. . "Temperatura potenziale"@it . . . . . . . . . . . "La temperatura potenziale di una particella di fluido alla pressione \u00E8 la temperatura che quella particella avrebbe se fosse portata, tramite uno spostamento adiabatico, ad una pressione standard di riferimento , in genere 1 bar. La temperatura potenziale si indica solitamente con e, per l'aria, \u00E8 espressa da: dove T \u00E8 la temperatura assoluta della particella, R la costante dei gas per l'aria e il calore specifico a pressione costante. Il concetto di temperatura potenziale si applica a qualsiasi fluido stratificato ed \u00E8 usato principalmente nelle scienze atmosferiche e in oceanografia."@it . "Temperatura potencial"@es . . . "Potenti\u00EBle temperatuur"@nl . "La temperatura potencial es una variable termodin\u00E1mica ampliamente utilizada en meteorolog\u00EDa que representa la temperatura que una parcela de aire seco, a una presi\u00F3n p y temperatura T (en Kelvin), tendr\u00EDa si fuera comprimida o expandida adiab\u00E1ticamente hasta una presi\u00F3n de referencia po (normalmente 1000 mb). Formalmente se define como La importancia de la temperatura potencial es que se trata de una variable conservada bajo procesos adiab\u00E1ticos."@es . . "\u041F\u043E\u0442\u0435\u043D\u0446\u0438\u0430\u043B\u044C\u043D\u0430\u044F \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u0430 \u2014 \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u0430 \u0433\u0430\u0437\u0430, \u043F\u0440\u0438\u0432\u0435\u0434\u0451\u043D\u043D\u043E\u0433\u043E \u0430\u0434\u0438\u0430\u0431\u0430\u0442\u0438\u0447\u0435\u0441\u043A\u0438 \u043A \u0441\u0442\u0430\u043D\u0434\u0430\u0440\u0442\u043D\u043E\u043C\u0443 \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u044E, \u043E\u0431\u044B\u0447\u043D\u043E 105 \u041F\u0430. \u041E\u0431\u043E\u0437\u043D\u0430\u0447\u0430\u0435\u0442\u0441\u044F \u0433\u0440\u0435\u0447\u0435\u0441\u043A\u043E\u0439 \u0431\u0443\u043A\u0432\u043E\u0439 \u0438 \u0432\u044B\u0440\u0430\u0436\u0430\u0435\u0442\u0441\u044F \u0447\u0435\u0440\u0435\u0437 \u0441\u043B\u0435\u0434\u0443\u044E\u0449\u0435\u0435 \u0443\u0440\u0430\u0432\u043D\u0435\u043D\u0438\u0435, \u043D\u0430\u0437\u044B\u0432\u0430\u0435\u043C\u043E\u0435 \u0442\u0430\u043A\u0436\u0435 \u0443\u0440\u0430\u0432\u043D\u0435\u043D\u0438\u0435\u043C \u041F\u0443\u0430\u0441\u0441\u043E\u043D\u0430: \u0433\u0434\u0435 \u2014 \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u0430 \u0432 \u043A\u0435\u043B\u044C\u0432\u0438\u043D\u0430\u0445, \u2014 \u0433\u0430\u0437\u043E\u0432\u0430\u044F \u043F\u043E\u0441\u0442\u043E\u044F\u043D\u043D\u0430\u044F \u0438 \u2014 \u0443\u0434\u0435\u043B\u044C\u043D\u0430\u044F \u0442\u0435\u043F\u043B\u043E\u0451\u043C\u043A\u043E\u0441\u0442\u044C \u0432 \u0438\u0437\u043E\u0431\u0430\u0440\u043D\u043E\u043C \u043F\u0440\u043E\u0446\u0435\u0441\u0441\u0435."