"Strato limite planetario"@it . "\u5927\u6C17\u5883\u754C\u5C64\uFF08\u305F\u3044\u304D\u304D\u3087\u3046\u304B\u3044\u305D\u3046\u3001\u82F1: atmospheric boundary layer, ABL\uFF09\u3068\u306F\u6C17\u8C61\u3001\u74B0\u5883\u3001\u7269\u8CEA\u5FAA\u74B0\u306B\u304A\u3044\u3066\u56FA\u4F53\u5883\u754C\u3067\u3042\u308B\u5730\u8868\u9762\u306E\u5F71\u97FF\u3092\u53D7\u3051\u308B\u5C64\u3092\u3044\u3046\u3002\u306E\u6700\u4E0B\u5C64\u306B\u3042\u305F\u308B\u3002\u6E29\u5E2F\u57DF\u3067\u306F\u5730\u4E0A\u304B\u3089\u304A\u304A\u3080\u306D 1 km \u4EE5\u5185\u3002\u71B1\u5E2F\u57DF\u3067\u306F 2 km \u4EE5\u4E0A\u306E\u539A\u307F\u3092\u6301\u3064\u3002\u5730\u8868\u9762\u306E\u5F71\u97FF\u3092\u307B\u3068\u3093\u3069\u53D7\u3051\u306A\u3044\u81EA\u7531\u5927\u6C17\u3068\u533A\u5225\u3055\u308C\u308B\u3002 \u98A8\u5411\u304D\u304C\u3070\u3089\u3070\u3089\u306A\u4E71\u6D41\u304C\u652F\u914D\u7684\u306A\u5C64\u3002\u6D41\u4F53\u529B\u5B66\u306B\u304A\u3051\u308B\u5883\u754C\u5C64\u306B\u3042\u305F\u308B\u3002\u5BFE\u6D41\u304C\u6D3B\u767A\u306A\u5834\u5408\u306F\u539A\u304F\u306A\u308A\u3001\u6210\u5C64\u304C\u5B89\u5B9A\u3057\u3066\u3044\u308B\u5834\u5408\u306F\u8584\u304F\u306A\u308B\u3002 \u6211\u3005\u304C\u751F\u6D3B\u3057\u3066\u3044\u308B\u306E\u306F\u3001\u307E\u3055\u306B\u3001\u3053\u306E\u5927\u6C17\u5883\u754C\u5C64\u5185\u90E8\u3067\u3042\u308B\u3002\u90FD\u5E02\u6C17\u5019\u3084\u74B0\u5883\u306E\u5206\u91CE\u306B\u304A\u3044\u3066\u91CD\u8981\u306A\u5F79\u5272\u3092\u679C\u305F\u3059\u3002\u3057\u304B\u3057\u3001\u5927\u6C17\u5883\u754C\u5C64\u306F\u5730\u8868\u9762\u306E\u72B6\u614B\uFF08\u305F\u3068\u3048\u3070\u3001\u6D77\u9762\u3001\u5185\u6C34\u9762\u3001\u6C34\u7530\u3001\u7551\u3001\u7267\u8349\u5730\u3001\u68EE\u6797\u3001\u8349\u539F\u3001\u30B3\u30F3\u30AF\u30EA\u30FC\u30C8\u304C\u8986\u3046\u90FD\u5E02\u306A\u3069\uFF09\u306B\u3088\u3063\u3066\u5909\u5316\u306B\u5BCC\u3093\u3067\u3044\u308B\u3002\u3057\u305F\u304C\u3063\u3066\u3001\u305D\u306E\u7814\u7A76\u306B\u306F\u7D30\u304B\u306A\u89B3\u6E2C\u7DB2\u304C\u5FC5\u8981\u3067\u3042\u308A\u3001\u9032\u6357\u72B6\u6CC1\u306F\u306F\u304B\u3070\u304B\u3057\u304F\u306A\u3044\u3002 \u82F1\u8A9E\u3067\u306F\u3001\u5927\u6C17\u306E\u3042\u308B\u4ED6\u306E\u60D1\u661F\u306E\u5883\u754C\u5C64\u3082\u542B\u3081\u305F\u4E00\u822C\u7684\u306A\u547C\u3073\u65B9\u3068\u3057\u3066\u3001Planetary Boundary Layer (PBL: \u65E5\u672C\u8A9E\u306B\u76F4\u8A33\u3059\u308B\u3068\u3001\u60D1\u661F\u5883\u754C\u5C64) \u3068\u3082\u547C\u3070\u308C\u308B\u3002 \u6C17\u8C61\u5B66\uFF65\u74B0\u5883\u5B66\u306E\u5206\u91CE\u3067\u5358\u7D14\u306B\u300C\u5883\u754C\u5C64\u300D\u3068\u8A00\u3046\u5834\u5408\u306F\u3001\u5927\u6C17\u5883\u754C\u5C64\u306E\u3053\u3068\u3092\u6307\u3059\u3002\u306F\u3001\u3053\u306E\u5C64\u306B\u304A\u3051\u308B\u5927\u6C17\u306E\u632F\u308B\u821E\u3044\u3084\u6C17\u8C61\u73FE\u8C61\u306B\u3064\u3044\u3066\u7814\u7A76\u3059\u308B\u5B66\u554F\u3067\u3042\u308B\u3002"@ja . . . "\uB300\uAE30\uACBD\uACC4\uCE35(\u5927\u6C23\u5883\u754C\u5C64, Planetary boundary layer, PBL)\uC740 \uAE30\uC0C1\uD559\uC5D0\uC11C \uB300\uAE30\uC758 \uAC00\uC7A5 \uB0AE\uC740 \uBD80\uBD84\uC774\uBA70, \uC774 \uCE35\uC758 \uD589\uC704\uB294 \uC9C0\uD45C \uC811\uCD09\uC5D0 \uC758\uD574 \uC9C1\uC811\uC801\uC778 \uC601\uD5A5\uC744 \uBC1B\uB294\uB2E4. \uC9C0\uAD6C\uC5D0\uC11C \uBCF4\uD1B5 1\uC2DC\uAC04 \uC774\uB0B4\uC5D0 \uD45C\uBA74 \uC758 \uBCC0\uD654\uC5D0 \uBC18\uC751\uD55C\uB2E4. \uC774 \uCE35\uC5D0\uC11C \uC720\uC18D, \uAE30\uC628, \uC2B5\uB3C4\uC640 \uAC19\uC740 \uBB3C\uB9AC\uC801\uC778 \uC591\uC740 \uB09C\uB958\uB97C \uBCF4\uC774\uBA70 \uC218\uC9C1 \uD63C\uD569\uC740 \uAC15\uD55C \uD3B8\uC774\uB2E4. \uC774 \uCE35\uC758 \uC717\uBD80\uBD84\uC740 \"\uC790\uC720\uB300\uAE30\"\uB77C\uACE0 \uBD80\uB974\uBA70 \uC5EC\uAE30\uC11C \uBC14\uB78C\uC740 \uB300\uCCB4\uB85C \uC9C0\uADE0\uD48D\uC774\uB2E4. \uBC18\uBA74\uC5D0 \uB300\uAE30\uACBD\uACC4\uCE35 \uB0B4\uC758 \uBC14\uB78C\uC740 \uD56D\uB825\uC758 \uC601\uD5A5\uC744 \uBC1B\uC73C\uBA70 \uB4F1\uCE58\uC120\uC744 \uAC00\uB85C\uC9C8\uB7EC \uD68C\uC804\uD55C\uB2E4."