043D\u0442 \u0433\u0435\u043E\u0441\u0442\u0440\u043E\u0444\u0456\u0447\u043D\u043E\u0433\u043E \u0432\u0456\u0442\u0440\u0443, \u0432\u0438\u043A\u043B\u0438\u043A\u0430\u043D\u0438\u0439 \u0433\u043E\u0440\u0438\u0437\u043E\u043D\u0442\u0430\u043B\u044C\u043D\u0438\u043C \u0433\u0440\u0430\u0434\u0456\u0454\u043D\u0442\u043E\u043C \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u0438 \u0430\u0442\u043C\u043E\u0441\u0444\u0435\u0440\u0438. \u0422\u0435\u0440\u043C\u0430\u043B\u044C\u043D\u0438\u0439 \u0432\u0456\u0442\u0435\u0440 \u0444\u0430\u043A\u0442\u0438\u0447\u043D\u043E \u0454 \u043D\u0435 \u0432\u0456\u0442\u0440\u043E\u043C, \u0430 \u0433\u0440\u0430\u0434\u0456\u0454\u043D\u0442\u043E\u043C \u0432\u0456\u0442\u0440\u0443."@uk . . . "1593644"^^ . . . . "\uC628\uB3C4\uD48D(\u6E29\u5EA6\u98A8, thermal wind)\uC740 \uB300\uAE30\uC758 \uC628\uB3C4\uCC28\uB97C \uC6D0\uC778\uC73C\uB85C \uD558\uC5EC \uBC1C\uC0DD\uD558\uB294, \uACE0\uB3C4\uAC00 \uC11C\uB85C \uB2E4\uB978 \uB450 \uC810 \uC0AC\uC774\uC758 \uBC14\uB78C\uC758 \uC18D\uB3C4\uBCA1\uD130 \uCC28\uC774\uC774\uB2E4. \uC5B4\uB514\uAE4C\uC9C0\uB098 \"\uCC28\uC774\"\uC774\uBA70, \uADF8\uB7F0 \uBC14\uB78C\uC774 \uC2E4\uC81C\uB85C \uBD88\uACE0 \uC788\uB294 \uAC83\uC740 \uC544\uB2C8\uB2E4. \uAE30\uC555\uC774 \uC77C\uC815\uD558\uC9C0\uB9CC \uAE30\uC628\uC740 \uADE0\uC77C\uD558\uC9C0 \uC54A\uC740 \uD3C9\uBA74\uC744 \uC0DD\uAC01\uD55C\uB2E4. \uAE30\uC555\uC774 \uADE0\uC77C\uD558\uBBC0\uB85C \uC774 \uC791\uC6A9\uD558\uC9C0 \uC54A\uACE0, \uC774 \uD3C9\uBA74\uC0C1\uC5D0\uC11C \uBC14\uB78C\uC740 \uBD88\uC9C0 \uC54A\uB294\uB2E4. \uD55C\uD3B8, \uC815\uC5ED\uD559\uC801 \uD3C9\uD615 \uAD00\uACC4\uC2DD\uC5D0 \uC758\uD574 \uACE0\uB3C4\uAC00 \uC62C\uB77C\uAC08 \uB54C\uB9C8\uB2E4 \uAE30\uC555\uC774 \uAC10\uC18C\uD558\uB294 \uC815\uB3C4\uB294 \uAE30\uC628\uC774 \uB0AE\uC740 \uACF3\uC5D0\uC11C \uB354 \uD06C\uB2E4. \uB530\uB77C\uC11C \uADF8 \uD3C9\uBA74 \uC0C1\uACF5\uC5D0\uC11C\uB294 \uAE30\uC628\uC774 \uB192\uC740 \uACF3\uC758 \uC0C1\uACF5\uC774 \uACE0\uAE30\uC555, \uAE30\uC628\uC774 \uB0AE\uC740 \uACF3\uC758 \uC0C1\uACF5\uC774 \uC800\uAE30\uC555\uC774 \uB41C\uB2E4. \uD558\uC5EC \uC9C0\uD45C\uC5D0\uC11C \uBD80\uB294 \uBC14\uB78C\uACFC \uBCC4\uAC1C\uB85C \uC0C1\uACF5\uC5D0\uC11C \uBD80\uB294 \uBC14\uB78C\uC774 \uC788\uB294\uB370, \uD55C \uC9C0\uC810\uC758 \uC0C1\uACF5 \uBC14\uB78C \uBCA1\uD130\uC5D0\uC11C \uC9C0\uD45C \uBC14\uB78C \uBCA1\uD130\uB97C \uBE7C\uBA74 \uADF8\uAC83\uC774 \uC628\uB3C4\uD48D \uBCA1\uD130\uAC00 \uB418\uACE0, \uADF8 \uBC29\uD5A5\uC740 \uB4F1\uC628\uC120\uACFC \uD3C9\uD589\uD558\uB2E4. \uD3C9\uBA74\uC0C1\uC758 \uAE30\uC555\uC774 \uC77C\uC815\uCE58 \uC54A\uACE0 \uD3C9\uBA74\uC0C1\uC5D0\uB3C4 \uBC14\uB78C\uC774 \uBD88 \uACBD\uC6B0 \uADF8 \uC0C1\uACF5\uC758 \uBC14\uB78C\uC740 \uC628\uB3C4\uD48D\uACFC \uD3C9\uBA74\uC0C1\uC758 \uBC14\uB78C\uC758 \uC131\uBD84\uC744 \uD569\uD55C \uAC83\uC774 \uB41C\uB2E4. \uBC18\uB300\uB85C \uC0C1\uACF5\uC758 \uBC14\uB78C\uC5D0\uC11C \uD3C9\uBA74\uC0C1\uC758 \uBC14\uB78C\uC744 \uBE7C\uBA74 \uC628\uB3C4\uD48D\uC774 \uB41C\uB2E4. \uB300\uB958\uAD8C\uC5D0\uC11C\uB294 \uC801\uB3C4 \uBD80\uADFC\uC774 \uAC00\uC7A5 \uAE30\uC628\uC774 \uB192\uACE0, \uC591\uADF9\uC73C\uB85C \uAC08\uC218\uB85D \uAE30\uC628\uC774 \uB0B4\uB824\uAC04\uB2E4. \uB530\uB77C\uC11C \uC628\uB3C4\uD48D\uC740 \uC11C\uD48D\uC73C\uB85C \uBD84\uB2E4. \uACE0\uB3C4\uAC00 \uB192\uC544\uC9C8\uC218\uB85D \uC11C\uD48D\uC774 \uAC15\uD574\uC9C0\uACE0, \uB300\uB958\uAD8C\uACC4\uBA74 \uBD80\uADFC\uC5D0\uC11C \uAC00\uC7A5 \uAC15\uD574\uC9C4\uB2E4."@ko . . . . . . . "Il vento termico non \u00E8 un vero e proprio vento quanto una differenza tra vettori del vento geostrofico tra due diverse e , con . \u00C8 presente solo in atmosfera con gradienti orizzontali di temperatura. In un'atmosfera (la cui pressione dipende cio\u00E8 dalla sola densit\u00E0) il vento geostrofico \u00E8 indipendente dall'altezza. Il nome di vento termico \u00E8 dovuto al fatto che si muove intorno a zone di bassa (ed alta) temperatura nello stesso modo in cui il vento geostrofico ruota intorno a zone di bassa (o alta) pressione.L'equazione del vento termico \u00E8:"@it . "1066545353"^^ . "El viento t\u00E9rmico no es un viento real sino m\u00E1s bien un concepto pr\u00E1ctico usado en meteorolog\u00EDa para calcular la variaci\u00F3n del viento entre dos alturas cuando se conoce la estructura t\u00E9rmica de la masa de aire."@es . "\u6E29\u5EA6\u98A8\uFF08\u304A\u3093\u3069\u3075\u3046\uFF09\u3068\u306F\u5927\u6C17\u5185\u306E\u6E29\u5EA6\u5DEE\u3092\u539F\u56E0\u3068\u3057\u3066\u751F\u3058\u308B\u3001\u9AD8\u5EA6\u306E\u7570\u306A\u308B2\u70B9\u3067\u306E\u98A8\u306E\u901F\u5EA6\u30D9\u30AF\u30C8\u30EB\u306E\u5DEE\u306E\u3053\u3068\u3067\u3042\u308B\u3002\u3042\u304F\u307E\u3067\u5DEE\u306E\u3053\u3068\u3067\u3042\u308A\u3001\u5B9F\u969B\u306B\u305D\u306E\u3088\u3046\u306A\u98A8\u304C\u5439\u3044\u3066\u3044\u308B\u308F\u3051\u3067\u306F\u306A\u3044\u3002"@ja . . "Vent thermique"@fr . . . "The thermal wind is the