@ru . . . . "Temperatura potencjalna cz\u0105stki pr\u00F3bnej powietrza o ci\u015Bnieniu i temperaturze \u2013 temperatura, jak\u0105 mia\u0142aby cz\u0105stka, gdyby zosta\u0142a sprowadzona adiabatycznie do ci\u015Bnienia standardowego r\u00F3wnego zazwyczaj 1000 hPa. Temperatura potencjalna jest r\u00F3wnowa\u017Cna poj\u0119ciu entropii powietrza. Jest ona oznaczona i jest zdefiniowana jako gdzie: \u2013 temperatura cz\u0105stki, \u2013 sta\u0142a gazowa, \u2013 ciep\u0142o w\u0142a\u015Bciwe powietrza przy sta\u0142ym ci\u015Bnieniu."@pl . . . "La temperatura potenziale di una particella di fluido alla pressione \u00E8 la temperatura che quella particella avrebbe se fosse portata, tramite uno spostamento adiabatico, ad una pressione standard di riferimento , in genere 1 bar. La temperatura potenziale si indica solitamente con e, per l'aria, \u00E8 espressa da: dove T \u00E8 la temperatura assoluta della particella, R la costante dei gas per l'aria e il calore specifico a pressione costante. Il concetto di temperatura potenziale si applica a qualsiasi fluido stratificato ed \u00E8 usato principalmente nelle scienze atmosferiche e in oceanografia."@it . . . . "Temperatura potencjalna"@pl . . "La temperatura potencial es una variable termodin\u00E1mica ampliamente utilizada en meteorolog\u00EDa que representa la temperatura que una parcela de aire seco, a una presi\u00F3n p y temperatura T (en Kelvin), tendr\u00EDa si fuera comprimida o expandida adiab\u00E1ticamente hasta una presi\u00F3n de referencia po (normalmente 1000 mb). Formalmente se define como La importancia de la temperatura potencial es que se trata de una variable conservada bajo procesos adiab\u00E1ticos."@es . . . . "2082201"^^ . "Temperatura potencjalna cz\u0105stki pr\u00F3bnej powietrza o ci\u015Bnieniu i temperaturze \u2013 temperatura, jak\u0105 mia\u0142aby cz\u0105stka, gdyby zosta\u0142a sprowadzona adiabatycznie do ci\u015Bnienia standardowego r\u00F3wnego zazwyczaj 1000 hPa. Temperatura potencjalna jest r\u00F3wnowa\u017Cna poj\u0119ciu entropii powietrza. Jest ona oznaczona i jest zdefiniowana jako gdzie: \u2013 temperatura cz\u0105stki, \u2013 sta\u0142a gazowa, \u2013 ciep\u0142o w\u0142a\u015Bciwe powietrza przy sta\u0142ym ci\u015Bnieniu."@pl . . "Die Zustandsgr\u00F6\u00DFe potentielle Temperatur \u03B8 ist ein fiktives Temperaturma\u00DF. Sie dient in der Meteorologie und der Meereskunde dazu, die Temperatur von Luft bzw. Wasser unterschiedlicher H\u00F6hen bzw. Tiefen miteinander vergleichbar zu machen, d. h. unterschiedliche Dr\u00FCcke zu ber\u00FCcksichtigen. Die potentielle Temperatur ist ein Ma\u00DF f\u00FCr die Summe aus innerer Energie (\u00F6rtlicher Temperatur) und potentieller Energie (H\u00F6he/Tiefe) und wurde 1888 von Wilhelm von Bezold eingef\u00FChrt."@de . . . . "The potential temperature of a parcel of fluid at pressure is the temperature that the parcel would attain if adiabatically brought to a standard reference pressure , usually 1,000 hPa (1,000 mb). The potential temperature is denoted and, for a gas well-approximated as ideal, is given by where is the current absolute temperature (in K) of the parcel, is the gas constant of air, and is the specific heat capacity at a constant pressure. for air (meteorology). The reference point for potential temperature in the ocean is usually at the ocean's surface which has a water pressure of 0 dbar. The potential temperature in the ocean doesn't account for the varying heat capacities of seawater, therefore it is not a conservative measure of heat content. Graphical representation of potential temperature will always be less than the actual temperature line in a temperature vs depth graph."