@ko . . "Als Peplosph\u00E4re, planetare Grenzschicht oder atmosph\u00E4rische Grenzschicht (englisch atmospheric boundary layer) wird der untere Teil der Erdatmosph\u00E4re bezeichnet, der an die Erdoberfl\u00E4che grenzt und insbesondere durch Bodenreibung und Erw\u00E4rmung turbulenzverursachend im Zeitbereich von Stunden beeinflusst wird. Typischerweise sind dies die untersten 1,5 bis 2 Kilometer in H\u00F6he, abh\u00E4ngig von Wind- und Temperaturverh\u00E4ltnissen. Die Peplosph\u00E4re ist w\u00F6rtlich genommen das \u201Eluftige Gewand\u201C, die Erdoberfl\u00E4che umh\u00FCllend (in Analogie zum Peplos als Kleid einer Frau)."@de . . "Planetarna warstwa graniczna (ang. planetary boundary layer, w skr\u00F3cie PBL), r\u00F3wnie\u017C: warstwa przyziemna, tarciowa \u2013 najni\u017Csza cz\u0119\u015B\u0107 atmosfery, b\u0119d\u0105ca pod bezpo\u015Brednim wp\u0142ywem powierzchni planety. Poj\u0119cie warstwy granicznej wywodzi si\u0119 z dynamiki p\u0142yn\u00F3w. Jest to warstwa, kt\u00F3ra szybko reaguje termicznie na zmiany temperatury powierzchni, w szczeg\u00F3lno\u015Bci nagrzewanie przez promienie s\u0142oneczne. Z tego powodu jej temperatura (i grubo\u015B\u0107) waha si\u0119 w cyklu dobowym, co nak\u0142ada si\u0119 na roczne zmiany wywo\u0142ane zmianami nas\u0142onecznienia. Warstwa graniczna w ziemskiej atmosferze zwykle si\u0119ga do wysoko\u015Bci kilkuset metr\u00F3w, ale lokalne czynniki mog\u0105 zmienia\u0107 jej grubo\u015B\u0107 od 100 m do 2 km. Pionowy gradient temperatury w tej warstwie mo\u017Ce by\u0107 bardzo zmienny, przy silnym wypromieniowaniu ciep\u0142a (np. w zimow\u0105 noc) mo\u017Ce wyst\u0119powa\u0107 przyziemna inwersja temperatury. Pr\u0119dko\u015B\u0107 ruchu mas powietrza w warstwie granicznej jest mniejsza ni\u017C w wy\u017Cszych warstwach; rze\u017Aba terenu ma silny wp\u0142yw na jej kszta\u0142towanie. Tarcie o niejednorodn\u0105 powierzchni\u0119 wywo\u0142uje zawirowania powietrza. Du\u017Ce s\u0105 tak\u017Ce ruchy pionowe wywo\u0142ywane konwekcj\u0105."@pl . . . . . "\u5728\u6C14\u8C61\u5B66\u4E2D\uFF0C\u5927\u6C14\u8FB9\u754C\u5C42\uFF08\u82F1\u8A9E\uFF1Aatmospheric boundary layer, ABL\uFF09\uFF0C\u4E5F\u79F0\u4E3A\u884C\u661F\u8FB9\u754C\u5C42\uFF08\u82F1\u8A9E\uFF1Aplanetary boundary layer, PBL\u6216peplosphere\uFF09\uFF0C\u662F\u5927\u6C14\u5C42\u4E2D\u6700\u63A5\u8FD1\u7684\u90E8\u5206\uFF08\u908A\u754C\u5C64\uFF09\uFF0C\u5927\u7EA6\u5360\u5BF9\u6D41\u5C42\u768410%-20%\u3002\u7531\u4E8E\u5730\u8868\u6469\u64E6\u529B\uFF0C\u5927\u6C14\u8FB9\u754C\u5C42\u4E2D\u5B58\u5728\u6E4D\u6D41\uFF0C\u5782\u76F4\u6DF7\u5408\u5F3A\u70C8\uFF0C\u98CE\u901F\u3001\u6E29\u5EA6\u548C\u6E7F\u5EA6\u7B49\u7269\u7406\u91CF\u5FEB\u901F\u6CE2\u52A8\u3002\u5927\u6C14\u8FB9\u754C\u5C42\u4E4B\u4E0A\u7684\u90E8\u5206\u79F0\u201C\u81EA\u7531\u5927\u6C14\u201D\uFF0C\u5176\u98CE\u901F\u98CE\u5411\u8FD1\u4F3C\u662F\u884C\u661F\u81EA\u8F6C\u5F15\u8D77\u7684\uFF0C\u5373\u5730\u8F6C\u98CE\uFF08\u5E73\u884C\u4E8E\u7B49\u538B\u7EBF\uFF09\u3002"@zh . . . . "A Camada Limite Atmosf\u00E9rica (CLA) ou Camada Limite Planet\u00E1ria(CLP), como tamb\u00E9m \u00E9 conhecida, com altura t\u00EDpica de 1 km, situa-se na baixa troposfera e assim sofre diretamente a influ\u00EAncia da superf\u00EDcie. A escala de tempo dos fen\u00F4menos da CLA \u00E9 igual ou inferior a uma (1) hora."@pt . . . . . . . "Couche limite atmosph\u00E9rique"@fr . . "In meteorologia lo strato limite planetario, o Planetary Boundary Layer (PBL), \u00E8 definito come quella porzione di troposfera posta a diretto contatto con il suolo, l'uomo e la biosfera, influenzata dalla presenza della superficie terrestre e che risponde alle variazioni atmosferiche con una scala di tempo di circa un'ora; tale strato spesso viene indicato semplicemente come boundary layer o strato di rimescolamento."