vector difference between the geostrophic wind at upper altitudes minus that at lower altitudes in the atmosphere. It is the hypothetical vertical wind shear that would exist if the winds obey geostrophic balance in the horizontal, while pressure obeys hydrostatic balance in the vertical. The combination of these two force balances is called thermal wind balance, a term generalizable also to more complicated horizontal flow balances such as gradient wind balance."@en . "Il vento termico non \u00E8 un vero e proprio vento quanto una differenza tra vettori del vento geostrofico tra due diverse e , con . \u00C8 presente solo in atmosfera con gradienti orizzontali di temperatura. In un'atmosfera (la cui pressione dipende cio\u00E8 dalla sola densit\u00E0) il vento geostrofico \u00E8 indipendente dall'altezza. Il nome di vento termico \u00E8 dovuto al fatto che si muove intorno a zone di bassa (ed alta) temperatura nello stesso modo in cui il vento geostrofico ruota intorno a zone di bassa (o alta) pressione.L'equazione del vento termico \u00E8: dove sono le altezze di geopotenziale con , \u00E8 il parametro di Coriolis e \u00E8 il versore verticale. L'equazione del vento termico non ha molto significato nelle zone tropicali poich\u00E9, essendo il parametro di Coriolis molto piccolo o nullo, l'unico risultato sarebbe che \u00E8 piccolo."@it . . . "Termisk vind \u00E4r en vind som g\u00E5r mellan omr\u00E5den i atmosf\u00E4ren med . Den existerar bara i atmosf\u00E4rer med horisontella temperaturgradienter, det vill s\u00E4ga baroklinitet. I en barotropisk atmosf\u00E4r \u00E4r den geotrofiska vinden oberoende av h\u00F6jd. Som namnet antyder bl\u00E5ser en geotermisk vind kring omr\u00E5den med l\u00E5g respektive h\u00F6g temperatur p\u00E5 samma vis som en geostrofisk vind bl\u00E5ser kring omr\u00E5den med l\u00E5gt respektive h\u00F6gt tryck."@sv . "Vent t\u00E8rmic"@ca . . . "El viento t\u00E9rmico no es un viento real sino m\u00E1s bien un concepto pr\u00E1ctico usado en meteorolog\u00EDa para calcular la variaci\u00F3n del viento entre dos alturas cuando se conoce la estructura t\u00E9rmica de la masa de aire. Cuando existen diferencias de temperatura en horizontal (atm\u00F3sfera baroclina) el viento geostr\u00F3fico var\u00EDa con la altura. Podemos considerar que el viento geostr\u00F3fico en altura es entonces la suma del viento geostr\u00F3fico en la base m\u00E1s un t\u00E9rmino al que se llama viento t\u00E9rmico. El viento t\u00E9rmico es paralelo a las isotermas. En el hemisferio norte deja el aire fr\u00EDo a su izquierda y el c\u00E1lido a su derecha, mientras que en el hemisferio sur sucede al rev\u00E9s."