@en . . "Temperatura potencial"@pt . . . . . "\u6E29\u4F4D"@ja . . "Temp\u00E9rature potentielle"@fr . "\u4F4D\u6E29\u662F\u6307\u6D41\u9AD4\u5F9E\u6C23\u58D3\u70BA \u3001\u6EAB\u5EA6\u70BA \uFF08\u55AE\u4F4D K\uFF09\u7684\u4F4D\u7F6E\u7D55\u71B1\u62AC\u5347\u6216\u4E0B\u964D\u81F3\u53C3\u7167\u6C23\u58D3\u503C \u7684\u4F4D\u7F6E\uFF08\u901A\u5E38\u70BA 1000 hPa\uFF09\u6240\u5177\u6709\u7684\u6EAB\u5EA6\uFF0C\u4E26\u4EE5 \u8868\u793A\u4E4B\u3002\u5C31\u7A7A\u6C23\u800C\u8A00\uFF0C\u5176\u4F4D\u6EAB\u53EF\u5F9E\u4E0B\u5217\u65B9\u7A0B\u5F0F\u6C42\u5F97\uFF1A \u70BA\u6C23\u584A\u7684\u7D55\u5C0D\u6EAB\u5EA6(K)\u3001 \u70BA\u6C23\u9AD4\u5E38\u6578\u3001 \u7B49\u58D3\u6BD4\u71B1\u5BB9\u3002 (\u4E7E\u7A7A\u6C23\u6C23\u9AD4\u5E38\u6578R\u2248287.43JK-1kg-1\uFF1Bcp\u22481005JK-1kg-1)"@zh . "\u4F4D\u6E29\u662F\u6307\u6D41\u9AD4\u5F9E\u6C23\u58D3\u70BA \u3001\u6EAB\u5EA6\u70BA \uFF08\u55AE\u4F4D K\uFF09\u7684\u4F4D\u7F6E\u7D55\u71B1\u62AC\u5347\u6216\u4E0B\u964D\u81F3\u53C3\u7167\u6C23\u58D3\u503C \u7684\u4F4D\u7F6E\uFF08\u901A\u5E38\u70BA 1000 hPa\uFF09\u6240\u5177\u6709\u7684\u6EAB\u5EA6\uFF0C\u4E26\u4EE5 \u8868\u793A\u4E4B\u3002\u5C31\u7A7A\u6C23\u800C\u8A00\uFF0C\u5176\u4F4D\u6EAB\u53EF\u5F9E\u4E0B\u5217\u65B9\u7A0B\u5F0F\u6C42\u5F97\uFF1A \u70BA\u6C23\u584A\u7684\u7D55\u5C0D\u6EAB\u5EA6(K)\u3001 \u70BA\u6C23\u9AD4\u5E38\u6578\u3001 \u7B49\u58D3\u6BD4\u71B1\u5BB9\u3002 (\u4E7E\u7A7A\u6C23\u6C23\u9AD4\u5E38\u6578R\u2248287.43JK-1kg-1\uFF1Bcp\u22481005JK-1kg-1)"@zh . "Temperatura potencial como uma parcela de ar teria se a mesma fosse levada por um escoamento adiab\u00E1tico at\u00E9 a press\u00E3o de refer\u00EAncia igual a 1000 hPa. Um escoamento adiab\u00E1tico \u00E9 aquele que ocorre sem que haja troca de energia com o meio, ou seja, um escoamento que se d\u00E1 conservando a entropia. Sua express\u00E3o matem\u00E1tica \u00E9:"@pt . . . "Die Zustandsgr\u00F6\u00DFe potentielle Temperatur \u03B8 ist ein fiktives Temperaturma\u00DF. Sie dient in der Meteorologie und der Meereskunde dazu, die Temperatur von Luft bzw. Wasser unterschiedlicher H\u00F6hen bzw. Tiefen miteinander vergleichbar zu machen, d. h. unterschiedliche Dr\u00FCcke zu ber\u00FCcksichtigen. Die potentielle Temperatur ist ein Ma\u00DF f\u00FCr die Summe aus innerer Energie (\u00F6rtlicher Temperatur) und potentieller Energie (H\u00F6he/Tiefe) und wurde 1888 von Wilhelm von Bezold eingef\u00FChrt."