@it . . "Als Peplosph\u00E4re, planetare Grenzschicht oder atmosph\u00E4rische Grenzschicht (englisch atmospheric boundary layer) wird der untere Teil der Erdatmosph\u00E4re bezeichnet, der an die Erdoberfl\u00E4che grenzt und insbesondere durch Bodenreibung und Erw\u00E4rmung turbulenzverursachend im Zeitbereich von Stunden beeinflusst wird. Typischerweise sind dies die untersten 1,5 bis 2 Kilometer in H\u00F6he, abh\u00E4ngig von Wind- und Temperaturverh\u00E4ltnissen. Die Peplosph\u00E4re ist w\u00F6rtlich genommen das \u201Eluftige Gewand\u201C, die Erdoberfl\u00E4che umh\u00FCllend (in Analogie zum Peplos als Kleid einer Frau)."@de . "La capa l\u00EDmit atmosf\u00E8rica tamb\u00E9 coneguda com a capa l\u00EDmit planet\u00E0ria \u00E9s la part m\u00E9s baixa de l'atmosfera i el seu comportament est\u00E0 directament influenciat pel seu contacte amb la superf\u00EDcie planet\u00E0ria. A la Terra normalment respon als canvis en la superf\u00EDcie en una hora o menys. En aquesta capa les quantitats f\u00EDsiques com la temperatura, la humitat, etc. mostren fluctuacions r\u00E0pides la turbul\u00E8ncia i la mescla vertical s\u00F3n acusades. Sobre aquesta capa l\u00EDmit es troba l'atmosfera lliure on el vent \u00E9s aproximadament vent geostr\u00F2fic (paral\u00B7lel a les is\u00F2bares) mentre que dins d'aquesta capa l\u00EDmit el vent est\u00E0 afectat pel forces de resist\u00E8ncia aerodin\u00E0mica i va perpendicular a les is\u00F2bares. L'atmosfera lliure no \u00E9s turbulenta o nom\u00E9s ho \u00E9s de manera intermitent."@ca . . "\u041F\u043B\u0430\u043D\u0435\u0442\u0430\u0301\u0440\u043D\u044B\u0439 \u043F\u043E\u0433\u0440\u0430\u043D\u0438\u0301\u0447\u043D\u044B\u0439 \u0441\u043B\u043E\u0439 (\u00AB\u043F\u043E\u0433\u0440\u0430\u043D\u0438\u0447\u043D\u044B\u0439 \u0441\u043B\u043E\u0439 \u0430\u0442\u043C\u043E\u0441\u0444\u0435\u0440\u044B\u00BB, \u00AB\u0441\u043B\u043E\u0439 \u0442\u0440\u0435\u043D\u0438\u044F\u00BB) \u2014 \u043D\u0438\u0436\u043D\u0438\u0439 \u0441\u043B\u043E\u0439 \u0433\u0430\u0437\u043E\u0432\u043E\u0439 \u043E\u0431\u043E\u043B\u043E\u0447\u043A\u0438 \u043F\u043B\u0430\u043D\u0435\u0442\u044B, \u0441\u0432\u043E\u0439\u0441\u0442\u0432\u0430 \u0438 \u0434\u0438\u043D\u0430\u043C\u0438\u043A\u0430 \u043A\u043E\u0442\u043E\u0440\u043E\u0433\u043E \u0432 \u0437\u043D\u0430\u0447\u0438\u0442\u0435\u043B\u044C\u043D\u043E\u0439 \u043C\u0435\u0440\u0435 \u043E\u043F\u0440\u0435\u0434\u0435\u043B\u044F\u044E\u0442\u0441\u044F \u0432\u0437\u0430\u0438\u043C\u043E\u0434\u0435\u0439\u0441\u0442\u0432\u0438\u0435\u043C \u0441 \u0442\u0432\u0451\u0440\u0434\u043E\u0439 (\u0438\u043B\u0438 \u0436\u0438\u0434\u043A\u043E\u0439) \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u043E\u0441\u0442\u044C\u044E \u043F\u043B\u0430\u043D\u0435\u0442\u044B (\u0442\u0430\u043A \u043D\u0430\u0437\u044B\u0432\u0430\u0435\u043C\u043E\u0439 \u00AB\u043F\u043E\u0434\u0441\u0442\u0438\u043B\u0430\u044E\u0449\u0435\u0439 \u043F\u043E\u0432\u0435\u0440\u0445\u043D\u043E\u0441\u0442\u044C\u044E\u00BB). \u0424\u0438\u0437\u0438\u0447\u0435\u0441\u043A\u0438\u0435 \u043F\u0440\u043E\u0446\u0435\u0441\u0441\u044B, \u043F\u0440\u043E\u0438\u0441\u0445\u043E\u0434\u044F\u0449\u0438\u0435 \u0432 \u043F\u043E\u0433\u0440\u0430\u043D\u0438\u0447\u043D\u043E\u043C \u0441\u043B\u043E\u0435 \u0430\u0442\u043C\u043E\u0441\u0444\u0435\u0440\u044B, \u044F\u0432\u043B\u044F\u044E\u0442\u0441\u044F \u043F\u0440\u0435\u0434\u043C\u0435\u0442\u043E\u043C \u0438\u0441\u0441\u043B\u0435\u0434\u043E\u0432\u0430\u043D\u0438\u044F \u043E\u0442\u0434\u0435\u043B\u044C\u043D\u043E\u0433\u043E \u0440\u0430\u0437\u0434\u0435\u043B\u0430 \u0434\u0438\u043D\u0430\u043C\u0438\u0447\u0435\u0441\u043A\u043E\u0439 \u043C\u0435\u0442\u0435\u043E\u0440\u043E\u043B\u043E\u0433\u0438\u0438.