. . "\u0412\u043E\u043B\u043D\u044B \u0420\u043E\u0301\u0441\u0441\u0431\u0438 \u2014 \u0431\u0435\u0433\u0443\u0449\u0438\u0435 \u0432\u043E\u043B\u043D\u044B, \u043E\u0431\u0440\u0430\u0437\u0443\u044E\u0449\u0438\u0435\u0441\u044F \u0432 \u0430\u0442\u043C\u043E\u0441\u0444\u0435\u0440\u0430\u0445 \u043F\u043B\u0430\u043D\u0435\u0442 \u0438 \u0432 \u043E\u043A\u0435\u0430\u043D\u0430\u0445 \u0432 \u0443\u043C\u0435\u0440\u0435\u043D\u043D\u044B\u0445 \u0448\u0438\u0440\u043E\u0442\u0430\u0445."@ru . . . . . "Tonnta Rossby"@ga . . . . "Las ondas de Rossby barotr\u00F3picas, denominadas as\u00ED por Carl-Gustaf Rossby que las identific\u00F3 en 1939, son oscilaciones que se producen en los fluidos geof\u00EDsicos (oc\u00E9ano y atm\u00F3sfera) y que tienen su origen en el principio de conservaci\u00F3n de la .\u200B La propagaci\u00F3n de la fase de las ondas de Rossby es siempre hacia el oeste aun cuando la energ\u00EDa (velocidad de grupo) puede ser hacia el este (ondas cortas) o el oeste (ondas largas). Las ondas de Rossby se conocen tambi\u00E9n en geof\u00EDsica como ondas planetarias."@es . . . "Fale Rossby\u2019ego"@pl . . . "Rossbyv\u00E5g"@sv . "\u0623\u0645\u0648\u0627\u062C \u0631\u0648\u0633\u0628\u064A"@ar . "Onde de Rossby"@fr . . . "Ondas de Rossby (ou planet\u00E1rias) s\u00E3o meandros gigantes nas correntes de fluidos de propor\u00E7\u00E3o planet\u00E1ria. Em atmosferas planet\u00E1rias, as ondas de Rossby formam-se devido a varia\u00E7\u00E3o do efeito Coriolis com a latitude. Estas ondas foram primeiramente identificadas na atmosfera terrestre em 1939 por , que passou a explicar o seu movimento. As ondas de Rossby s\u00E3o um subconjunto das ."@pt . . . . "\u7F57\u65AF\u8D1D\u6CE2"@zh . . . . "Tonnta ar sc\u00E1la domhanda a bhaineann leis an scairdsruth sa d\u00E1 leathsf\u00E9ar, ainmnithe as an meit\u00E9areola\u00ED Sualannach-Mheirice\u00E1nach C. G. Rossby (1898-1957). De thoradh rothl\u00FA an Domhain f\u00E9in (a chuilitheacht), athr\u00FA fh\u00F3rsa Coriolis le domhanleithead, sraontar na scairdsruthanna, a bh\u00EDonn aniar sa d\u00E1 leathsf\u00E9ar, \u00F3 thuaidh i dtreo an Mhoil oiread ar leith, agus ansin \u00F3 dheas i dtreo an mhe\u00E1nchiorcail. Tarla\u00EDonn an t-athr\u00FA treo seo sa sraonadh 3-5 bhabhta is an scairdsruth ag timpeall\u00FA an Domhain."