@de . . . . "\u041F\u043E\u0442\u0435\u043D\u0446\u0438\u0430\u043B\u044C\u043D\u0430\u044F \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u0430 \u2014 \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u0430 \u0433\u0430\u0437\u0430, \u043F\u0440\u0438\u0432\u0435\u0434\u0451\u043D\u043D\u043E\u0433\u043E \u0430\u0434\u0438\u0430\u0431\u0430\u0442\u0438\u0447\u0435\u0441\u043A\u0438 \u043A \u0441\u0442\u0430\u043D\u0434\u0430\u0440\u0442\u043D\u043E\u043C\u0443 \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u044E, \u043E\u0431\u044B\u0447\u043D\u043E 105 \u041F\u0430. \u041E\u0431\u043E\u0437\u043D\u0430\u0447\u0430\u0435\u0442\u0441\u044F \u0433\u0440\u0435\u0447\u0435\u0441\u043A\u043E\u0439 \u0431\u0443\u043A\u0432\u043E\u0439 \u0438 \u0432\u044B\u0440\u0430\u0436\u0430\u0435\u0442\u0441\u044F \u0447\u0435\u0440\u0435\u0437 \u0441\u043B\u0435\u0434\u0443\u044E\u0449\u0435\u0435 \u0443\u0440\u0430\u0432\u043D\u0435\u043D\u0438\u0435, \u043D\u0430\u0437\u044B\u0432\u0430\u0435\u043C\u043E\u0435 \u0442\u0430\u043A\u0436\u0435 \u0443\u0440\u0430\u0432\u043D\u0435\u043D\u0438\u0435\u043C \u041F\u0443\u0430\u0441\u0441\u043E\u043D\u0430: \u0433\u0434\u0435 \u2014 \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u0430 \u0432 \u043A\u0435\u043B\u044C\u0432\u0438\u043D\u0430\u0445, \u2014 \u0433\u0430\u0437\u043E\u0432\u0430\u044F \u043F\u043E\u0441\u0442\u043E\u044F\u043D\u043D\u0430\u044F \u0438 \u2014 \u0443\u0434\u0435\u043B\u044C\u043D\u0430\u044F \u0442\u0435\u043F\u043B\u043E\u0451\u043C\u043A\u043E\u0441\u0442\u044C \u0432 \u0438\u0437\u043E\u0431\u0430\u0440\u043D\u043E\u043C \u043F\u0440\u043E\u0446\u0435\u0441\u0441\u0435."@ru . . . . . "\u6E29\u4F4D\uFF08\u304A\u3093\u3044\u3001\u82F1\u8A9E: potential temperature\uFF09\u3068\u306F\u3001\u6C17\u5727\u3001\u6E29\u5EA6\u306E\u7A7A\u6C17\u584A\u3092\u5727\u529B hPa\u306B\u65AD\u71B1\u5909\u5316\u3055\u305B\u305F\u3068\u304D\u306E\u6E29\u5EA6\u306E\u3053\u3068\u3067\u3042\u308B\u3002 \u6E29\u4F4D\u3092\u3068\u3059\u308B\u3068\u3001 \uFF08\u306F\u6C17\u4F53\u5B9A\u6570\u3001\u306F\u5B9A\u5727\u6BD4\u71B1\uFF09 \u3068\u3057\u3066\u8868\u3055\u308C\u308B\u3002"@ja . . "\u041F\u043E\u0442\u0435\u043D\u0446\u0438\u0430\u043B\u044C\u043D\u0430\u044F \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u0430"@ru . . "La temp\u00E9rature potentielle d'un fluide est celle qu'il aurait si on le comprimait ou d\u00E9tendait adiabatiquement jusqu'\u00E0 un niveau de pression standard , en g\u00E9n\u00E9ral 105 Pa (= 1 atm = 1 000 hPa). Cette notion est surtout utilis\u00E9e en m\u00E9t\u00E9orologie, en oc\u00E9anographie et en g\u00E9ophysique interne (g\u00E9odynamique et g\u00E9ochimie). Dans le cas de l'atmosph\u00E8re, on calcule la temp\u00E9rature qu'aurait une certaine parcelle d'air \u00E0 la pression de 1 000 hPa, pression proche de la normale \u00E0 la surface de la Terre. Dans le cas de l'eau, on calcule la temp\u00E9rature qu'aurait une certaine parcelle d'eau en surface. Dans le cas des roches du manteau, on calcule la temp\u00E9rature qu'elles auraient si elles remontaient jusqu'\u00E0 la surface de la Terre sans \u00E9change de chaleur avec l'encaissant et sans subir de transitions de phas"@fr . "1122638769"^^ . . . . . "\u6E29\u4F4D\uFF08\u304A\u3093\u3044\u3001\u82F1\u8A9E: potential