\u0412\u0435\u0440\u0445\u043D\u0438\u0439 \u0441\u043B\u043E\u0439 \u043E\u043A\u0435\u0430\u043D\u0430 \u0442\u043E\u0436\u0435 \u044F\u0432\u043B\u044F\u0435\u0442\u0441\u044F \u043F\u043E\u0433\u0440\u0430\u043D\u0438\u0447\u043D\u044B\u043C. \u0412\u0437\u0430\u0438\u043C\u043E\u0434\u0435\u0439\u0441\u0442\u0432\u0438\u0435 \u0430\u0442\u043C\u043E\u0441\u0444\u0435\u0440\u044B \u0438 \u043E\u043A\u0435\u0430\u043D\u0430 \u0441\u043E\u0441\u0440\u0435\u0434\u043E\u0442\u043E\u0447\u0435\u043D\u043E \u0432 \u0438\u0445 \u043F\u043E\u0433\u0440\u0430\u043D\u0438\u0447\u043D\u044B\u0445 \u0441\u043B\u043E\u044F\u0445."@ru . . . "Camada limite atmosf\u00E9rica"@pt . . . . . "\u0641\u064A \u0645\u062C\u0627\u0644 \u0627\u0644\u0623\u0631\u0635\u0627\u062F \u0627\u0644\u062C\u0648\u064A\u0629 \u0644\u0644\u0637\u0628\u0642\u0629 \u0628\u064A\u0646 \u0627\u0644\u062D\u062F\u0648\u062F \u0627\u0644\u0643\u0648\u0643\u0628\u064A\u0629 (PBL)\u060C \u0627\u0644\u0645\u0639\u0631\u0648\u0641\u0629 \u0623\u064A\u0636\u0627 \u0628\u0627\u0633\u0645 \u0637\u0628\u0642\u0629 \u062D\u062F\u0648\u062F \u0627\u0644\u063A\u0644\u0627\u0641 \u0627\u0644\u062C\u0648\u064A (ABL)\u060C \u0647\u064A \u0627\u0644\u062C\u0632\u0621 \u0627\u0644\u0623\u062F\u0646\u0649 \u0645\u0646 \u0627\u0644\u063A\u0644\u0627\u0641 \u0627\u0644\u062C\u0648\u064A. \u0648\u064A\u062A\u0623\u062B\u0631 \u0633\u0644\u0648\u0643\u0647 \u0645\u0628\u0627\u0634\u0631\u0629 \u0639\u0646 \u0637\u0631\u064A\u0642 \u0627\u0644\u0627\u062A\u0635\u0627\u0644 \u0645\u0639 \u0633\u0637\u062D \u0627\u0644\u0643\u0648\u0627\u0643\u0628. \u0639\u0644\u0649 \u0627\u0644\u0623\u0631\u0636 \u0641\u0625\u0646\u0647 \u0639\u0627\u062F\u0629 \u0645\u0627 \u064A\u0633\u062A\u062C\u064A\u0628 \u0644\u0644\u062A\u063A\u064A\u0631\u0627\u062A \u0641\u064A \u0642\u0648\u0629 \u0627\u0634\u0639\u0627\u0639 \u0627\u0644\u0633\u0637\u062D \u0641\u064A \u0633\u0627\u0639\u0629 \u0648\u0627\u062D\u062F\u0629 \u0623\u0648 \u0623\u0642\u0644. \u0641\u064A \u0647\u0630\u0647 \u0627\u0644\u0643\u0645\u064A\u0627\u062A \u0627\u0644\u0641\u064A\u0632\u064A\u0627\u0626\u064A\u0629 \u0644\u0644\u0637\u0628\u0642\u0629 \u0645\u062B\u0644 \u0633\u0631\u0639\u0629 \u0627\u0644\u062A\u062F\u0641\u0642\u060C \u0648\u062F\u0631\u062C\u0629 \u0627\u0644\u062D\u0631\u0627\u0631\u0629\u060C \u0648\u0627\u0644\u0631\u0637\u0648\u0628\u0629\u060C \u0648\u0645\u0627 \u0625\u0644\u0649 \u0630\u0644\u0643\u060C \u0639\u0631\u0636 \u0627\u0644\u062A\u0642\u0644\u0628\u0627\u062A \u0627\u0644\u0633\u0631\u064A\u0639\u0629 (\u0627\u0644\u0627\u0636\u0637\u0631\u0627\u0628) \u0648\u0627\u0644\u0627\u0646\u062F\u0645\u0627\u062C \u0627\u0644\u0631\u0623\u0633\u064A \u064A\u0643\u0648\u0646 \u0642\u0648\u064A\u0627. \u0641\u0648\u0642 PBL \u0647\u0648 \u00AB\u0627\u0644\u063A\u0644\u0627\u0641 \u0627\u0644\u062C\u0648\u064A \u0627\u0644\u062D\u0631\u00BB \u062D\u064A\u062B \u062A\u0643\u0648\u0646 \u0627\u0644\u0631\u064A\u0627\u062D \u062A\u0642\u0631\u064A\u0628\u0627 \u062C\u064A\u0648\u0633\u062A\u0631\u0648\u0641\u064A\u0629 (\u0645\u0648\u0627\u0632\u064A\u0629 \u0644\u0644\u0623\u064A\u0633\u0648\u0628\u0627\u0631)\u060C \u0641\u064A \u062D\u064A\u0646 \u0636\u0645\u0646 PBL \u062A\u062A\u0623\u062B\u0631 \u0627\u0644\u0631\u064A\u0627\u062D \u0627\u0644\u0633\u0637\u062D\u064A\u0629 \u0639\u0646 \u0637\u0631\u064A\u0642 \u0627\u0644\u0633\u062D\u0628 \u0648\u062A\u062A\u062D\u0648\u0644 \u0639\u0628\u0631 \u0627\u0644\u0623\u064A\u0633\u0648\u0628\u0627\u0631. \u0641\u064A \u0627\u0644\u063A\u0644\u0627\u0641 \u0627\u0644\u062C\u0648\u064A \u0627\u0644\u062D\u0631 \u0627\u0644\u0630\u064A \u064A\u0643\u0648\u0646 \u0639\u0627\u062F\u0629 \u063A\u064A\u0631 \u0645\u0636\u0637\u0631\u0628\u0627\u060C \u0623\u0648 \u0641\u0642\u0637 \u0645\u0636\u0637\u0631\u0628\u0627 \u0628\u0634\u0643\u0644 \u0645\u062A\u0642\u0637\u0639."@ar . "Planetarna warstwa graniczna (ang. planetary boundary layer, w skr\u00F3cie PBL), r\u00F3wnie\u017C: warstwa przyziemna, tarciowa \u2013 najni\u017Csza cz\u0119\u015B\u0107 atmosfery, b\u0119d\u0105ca pod bezpo\u015Brednim wp\u0142ywem powierzchni planety. Poj\u0119cie warstwy granicznej wywodzi si\u0119 z dynamiki p\u0142yn\u00F3w. Pr\u0119dko\u015B\u0107 ruchu mas powietrza w warstwie granicznej jest mniejsza ni\u017C w wy\u017Cszych warstwach; rze\u017Aba terenu ma silny wp\u0142yw na jej kszta\u0142towanie. Tarcie o niejednorodn\u0105 powierzchni\u0119 wywo\u0142uje zawirowania powietrza. Du\u017Ce s\u0105 tak\u017Ce ruchy pionowe wywo\u0142ywane konwekcj\u0105."