@es . . . . "\uC628\uB3C4\uD48D"@ko . . "Termisk vind"@sv . "\u0422\u0435\u0440\u043C\u0438\u0447\u0435\u0441\u043A\u0438\u0439 \u0432\u0435\u0442\u0435\u0440"@ru . . . . . "Wiatr termiczny \u2013 r\u00F3\u017Cnica wektor\u00F3w pr\u0119dko\u015Bci wiatr\u00F3w geostroficznych mi\u0119dzy dwoma poziomami ci\u015Bnienia (wysoko\u015Bci) wynikaj\u0105ca z poziomej r\u00F3\u017Cnicy temperatury powietrza. Nie jest to faktyczny wiatr, ale jest to u\u017Cyteczna konstrukcja, kt\u00F3ra pozwala wyznaczy\u0107 w przestrzeni w kt\u00F3rej zachodz\u0105 poziome zmiany ci\u015Bnienia i temperatury."@pl . . "\u6E29\u5EA6\u98A8\uFF08\u304A\u3093\u3069\u3075\u3046\uFF09\u3068\u306F\u5927\u6C17\u5185\u306E\u6E29\u5EA6\u5DEE\u3092\u539F\u56E0\u3068\u3057\u3066\u751F\u3058\u308B\u3001\u9AD8\u5EA6\u306E\u7570\u306A\u308B2\u70B9\u3067\u306E\u98A8\u306E\u901F\u5EA6\u30D9\u30AF\u30C8\u30EB\u306E\u5DEE\u306E\u3053\u3068\u3067\u3042\u308B\u3002\u3042\u304F\u307E\u3067\u5DEE\u306E\u3053\u3068\u3067\u3042\u308A\u3001\u5B9F\u969B\u306B\u305D\u306E\u3088\u3046\u306A\u98A8\u304C\u5439\u3044\u3066\u3044\u308B\u308F\u3051\u3067\u306F\u306A\u3044\u3002"@ja . "El vent t\u00E8rmic \u00E9s un cisallament vertical dins del vent geostr\u00F2fic causat per un gradient de temperatura horitzontal. En realitat no \u00E9s un vent pr\u00F2piament dit. El vent t\u00E8rmic \u00E9s un concepte que es fa servir per calcular la variaci\u00F3 del vent entre dues altures quan es coneix l'estructura t\u00E8rmica de la massa d'aire."@ca . . . . "\uC628\uB3C4\uD48D(\u6E29\u5EA6\u98A8, thermal wind)\uC740 \uB300\uAE30\uC758 \uC628\uB3C4\uCC28\uB97C \uC6D0\uC778\uC73C\uB85C \uD558\uC5EC \uBC1C\uC0DD\uD558\uB294, \uACE0\uB3C4\uAC00 \uC11C\uB85C \uB2E4\uB978 \uB450 \uC810 \uC0AC\uC774\uC758 \uBC14\uB78C\uC758 \uC18D\uB3C4\uBCA1\uD130 \uCC28\uC774\uC774\uB2E4. \uC5B4\uB514\uAE4C\uC9C0\uB098 \"\uCC28\uC774\"\uC774\uBA70, \uADF8\uB7F0 \uBC14\uB78C\uC774 \uC2E4\uC81C\uB85C \uBD88\uACE0 \uC788\uB294 \uAC83\uC740 \uC544\uB2C8\uB2E4. \uAE30\uC555\uC774 \uC77C\uC815\uD558\uC9C0\uB9CC \uAE30\uC628\uC740 \uADE0\uC77C\uD558\uC9C0 \uC54A\uC740 \uD3C9\uBA74\uC744 \uC0DD\uAC01\uD55C\uB2E4. \uAE30\uC555\uC774 \uADE0\uC77C\uD558\uBBC0\uB85C \uC774 \uC791\uC6A9\uD558\uC9C0 \uC54A\uACE0, \uC774 \uD3C9\uBA74\uC0C1\uC5D0\uC11C \uBC14\uB78C\uC740 \uBD88\uC9C0 \uC54A\uB294\uB2E4. \uD55C\uD3B8, \uC815\uC5ED\uD559\uC801 \uD3C9\uD615 \uAD00\uACC4\uC2DD\uC5D0 \uC758\uD574 \uACE0\uB3C4\uAC00 \uC62C\uB77C\uAC08 \uB54C\uB9C8\uB2E4 \uAE30\uC555\uC774 \uAC10\uC18C\uD558\uB294 \uC815\uB3C4\uB294 \uAE30\uC628\uC774 \uB0AE\uC740 \uACF3\uC5D0\uC11C \uB354 \uD06C\uB2E4. \uB530\uB77C\uC11C \uADF8 \uD3C9\uBA74 \uC0C1\uACF5\uC5D0\uC11C\uB294 \uAE30\uC628\uC774 \uB192\uC740 \uACF3\uC758 \uC0C1\uACF5\uC774 \uACE0\uAE30\uC555, \uAE30\uC628\uC774 \uB0AE\uC740 \uACF3\uC758 \uC0C1\uACF5\uC774 \uC800\uAE30\uC555\uC774 \uB41C\uB2E4. \uD558\uC5EC \uC9C0\uD45C\uC5D0\uC11C \uBD80\uB294 \uBC14\uB78C\uACFC \uBCC4\uAC1C\uB85C \uC0C1\uACF5\uC5D0\uC11C \uBD80\uB294 \uBC14\uB78C\uC774 \uC788\uB294\uB370, \uD55C \uC9C0\uC810\uC758 \uC0C1\uACF5 \uBC14\uB78C \uBCA1\uD130\uC5D0\uC11C \uC9C0\uD45C \uBC14\uB78C \uBCA1\uD130\uB97C \uBE7C\uBA74 \uADF8\uAC83\uC774 \uC628\uB3C4\uD48D \uBCA1\uD130\uAC00 \uB418\uACE0, \uADF8 \uBC29\uD5A5\uC740 \uB4F1\uC628\uC120\uACFC \uD3C9\uD589\uD558\uB2E4."@ko . . . . "\u70ED\u6210\u98CE"@zh . . . "El vent t\u00E8rmic \u00E9s un cisallament vertical dins del vent geostr\u00F2fic causat per un gradient de temperatura horitzontal. En realitat no \u00E9s un vent pr\u00F2piament dit. El vent t\u00E8rmic \u00E9s un concepte que es fa servir per calcular la variaci\u00F3 del vent entre dues altures quan es coneix l'estructura t\u00E8rmica de la massa d'aire. Quan hi ha difer\u00E8ncies de temperatura en horitzontal (atmosfera baroclina) el vent geostr\u00F2fic varia amb l'altitud. Es pot considerar aleshores que el vent geostr\u00F2fic en altura \u00E9s la suma del vent geostr\u00F2fic en la base m\u00E9s el terme que es coneix com a vent t\u00E8rmic. El vent t\u00E8rmic \u00E9s paral\u00B7lel a les isotermes. En l'hemisferi nord deixa l'aire fred a la seva esquerra i el c\u00E0lid a la seva dreta, en l'hemisferi sud \u00E9s a l'inrev\u00E9s."@ca . "Viento t\u00E9rmico"@es . "\u0422\u0435\u0440\u043C\u0430\u043B\u044C\u043D\u0438\u0439 \u0432\u0456\u0442\u0435\u0440"@uk . "Vento t\u00E9rmico n\u00E3o \u00E9 um vento real, mas sim um conceito pr\u00E1tico usado em meteorologia para calcular a varia\u00E7\u00E3o do vento entre dois n\u00EDveis relativos \u00E0 estrutura t\u00E9rmica da massa de ar. Quando existem diferen\u00E7as de temperatura horizontal (atmosfera baroclinia), o vento geostr\u00F3fico varia de acordo com a altura. Podemos portanto considerar que o vento geostr\u00F3fico em altura \u00E9 a soma do vento geostr\u00F3fico na base acrescido de um termo designado de vento t\u00E9rmico. O vento t\u00E9rmico \u00E9 paralelo \u00E0s linhas . No hemisf\u00E9rio norte o ar frio \u00E9 move-se para a esquerda enquanto que o quente situa a direita. J\u00E1 no hemisf\u00E9rio sul esta din\u00E2mica revela-se o oposto."