temperature\uFF09\u3068\u306F\u3001\u6C17\u5727\u3001\u6E29\u5EA6\u306E\u7A7A\u6C17\u584A\u3092\u5727\u529B hPa\u306B\u65AD\u71B1\u5909\u5316\u3055\u305B\u305F\u3068\u304D\u306E\u6E29\u5EA6\u306E\u3053\u3068\u3067\u3042\u308B\u3002 \u6E29\u4F4D\u3092\u3068\u3059\u308B\u3068\u3001 \uFF08\u306F\u6C17\u4F53\u5B9A\u6570\u3001\u306F\u5B9A\u5727\u6BD4\u71B1\uFF09 \u3068\u3057\u3066\u8868\u3055\u308C\u308B\u3002"@ja . . "10157"^^ . . "\u4F4D\u6EAB"@zh . . "La temp\u00E9rature potentielle d'un fluide est celle qu'il aurait si on le comprimait ou d\u00E9tendait adiabatiquement jusqu'\u00E0 un niveau de pression standard , en g\u00E9n\u00E9ral 105 Pa (= 1 atm = 1 000 hPa). Cette notion est surtout utilis\u00E9e en m\u00E9t\u00E9orologie, en oc\u00E9anographie et en g\u00E9ophysique interne (g\u00E9odynamique et g\u00E9ochimie). Dans le cas de l'atmosph\u00E8re, on calcule la temp\u00E9rature qu'aurait une certaine parcelle d'air \u00E0 la pression de 1 000 hPa, pression proche de la normale \u00E0 la surface de la Terre. Dans le cas de l'eau, on calcule la temp\u00E9rature qu'aurait une certaine parcelle d'eau en surface. Dans le cas des roches du manteau, on calcule la temp\u00E9rature qu'elles auraient si elles remontaient jusqu'\u00E0 la surface de la Terre sans \u00E9change de chaleur avec l'encaissant et sans subir de transitions de phase (de fusion, notamment)."@fr . . . "De potenti\u00EBle temperatuur is de temperatuur die een lucht- of waterhoeveelheid krijgt wanneer deze adiabatisch van een bepaalde temperatuur en druk naar een referentiedruk wordt gebracht. Het begrip wordt gebruikt in de meteorologie en de oceanografie om de invloed van de druk op de temperatuur te vereffenen. Zo kan bepaald worden of lucht op verschillende hoogtes tot dezelfde luchtsoort hoort, wat van invloed is op de atmosferische stabiliteit."@nl . . . . "Potentielle Temperatur"@de . . . . "De potenti\u00EBle temperatuur is de temperatuur die een lucht- of waterhoeveelheid krijgt wanneer deze adiabatisch van een bepaalde temperatuur en druk naar een referentiedruk wordt gebracht. Het begrip wordt gebruikt in de meteorologie en de oceanografie om de invloed van de druk op de temperatuur te vereffenen. Zo kan bepaald worden of lucht op verschillende hoogtes tot dezelfde luchtsoort hoort, wat van invloed is op de atmosferische stabiliteit."@nl . . . . . "Potential temperature"@en . . "The potential temperature of a parcel of fluid at pressure is the temperature that the parcel would attain if adiabatically brought to a standard reference pressure , usually 1,000 hPa (1,000 mb). The potential temperature is denoted and, for a gas well-approximated as ideal, is given by"@en . . . "Temperatura potencial como uma parcela de ar teria se a mesma fosse levada por um escoamento adiab\u00E1tico at\u00E9 a press\u00E3o de refer\u00EAncia igual a 1000 hPa. Um escoamento adiab\u00E1tico \u00E9 aquele que ocorre sem que haja troca de energia com o meio, ou seja, um escoamento que se d\u00E1 conservando a entropia. Sua express\u00E3o matem\u00E1tica \u00E9:"@pt . . . .