@pl . "La capa l\u00EDmit atmosf\u00E8rica tamb\u00E9 coneguda com a capa l\u00EDmit planet\u00E0ria \u00E9s la part m\u00E9s baixa de l'atmosfera i el seu comportament est\u00E0 directament influenciat pel seu contacte amb la superf\u00EDcie planet\u00E0ria. A la Terra normalment respon als canvis en la superf\u00EDcie en una hora o menys. En aquesta capa les quantitats f\u00EDsiques com la temperatura, la humitat, etc. mostren fluctuacions r\u00E0pides la turbul\u00E8ncia i la mescla vertical s\u00F3n acusades. Sobre aquesta capa l\u00EDmit es troba l'atmosfera lliure on el vent \u00E9s aproximadament vent geostr\u00F2fic (paral\u00B7lel a les is\u00F2bares) mentre que dins d'aquesta capa l\u00EDmit el vent est\u00E0 afectat pel forces de resist\u00E8ncia aerodin\u00E0mica i va perpendicular a les is\u00F2bares. L'atmosfera lliure no \u00E9s turbulenta o nom\u00E9s ho \u00E9s de manera intermitent."@ca . . . . "Peplosph\u00E4re"@de . . . . . . . . . . "Planetary boundary layer"@en . . "\u5927\u6C23\u908A\u754C\u5C64"@zh . "La couche limite atmosph\u00E9rique (CLA), \u00E9galement connu sous le nom de couche limite plan\u00E9taire (CLP) ou couche limite de frottement, est en m\u00E9t\u00E9orologie la partie la plus basse de la troposph\u00E8re dont le comportement est directement influenc\u00E9 par le frottement avec une surface plan\u00E9taire. Sur Terre, elle r\u00E9pond g\u00E9n\u00E9ralement aux changements du for\u00E7age radiatif de surface en une heure ou moins. Dans cette couche, des quantit\u00E9s physiques telles que la vitesse d'\u00E9coulement, la temp\u00E9rature et l'humidit\u00E9 pr\u00E9sentent des fluctuations rapides (turbulence) et le m\u00E9lange vertical est intense. Au-dessus de la CLA se trouve l'atmosph\u00E8re libre, l\u00E0 o\u00F9 le vent est approximativement g\u00E9ostrophique (parall\u00E8le aux isobares), tandis que dans la couche limite, le vent est affect\u00E9 par la tra\u00EEn\u00E9e superficielle due "@fr . . . . . "Planetarna warstwa graniczna"@pl . . . . . "\uB300\uAE30\uACBD\uACC4\uCE35(\u5927\u6C23\u5883\u754C\u5C64, Planetary boundary layer, PBL)\uC740 \uAE30\uC0C1\uD559\uC5D0\uC11C \uB300\uAE30\uC758 \uAC00\uC7A5 \uB0AE\uC740 \uBD80\uBD84\uC774\uBA70, \uC774 \uCE35\uC758 \uD589\uC704\uB294 \uC9C0\uD45C \uC811\uCD09\uC5D0 \uC758\uD574 \uC9C1\uC811\uC801\uC778 \uC601\uD5A5\uC744 \uBC1B\uB294\uB2E4. \uC9C0\uAD6C\uC5D0\uC11C \uBCF4\uD1B5 1\uC2DC\uAC04 \uC774\uB0B4\uC5D0 \uD45C\uBA74 \uC758 \uBCC0\uD654\uC5D0 \uBC18\uC751\uD55C\uB2E4. \uC774 \uCE35\uC5D0\uC11C \uC720\uC18D, \uAE30\uC628, \uC2B5\uB3C4\uC640 \uAC19\uC740 \uBB3C\uB9AC\uC801\uC778 \uC591\uC740 \uB09C\uB958\uB97C \uBCF4\uC774\uBA70 \uC218\uC9C1 \uD63C\uD569\uC740 \uAC15\uD55C \uD3B8\uC774\uB2E4. \uC774 \uCE35\uC758 \uC717\uBD80\uBD84\uC740 \"\uC790\uC720\uB300\uAE30\"\uB77C\uACE0 \uBD80\uB974\uBA70 \uC5EC\uAE30\uC11C \uBC14\uB78C\uC740 \uB300\uCCB4\uB85C \uC9C0\uADE0\uD48D\uC774\uB2E4. \uBC18\uBA74\uC5D0 \uB300\uAE30\uACBD\uACC4\uCE35 \uB0B4\uC758 \uBC14\uB78C\uC740 \uD56D\uB825\uC758 \uC601\uD5A5\uC744 \uBC1B\uC73C\uBA70 \uB4F1\uCE58\uC120\uC744 \uAC00\uB85C\uC9C8\uB7EC \uD68C\uC804\uD55C\uB2E4."@ko . . . . . "1089423960"^^ . . . . . . "Capa l\u00EDmit atmosf\u00E8rica"@ca . . . . . "20468"^^ . . "In meteorologia lo strato limite planetario, o Planetary Boundary Layer (PBL), \u00E8 definito come quella porzione di troposfera posta a diretto contatto con il suolo, l'uomo e la biosfera, influenzata dalla presenza della superficie terrestre e che risponde alle variazioni atmosferiche con una scala di tempo di circa un'ora; tale strato spesso viene indicato semplicemente come boundary layer o strato di rimescolamento."