@pt . "\u0422\u0435\u0440\u043C\u0438\u0447\u0435\u0441\u043A\u0438\u0439 \u0432\u0435\u0442\u0435\u0440 \u0438\u043B\u0438 \u0442\u0435\u0440\u043C\u0438\u0447\u0435\u0441\u043A\u0430\u044F \u0441\u043E\u0441\u0442\u0430\u0432\u043B\u044F\u044E\u0449\u0430\u044F \u0432\u0435\u0442\u0440\u0430 \u2014 \u0432\u0435\u043A\u0442\u043E\u0440\u043D\u044B\u0439 \u0441\u0434\u0432\u0438\u0433 \u0433\u0435\u043E\u0441\u0442\u0440\u043E\u0444\u0438\u0447\u0435\u0441\u043A\u043E\u0433\u043E \u0432\u0435\u0442\u0440\u0430 \u043F\u043E \u0432\u0435\u0440\u0442\u0438\u043A\u0430\u043B\u0438 \u043E\u0442 \u043E\u0434\u043D\u043E\u0433\u043E \u0433\u043E\u0440\u0438\u0437\u043E\u043D\u0442\u0430\u043B\u044C\u043D\u043E\u0433\u043E \u0441\u043B\u043E\u044F \u043A \u0434\u0440\u0443\u0433\u043E\u043C\u0443, \u043A\u043E\u0442\u043E\u0440\u044B\u0439 \u043E\u043F\u0440\u0435\u0434\u0435\u043B\u044F\u0435\u0442\u0441\u044F \u0443\u0441\u0440\u0435\u0434\u043D\u0451\u043D\u043D\u044B\u043C \u0437\u043D\u0430\u0447\u0435\u043D\u0438\u0435\u043C \u0433\u0440\u0430\u0434\u0438\u0435\u043D\u0442\u0430 \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u044B \u043C\u0435\u0436\u0434\u0443 \u044D\u0442\u0438\u043C\u0438 \u0432\u044B\u0441\u043E\u0442\u0430\u043C\u0438."@ru . . . . "Vento t\u00E9rmico n\u00E3o \u00E9 um vento real, mas sim um conceito pr\u00E1tico usado em meteorologia para calcular a varia\u00E7\u00E3o do vento entre dois n\u00EDveis relativos \u00E0 estrutura t\u00E9rmica da massa de ar. Quando existem diferen\u00E7as de temperatura horizontal (atmosfera baroclinia), o vento geostr\u00F3fico varia de acordo com a altura. Podemos portanto considerar que o vento geostr\u00F3fico em altura \u00E9 a soma do vento geostr\u00F3fico na base acrescido de um termo designado de vento t\u00E9rmico. O vento t\u00E9rmico \u00E9 paralelo \u00E0s linhas . No hemisf\u00E9rio norte o ar frio \u00E9 move-se para a esquerda enquanto que o quente situa a direita. J\u00E1 no hemisf\u00E9rio sul esta din\u00E2mica revela-se o oposto."@pt . . "Le vent thermique est un concept pratique en m\u00E9t\u00E9orologie pour calculer la variation du vent entre deux altitudes quand on conna\u00EEt la structure thermique de la masse d'air."@fr .