@it . . . . . . . "\u5728\u6C14\u8C61\u5B66\u4E2D\uFF0C\u5927\u6C14\u8FB9\u754C\u5C42\uFF08\u82F1\u8A9E\uFF1Aatmospheric boundary layer, ABL\uFF09\uFF0C\u4E5F\u79F0\u4E3A\u884C\u661F\u8FB9\u754C\u5C42\uFF08\u82F1\u8A9E\uFF1Aplanetary boundary layer, PBL\u6216peplosphere\uFF09\uFF0C\u662F\u5927\u6C14\u5C42\u4E2D\u6700\u63A5\u8FD1\u7684\u90E8\u5206\uFF08\u908A\u754C\u5C64\uFF09\uFF0C\u5927\u7EA6\u5360\u5BF9\u6D41\u5C42\u768410%-20%\u3002\u7531\u4E8E\u5730\u8868\u6469\u64E6\u529B\uFF0C\u5927\u6C14\u8FB9\u754C\u5C42\u4E2D\u5B58\u5728\u6E4D\u6D41\uFF0C\u5782\u76F4\u6DF7\u5408\u5F3A\u70C8\uFF0C\u98CE\u901F\u3001\u6E29\u5EA6\u548C\u6E7F\u5EA6\u7B49\u7269\u7406\u91CF\u5FEB\u901F\u6CE2\u52A8\u3002\u5927\u6C14\u8FB9\u754C\u5C42\u4E4B\u4E0A\u7684\u90E8\u5206\u79F0\u201C\u81EA\u7531\u5927\u6C14\u201D\uFF0C\u5176\u98CE\u901F\u98CE\u5411\u8FD1\u4F3C\u662F\u884C\u661F\u81EA\u8F6C\u5F15\u8D77\u7684\uFF0C\u5373\u5730\u8F6C\u98CE\uFF08\u5E73\u884C\u4E8E\u7B49\u538B\u7EBF\uFF09\u3002"@zh . "La couche limite atmosph\u00E9rique (CLA), \u00E9galement connu sous le nom de couche limite plan\u00E9taire (CLP) ou couche limite de frottement, est en m\u00E9t\u00E9orologie la partie la plus basse de la troposph\u00E8re dont le comportement est directement influenc\u00E9 par le frottement avec une surface plan\u00E9taire. Sur Terre, elle r\u00E9pond g\u00E9n\u00E9ralement aux changements du for\u00E7age radiatif de surface en une heure ou moins. Dans cette couche, des quantit\u00E9s physiques telles que la vitesse d'\u00E9coulement, la temp\u00E9rature et l'humidit\u00E9 pr\u00E9sentent des fluctuations rapides (turbulence) et le m\u00E9lange vertical est intense. Au-dessus de la CLA se trouve l'atmosph\u00E8re libre, l\u00E0 o\u00F9 le vent est approximativement g\u00E9ostrophique (parall\u00E8le aux isobares), tandis que dans la couche limite, le vent est affect\u00E9 par la tra\u00EEn\u00E9e superficielle due au frottement avec le relief et s'oriente en travers des isobares vers les pressions plus basses. L'\u00E9paisseur de cette couche limite atmosph\u00E9rique varie entre 50 m et 3 km, selon la stabilit\u00E9 de l'air et la rugosit\u00E9 de la surface, la moyenne \u00E9tant de 1 000 \u00E0 1 500 m. Au-dessus de la couche limite atmosph\u00E9rique (form\u00E9e d'une couche de surface et de la couche d\u2019Ekman) s\u2019\u00E9tend ce que l\u2019on appelle l\u2019atmosph\u00E8re libre (sous-entendu \u00AB libre de l\u2019influence du sol \u00BB, mais pas de l\u2019influence de la force de Coriolis ou autres) : Plus on s\u2019\u00E9l\u00E8ve au sein de l\u2019atmosph\u00E8re libre plus le vent s\u2019approche (en force et direction) du vent g\u00E9ostrophique. L'\u00E9tude des \u00E9changes de mati\u00E8re, d'\u00E9nergie et de mouvement se produisant au sein de la couche limite atmosph\u00E9rique joue un r\u00F4le important dans la mise au point des mod\u00E8les de pr\u00E9vision num\u00E9rique du temps. La param\u00E9trisation des \u00E9changes horizontaux et verticaux, selon les conditions de stabilit\u00E9 de l'air, sert \u00E0 d\u00E9terminer le type et la formation de nuages, des pr\u00E9cipitations, ainsi que la structure verticale des vents \u00E0 chaque instant de la pr\u00E9vision, la surface terrestre constituant l'une des limites physiques o\u00F9 la vitesse et les mouvements verticaux doivent \u00EAtre nuls."@fr . . "July 2020"@en . "In meteorology, the planetary boundary layer (PBL), also known as the atmospheric boundary layer (ABL) or peplosphere, is the lowest part of the atmosphere and its behaviour is directly influenced by its contact with a planetary surface. On Earth it usually responds to changes in surface radiative forcing in an hour or less. In this layer physical quantities such as flow velocity, temperature, and moisture display rapid fluctuations (turbulence) and vertical mixing is strong. Above the PBL is the \"free atmosphere\", where the wind is approximately geostrophic (parallel to the isobars), while within the PBL the wind is affected by surface drag and turns across the isobars (see Ekman layer for more detail)."@en . . . . . . . . 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\u0441\u043B\u043E\u0435 \u0432\u044B\u0434\u0435\u043B\u044F\u044E\u0442 \u0442\u0440\u0438 \u0441\u043B\u043E\u044F:"@ru . . "it is unclear what they would be most important for, and what causes them to be most important for it; is the next clause meant as a defining relative clause ?"@en . . . . . "\u5927\u6C17\u5883\u754C\u5C64"@ja . "\u5927\u6C17\u5883\u754C\u5C64\uFF08\u305F\u3044\u304D\u304D\u3087\u3046\u304B\u3044\u305D\u3046\u3001\u82F1: atmospheric boundary layer, ABL\uFF09\u3068\u306F\u6C17\u8C61\u3001\u74B0\u5883\u3001\u7269\u8CEA\u5FAA\u74B0\u306B\u304A\u3044\u3066\u56FA\u4F53\u5883\u754C\u3067\u3042\u308B\u5730\u8868\u9762\u306E\u5F71\u97FF\u3092\u53D7\u3051\u308B\u5C64\u3092\u3044\u3046\u3002\u306E\u6700\u4E0B\u5C64\u306B\u3042\u305F\u308B\u3002\u6E29\u5E2F\u57DF\u3067\u306F\u5730\u4E0A\u304B\u3089\u304A\u304A\u3080\u306D 1 km \u4EE5\u5185\u3002\u71B1\u5E2F\u57DF\u3067\u306F 2 km \u4EE5\u4E0A\u306E\u539A\u307F\u3092\u6301\u3064\u3002\u5730\u8868\u9762\u306E\u5F71\u97FF\u3092\u307B\u3068\u3093\u3069\u53D7\u3051\u306A\u3044\u81EA\u7531\u5927\u6C17\u3068\u533A\u5225\u3055\u308C\u308B\u3002 \u98A8\u5411\u304D\u304C\u3070\u3089\u3070\u3089\u306A\u4E71\u6D41\u304C\u652F\u914D\u7684\u306A\u5C64\u3002\u6D41\u4F53\u529B\u5B66\u306B\u304A\u3051\u308B\u5883\u754C\u5C64\u306B\u3042\u305F\u308B\u3002\u5BFE\u6D41\u304C\u6D3B\u767A\u306A\u5834\u5408\u306F\u539A\u304F\u306A\u308A\u3001\u6210\u5C64\u304C\u5B89\u5B9A\u3057\u3066\u3044\u308B\u5834\u5408\u306F\u8584\u304F\u306A\u308B\u3002 \u6211\u3005\u304C\u751F\u6D3B\u3057\u3066\u3044\u308B\u306E\u306F\u3001\u307E\u3055\u306B\u3001\u3053\u306E\u5927\u6C17\u5883\u754C\u5C64\u5185\u90E8\u3067\u3042\u308B\u3002\u90FD\u5E02\u6C17\u5019\u3084\u74B0\u5883\u306E\u5206\u91CE\u306B\u304A\u3044\u3066\u91CD\u8981\u306A\u5F79\u5272\u3092\u679C\u305F\u3059\u3002\u3057\u304B\u3057\u3001\u5927\u6C17\u5883\u754C\u5C64\u306F\u5730\u8868\u9762\u306E\u72B6\u614B\uFF08\u305F\u3068\u3048\u3070\u3001\u6D77\u9762\u3001\u5185\u6C34\u9762\u3001\u6C34\u7530\u3001\u7551\u3001\u7267\u8349\u5730\u3001\u68EE\u6797\u3001\u8349\u539F\u3001\u30B3\u30F3\u30AF\u30EA\u30FC\u30C8\u304C\u8986\u3046\u90FD\u5E02\u306A\u3069\uFF09\u306B\u3088\u3063\u3066\u5909\u5316\u306B\u5BCC\u3093\u3067\u3044\u308B\u3002\u3057\u305F\u304C\u3063\u3066\u3001\u305D\u306E\u7814\u7A76\u306B\u306F\u7D30\u304B\u306A\u89B3\u6E2C\u7DB2\u304C\u5FC5\u8981\u3067\u3042\u308A\u3001\u9032\u6357\u72B6\u6CC1\u306F\u306F\u304B\u3070\u304B\u3057\u304F\u306A\u3044\u3002 \u82F1\u8A9E\u3067\u306F\u3001\u5927\u6C17\u306E\u3042\u308B\u4ED6\u306E\u60D1\u661F\u306E\u5883\u754C\u5C64\u3082\u542B\u3081\u305F\u4E00\u822C\u7684\u306A\u547C\u3073\u65B9\u3068\u3057\u3066\u3001Planetary Boundary Layer (PBL: \u65E5\u672C\u8A9E\u306B\u76F4\u8A33\u3059\u308B\u3068\u3001\u60D1\u661F\u5883\u754C\u5C64) \u3068\u3082\u547C\u3070\u308C\u308B\u3002 \u6C17\u8C61\u5B66\uFF65\u74B0\u5883\u5B66\u306E\u5206\u91CE\u3067\u5358\u7D14\u306B\u300C\u5883\u754C\u5C64\u300D\u3068\u8A00\u3046\u5834\u5408\u306F\u3001\u5927\u6C17\u5883\u754C\u5C64\u306E\u3053\u3068\u3092\u6307\u3059\u3002\u306F\u3001\u3053\u306E\u5C64\u306B\u304A\u3051\u308B\u5927\u6C17\u306E\u632F\u308B\u821E\u3044\u3084\u6C17\u8C61\u73FE\u8C61\u306B\u3064\u3044\u3066\u7814\u7A76\u3059\u308B\u5B66\u554F\u3067\u3042\u308B\u3002"@ja . . . "\u041F\u043B\u0430\u043D\u0435\u0442\u0430\u0440\u043D\u044B\u0439 \u043F\u043E\u0433\u0440\u0430\u043D\u0438\u0447\u043D\u044B\u0439 \u0441\u043B\u043E\u0439"@ru . . . . "In meteorology, the planetary boundary layer (PBL), also known as the atmospheric boundary layer (ABL) or peplosphere, is the lowest part of the atmosphere and its behaviour is directly influenced by its contact with a planetary surface. On Earth it usually responds to changes in surface radiative forcing in an hour or less. In this layer physical quantities such as flow velocity, temperature, and moisture display rapid fluctuations (turbulence) and vertical mixing is strong. Above the PBL is the \"free atmosphere\", where the wind is approximately geostrophic (parallel to the isobars), while within the PBL the wind is affected by surface drag and turns across the isobars (see Ekman layer for more detail)."@en . . . . "927641"^^ . . . . . . "\u0637\u0628\u0642\u0629 \u0627\u0644\u062D\u062F\u0648\u062F \u0627\u0644\u0643\u0648\u0643\u0628\u064A\u0629"@ar . . . . . . . . . . . "\uB300\uAE30\uACBD\uACC4\uCE35"@ko . . . . . . . "\u0641\u064A \u0645\u062C\u0627\u0644 \u0627\u0644\u0623\u0631\u0635\u0627\u062F \u0627\u0644\u062C\u0648\u064A\u0629 \u0644\u0644\u0637\u0628\u0642\u0629 \u0628\u064A\u0646 \u0627\u0644\u062D\u062F\u0648\u062F \u0627\u0644\u0643\u0648\u0643\u0628\u064A\u0629 (PBL)\u060C \u0627\u0644\u0645\u0639\u0631\u0648\u0641\u0629 \u0623\u064A\u0636\u0627 \u0628\u0627\u0633\u0645 \u0637\u0628\u0642\u0629 \u062D\u062F\u0648\u062F \u0627\u0644\u063A\u0644\u0627\u0641 \u0627\u0644\u062C\u0648\u064A (ABL)\u060C \u0647\u064A \u0627\u0644\u062C\u0632\u0621 \u0627\u0644\u0623\u062F\u0646\u0649 \u0645\u0646 \u0627\u0644\u063A\u0644\u0627\u0641 \u0627\u0644\u062C\u0648\u064A. \u0648\u064A\u062A\u0623\u062B\u0631 \u0633\u0644\u0648\u0643\u0647 \u0645\u0628\u0627\u0634\u0631\u0629 \u0639\u0646 \u0637\u0631\u064A\u0642 \u0627\u0644\u0627\u062A\u0635\u0627\u0644 \u0645\u0639 \u0633\u0637\u062D \u0627\u0644\u0643\u0648\u0627\u0643\u0628. \u0639\u0644\u0649 \u0627\u0644\u0623\u0631\u0636 \u0641\u0625\u0646\u0647 \u0639\u0627\u062F\u0629 \u0645\u0627 \u064A\u0633\u062A\u062C\u064A\u0628 \u0644\u0644\u062A\u063A\u064A\u0631\u0627\u062A \u0641\u064A \u0642\u0648\u0629 \u0627\u0634\u0639\u0627\u0639 \u0627\u0644\u0633\u0637\u062D \u0641\u064A \u0633\u0627\u0639\u0629 \u0648\u0627\u062D\u062F\u0629 \u0623\u0648 \u0623\u0642\u0644. \u0641\u064A \u0647\u0630\u0647 \u0627\u0644\u0643\u0645\u064A\u0627\u062A \u0627\u0644\u0641\u064A\u0632\u064A\u0627\u0626\u064A\u0629 \u0644\u0644\u0637\u0628\u0642\u0629 \u0645\u062B\u0644 \u0633\u0631\u0639\u0629 \u0627\u0644\u062A\u062F\u0641\u0642\u060C \u0648\u062F\u0631\u062C\u0629 \u0627\u0644\u062D\u0631\u0627\u0631\u0629\u060C \u0648\u0627\u0644\u0631\u0637\u0648\u0628\u0629\u060C \u0648\u0645\u0627 \u0625\u0644\u0649 \u0630\u0644\u0643\u060C \u0639\u0631\u0636 \u0627\u0644\u062A\u0642\u0644\u0628\u0627\u062A \u0627\u0644\u0633\u0631\u064A\u0639\u0629 (\u0627\u0644\u0627\u0636\u0637\u0631\u0627\u0628) \u0648\u0627\u0644\u0627\u0646\u062F\u0645\u0627\u062C \u0627\u0644\u0631\u0623\u0633\u064A \u064A\u0643\u0648\u0646 \u0642\u0648\u064A\u0627. \u0641\u0648\u0642 PBL \u0647\u0648 \u00AB\u0627\u0644\u063A\u0644\u0627\u0641 \u0627\u0644\u062C\u0648\u064A \u0627\u0644\u062D\u0631\u00BB \u062D\u064A\u062B \u062A\u0643\u0648\u0646 \u0627\u0644\u0631\u064A\u0627\u062D \u062A\u0642\u0631\u064A\u0628\u0627 \u062C\u064A\u0648\u0633\u062A\u0631\u0648\u0641\u064A\u0629 (\u0645\u0648\u0627\u0632\u064A\u0629 \u0644\u0644\u0623\u064A\u0633\u0648\u0628\u0627\u0631)\u060C \u0641\u064A \u062D\u064A\u0646 \u0636\u0645\u0646 PBL \u062A\u062A\u0623\u062B\u0631 \u0627\u0644\u0631\u064A\u0627\u062D \u0627\u0644\u0633\u0637\u062D\u064A\u0629 \u0639\u0646 \u0637\u0631\u064A\u0642 \u0627\u0644\u0633\u062D\u0628 \u0648\u062A\u062A\u062D\u0648\u0644 \u0639\u0628\u0631 \u0627\u0644\u0623\u064A\u0633\u0648\u0628\u0627\u0631. \u0641\u064A \u0627\u0644\u063A\u0644\u0627\u0641 \u0627\u0644\u062C\u0648\u064A \u0627\u0644\u062D\u0631 \u0627\u0644\u0630\u064A \u064A\u0643\u0648\u0646 \u0639\u0627\u062F\u0629 \u063A\u064A\u0631 \u0645\u0636\u0637\u0631\u0628\u0627\u060C \u0623\u0648 \u0641\u0642\u0637 \u0645\u0636\u0637\u0631\u0628\u0627 \u0628\u0634\u0643\u0644 \u0645\u062A\u0642\u0637\u0639."@ar . . . . "A Camada Limite Atmosf\u00E9rica (CLA) ou Camada Limite Planet\u00E1ria(CLP), como tamb\u00E9m \u00E9 conhecida, com altura t\u00EDpica de 1 km, situa-se na baixa troposfera e assim sofre diretamente a influ\u00EAncia da superf\u00EDcie. A escala de tempo dos fen\u00F4menos da CLA \u00E9 igual ou inferior a uma (1) hora."@pt . . .