@ga . "Onda de Rossby"@pt . "Rossby-Wellen, auch als planetarische Wellen bezeichnet, sind gro\u00DFr\u00E4umige Wellenbewegungen im Ozean oder der Erdatmosph\u00E4re. Das den planetaren Wellen zugrunde liegende physikalische Prinzip ist die Erhaltung der potentiellen Vortizit\u00E4t. Wenn ein Fl\u00FCssigkeitsteilchen in der Luft oder dem Wasser an der Oberfl\u00E4che einer rotierenden Kugel nicht parallel zur Rotationsachse verschoben wird, wird es durch die Coriolisbeschleunigung abgelenkt, deren Parameter von der geografischen Breite abh\u00E4ngt. Die sich \u00E4ndernde potentielle Vortizit\u00E4t ruft eine r\u00FCckstellende Kraft hervor, die proportional zur Verschiebung aus der Ausgangslage des Teilchens ist. Dies f\u00FChrt zu einer meridionalen Schwingung mit einer westw\u00E4rts gerichteten Phasengeschwindigkeit. Sydney Samuel Hough formulierte 1897 als erster die Gleichungen f\u00FCr die Bewegung planetarer Wellen auf einer rotierenden Kugel und diskutierte die L\u00F6sungen in sph\u00E4rischen Koordinaten. Benannt werden die Wellen nach Carl-Gustaf Rossby, der f\u00FCr das Problem eine N\u00E4herungsl\u00F6sung in kartesischen Koordinaten entwickelte."@de . . . . . . "Onda de Rossby"@es . . "\u0412\u043E\u043B\u043D\u044B \u0420\u043E\u0301\u0441\u0441\u0431\u0438 \u2014 \u0431\u0435\u0433\u0443\u0449\u0438\u0435 \u0432\u043E\u043B\u043D\u044B, \u043E\u0431\u0440\u0430\u0437\u0443\u044E\u0449\u0438\u0435\u0441\u044F \u0432 \u0430\u0442\u043C\u043E\u0441\u0444\u0435\u0440\u0430\u0445 \u043F\u043B\u0430\u043D\u0435\u0442 \u0438 \u0432 \u043E\u043A\u0435\u0430\u043D\u0430\u0445 \u0432 \u0443\u043C\u0435\u0440\u0435\u043D\u043D\u044B\u0445 \u0448\u0438\u0440\u043E\u0442\u0430\u0445."@ru . . . "\u5929\u6C14\u56FE\u4E0A\u7684\u5BF9\u6D41\u5C42\u4E2D\u4E0A\u5C42\u5448\u6CE2\u72B6\u5F62\u5F0F\u7684\u6C14\u538B\u573A\u6216\u6D41\u573A\u4E2D\uFF0C\u5728\u5317\u534A\u7403\u4F1A\u67093~5\u4E2A\u6CE2\uFF0C\u8FD9\u79CD\u6CE2\u5373\u5927\u6C14\u957F\u6CE2\u3002\u7531\u4E8E\u5176\u6C34\u5E73\u5C3A\u5EA6\u4E0E\u5730\u7403\u534A\u5F84\u76F8\u5F53\uFF0C\u4E5F\u79F0\u884C\u661F\u6CE2\uFF08planetary waves\uFF09\u30021939\u5E74\uFF0C\u5361\u5C14-\u53E4\u65AF\u5854\u592B\u00B7\u7F57\u65AF\u8D1D\u9996\u5148\u4ECE\u7406\u8BBA\u4E0A\u7814\u7A76\u4E86\u5176\u6027\u8D28\uFF0C\u5E76\u505A\u51FA\u5353\u8D8A\u8D21\u732E\uFF0C\u540E\u4E16\u4E3A\u4E86\u7EAA\u5FF5\u4ED6\u6240\u5EFA\u7ACB\u7684\u5927\u6C14\u957F\u6CE2\u7406\u8BBA\uFF0C\u800C\u79F0\u5927\u6C14\u957F\u6CE2\u4E3A\u7F57\u65AF\u8D1D\u6CE2\u3002 \u7F57\u65AF\u8D1D\u6CE2\u6CE2\u901F\u4E0E\u98CE\u901F\u76F8\u5F53\uFF0C\u91CF\u7EA7\u572810m/s\uFF0C\u4F20\u64AD\u5177\u6709\u51C6\u6C34\u5E73\u3001\u65E0\u7684\u7279\u70B9\uFF0C\u5C5E\u4E8E\u6DA1\u65CB\u6027\u6162\u6CE2\u3002\u5927\u5C3A\u5EA6\u5929\u6C14\u8FC7\u7A0B\u4E0E\u5927\u6C14\u957F\u6CE2\u5173\u7CFB\u5341\u5206\u5BC6\u5207\uFF0C\u6240\u4EE5\u7F57\u65AF\u8D1D\u6CE2\u5728\u5927\u5C3A\u5EA6\u6C14\u8C61\u7814\u7A76\u4E2D\uFF0C\u5360\u6709\u5341\u5206\u91CD\u8981\u7684\u5730\u4F4D\u3002 \u7F57\u65AF\u8D1D\u6CE2\u7684\u5F62\u6210\uFF0C\u4E0E\u5730\u8F6C\u53C2\u6570\u968F\u7EAC\u5EA6\u7684\u53D8\u5316\u6709\u5173\uFF0C\u5373\u03B2\u6548\u5E94\uFF08, or simply beta\uFF09\u6240\u5F15\u8D77\u3002"@zh . . . . "\u0623\u0645\u0648\u0627\u062C \u0631\u0648\u0633\u0628\u064A (\u0628\u0627\u0644\u0625\u0646\u063A\u0648\u0634\u064A\u0629: Rossby wave) \u0647\u064A \u062A\u0644\u0643 \u0627\u0644\u0623\u0645\u0648\u0627\u062C \u0627\u0644\u0628\u0627\u0644\u063A \u0639\u062F\u062F\u0647\u0627 3-6 \u0623\u0645\u0648\u0627\u062C \u0627\u0644\u062A\u064A \u062A\u062A\u0634\u0643\u0644 \u0641\u064A \u0627\u0644\u0631\u064A\u0627\u062D \u0627\u0644\u063A\u0631\u0628\u064A\u0629 \u0627\u0644\u0639\u0644\u0648\u064A\u0629 \u0630\u0627\u062A \u0627\u0644\u062D\u0631\u0643\u0629 \u0627\u0644\u0645\u0648\u062C\u064A\u0629\u060C \u0648\u0642\u062F \u0633\u0645\u064A\u062A \u062A\u0644\u0643 \u0627\u0644\u0623\u0645\u0648\u0627\u062C \u0628\u0623\u0645\u0648\u0627\u062C \u0631\u0648\u0633\u0628\u064A \u0646\u0633\u0628\u0629 \u0625\u0644\u0649 \u0645\u0643\u062A\u0634\u0641 \u0627\u0644\u062D\u0631\u0643\u0629 \u0627\u0644\u0631\u064A\u062D\u064A\u0629 \u0627\u0644\u0639\u0644\u064A\u0627 \u0627\u0644\u0645\u0648\u062C\u064A\u0629 \u0648\u0647\u0648 \u0639\u0627\u0644\u0645 \u0627\u0644\u0623\u0631\u0635\u0627\u062F \u0627\u0644\u0633\u0648\u064A\u062F\u064A \u0643\u0627\u0631\u0644 \u062C\u0648\u0633\u062A\u0627\u0641 \u0631\u0648\u0633\u0628\u064A."@ar . . . . "\u0425\u0432\u0438\u043B\u0456 \u0420\u043E\u0301\u0441\u0441\u0431\u0456 (\u0430\u043D\u0433\u043B. Rossby waves) \u0430\u0431\u043E \u043F\u043B\u0430\u043D\u0435\u0442\u0430\u0301\u0440\u043D\u0456 \u0445\u0432\u0438\u0301\u043B\u0456 (\u0430\u043D\u0433\u043B. planetary waves) \u2014 \u043D\u0438\u0437\u044C\u043A\u043E\u0447\u0430\u0441\u0442\u043E\u0442\u043D\u0456, \u043F\u0435\u0440\u0435\u0432\u0430\u0436\u043D\u043E \u0433\u043E\u0440\u0438\u0437\u043E\u043D\u0442\u0430\u043B\u044C\u043D\u0456 \u0445\u0432\u0438\u043B\u0435\u043F\u043E\u0434\u0456\u0431\u043D\u0456 \u0440\u0443\u0445\u0438, \u0449\u043E \u0443\u0442\u0432\u043E\u0440\u044E\u044E\u0442\u044C\u0441\u044F \u0432 \u0430\u0442\u043C\u043E\u0441\u0444\u0435\u0440\u0430\u0445 \u043F\u043B\u0430\u043D\u0435\u0442 \u0442\u0430 \u0432 \u043E\u043A\u0435\u0430\u043D\u0430\u0445 \u0443 \u043F\u043E\u043C\u0456\u0440\u043D\u0438\u0445 \u0448\u0438\u0440\u043E\u0442\u0430\u0445, \u043E\u0431\u0443\u043C\u043E\u0432\u043B\u0435\u043D\u0456 \u043E\u0431\u0435\u0440\u0442\u0430\u043D\u043D\u044F\u043C \u0442\u0430 \u0441\u0444\u0435\u0440\u0438\u0447\u043D\u0456\u0441\u0442\u044E \u043F\u043B\u0430\u043D\u0435\u0442\u0438. \u041F\u0440\u043E\u044F\u0432\u043B\u044F\u044E\u0442\u044C\u0441\u044F \u0443 \u0432\u0438\u0433\u043B\u044F\u0434\u0456 \u0440\u0443\u0445\u043E\u043C\u0438\u0445 \u0441\u0438\u0441\u0442\u0435\u043C \u0442\u0435\u0447\u0456\u0439. \u041D\u0430\u0437\u0432\u0430\u043D\u0456 \u0456\u043C\u0435\u043D\u0435\u043C \u0448\u0432\u0435\u0434\u0441\u044C\u043A\u043E\u0433\u043E \u0433\u0435\u043E\u0444\u0456\u0437\u0438\u043A\u0430 \u041A.-\u0413. \u0420\u043E\u0441\u0441\u0431\u0456 (1898\u20141957), \u044F\u043A\u0438\u0439 \u0432\u0438\u044F\u0432\u0438\u0432 \u0446\u0456 \u0445\u0432\u0438\u043B\u0456 \u0432 \u0430\u0442\u043C\u043E\u0441\u0444\u0435\u0440\u0456 \u0417\u0435\u043C\u043B\u0456. \u0426\u0456 \u0445\u0432\u0438\u043B\u0456 \u0433\u0440\u0430\u044E\u0442\u044C \u0456\u0441\u0442\u043E\u0442\u043D\u0443 \u0440\u043E\u043B\u044C \u0443 \u043F\u0435\u0440\u0435\u043D\u0435\u0441\u0435\u043D\u043D\u0456 \u0442\u0435\u043F\u043B\u0430 \u0432\u0456\u0434 \u0435\u043A\u0432\u0430\u0442\u043E\u0440\u0456\u0430\u043B\u044C\u043D\u0438\u0445 \u0434\u043E \u043F\u043E\u043B\u044F\u0440\u043D\u0438\u0445 \u043E\u0431\u043B\u0430\u0441\u0442\u0435\u0439 \u0417\u0435\u043C\u043B\u0456."@uk . "Rossbyho vlna je v\u00FDb\u011B\u017Eek tekutiny, kter\u00FD vznik\u00E1 v atmosf\u00E9\u0159e \u010Di v oce\u00E1nu - obecn\u011B na planet\u00E1ch, pochopiteln\u011B a p\u0159edev\u0161\u00EDm v\u010Detn\u011B Zem\u011B. Poprv\u00E9 ji v atmosf\u00E9\u0159e popsal Carl-Gustav Arvid Rossby roku 1939. Jsou d\u016Fsledkem zachov\u00E1n\u00ED vorticity potenci\u00E1lu a ovliv\u0148ov\u00E1ny Coriolisovou silou. Rossbyho vlny jsou dob\u0159e pozorovateln\u00E9 na tzv. tryskov\u00E9m proud\u011Bn\u00ED."@cs . . . . . . "1120501933"^^ . . . . "\u0425\u0432\u0438\u043B\u0456 \u0420\u043E\u0441\u0441\u0431\u0456"@uk . . . . . "\u0425\u0432\u0438\u043B\u0456 \u0420\u043E\u0301\u0441\u0441\u0431\u0456 (\u0430\u043D\u0433\u043B. Rossby waves) \u0430\u0431\u043E \u043F\u043B\u0430\u043D\u0435\u0442\u0430\u0301\u0440\u043D\u0456 \u0445\u0432\u0438\u0301\u043B\u0456 (\u0430\u043D\u0433\u043B. planetary waves) \u2014 \u043D\u0438\u0437\u044C\u043A\u043E\u0447\u0430\u0441\u0442\u043E\u0442\u043D\u0456, \u043F\u0435\u0440\u0435\u0432\u0430\u0436\u043D\u043E \u0433\u043E\u0440\u0438\u0437\u043E\u043D\u0442\u0430\u043B\u044C\u043D\u0456 \u0445\u0432\u0438\u043B\u0435\u043F\u043E\u0434\u0456\u0431\u043D\u0456 \u0440\u0443\u0445\u0438, \u0449\u043E \u0443\u0442\u0432\u043E\u0440\u044E\u044E\u0442\u044C\u0441\u044F \u0432 \u0430\u0442\u043C\u043E\u0441\u0444\u0435\u0440\u0430\u0445 \u043F\u043B\u0430\u043D\u0435\u0442 \u0442\u0430 \u0432 \u043E\u043A\u0435\u0430\u043D\u0430\u0445 \u0443 \u043F\u043E\u043C\u0456\u0440\u043D\u0438\u0445 \u0448\u0438\u0440\u043E\u0442\u0430\u0445, \u043E\u0431\u0443\u043C\u043E\u0432\u043B\u0435\u043D\u0456 \u043E\u0431\u0435\u0440\u0442\u0430\u043D\u043D\u044F\u043C \u0442\u0430 \u0441\u0444\u0435\u0440\u0438\u0447\u043D\u0456\u0441\u0442\u044E \u043F\u043B\u0430\u043D\u0435\u0442\u0438. \u041F\u0440\u043E\u044F\u0432\u043B\u044F\u044E\u0442\u044C\u0441\u044F \u0443 \u0432\u0438\u0433\u043B\u044F\u0434\u0456 \u0440\u0443\u0445\u043E\u043C\u0438\u0445 \u0441\u0438\u0441\u0442\u0435\u043C \u0442\u0435\u0447\u0456\u0439. \u041D\u0430\u0437\u0432\u0430\u043D\u0456 \u0456\u043C\u0435\u043D\u0435\u043C \u0448\u0432\u0435\u0434\u0441\u044C\u043A\u043E\u0433\u043E \u0433\u0435\u043E\u0444\u0456\u0437\u0438\u043A\u0430 \u041A.-\u0413. \u0420\u043E\u0441\u0441\u0431\u0456 (1898\u20141957), \u044F\u043A\u0438\u0439 \u0432\u0438\u044F\u0432\u0438\u0432 \u0446\u0456 \u0445\u0432\u0438\u043B\u0456 \u0432 \u0430\u0442\u043C\u043E\u0441\u0444\u0435\u0440\u0456 \u0417\u0435\u043C\u043B\u0456. \u0426\u0456 \u0445\u0432\u0438\u043B\u0456 \u0433\u0440\u0430\u044E\u0442\u044C \u0456\u0441\u0442\u043E\u0442\u043D\u0443 \u0440\u043E\u043B\u044C \u0443 \u043F\u0435\u0440\u0435\u043D\u0435\u0441\u0435\u043D\u043D\u0456 \u0442\u0435\u043F\u043B\u0430 \u0432\u0456\u0434 \u0435\u043A\u0432\u0430\u0442\u043E\u0440\u0456\u0430\u043B\u044C\u043D\u0438\u0445 \u0434\u043E \u043F\u043E\u043B\u044F\u0440\u043D\u0438\u0445 \u043E\u0431\u043B\u0430\u0441\u0442\u0435\u0439 \u0417\u0435\u043C\u043B\u0456."@uk . . . . . "\u5929\u6C14\u56FE\u4E0A\u7684\u5BF9\u6D41\u5C42\u4E2D\u4E0A\u5C42\u5448\u6CE2\u72B6\u5F62\u5F0F\u7684\u6C14\u538B\u573A\u6216\u6D41\u573A\u4E2D\uFF0C\u5728\u5317\u534A\u7403\u4F1A\u67093~5\u4E2A\u6CE2\uFF0C\u8FD9\u79CD\u6CE2\u5373\u5927\u6C14\u957F\u6CE2\u3002\u7531\u4E8E\u5176\u6C34\u5E73\u5C3A\u5EA6\u4E0E\u5730\u7403\u534A\u5F84\u76F8\u5F53\uFF0C\u4E5F\u79F0\u884C\u661F\u6CE2\uFF08planetary waves\uFF09\u30021939\u5E74\uFF0C\u5361\u5C14-\u53E4\u65AF\u5854\u592B\u00B7\u7F57\u65AF\u8D1D\u9996\u5148\u4ECE\u7406\u8BBA\u4E0A\u7814\u7A76\u4E86\u5176\u6027\u8D28\uFF0C\u5E76\u505A\u51FA\u5353\u8D8A\u8D21\u732E\uFF0C\u540E\u4E16\u4E3A\u4E86\u7EAA\u5FF5\u4ED6\u6240\u5EFA\u7ACB\u7684\u5927\u6C14\u957F\u6CE2\u7406\u8BBA\uFF0C\u800C\u79F0\u5927\u6C14\u957F\u6CE2\u4E3A\u7F57\u65AF\u8D1D\u6CE2\u3002 \u7F57\u65AF\u8D1D\u6CE2\u6CE2\u901F\u4E0E\u98CE\u901F\u76F8\u5F53\uFF0C\u91CF\u7EA7\u572810m/s\uFF0C\u4F20\u64AD\u5177\u6709\u51C6\u6C34\u5E73\u3001\u65E0\u7684\u7279\u70B9\uFF0C\u5C5E\u4E8E\u6DA1\u65CB\u6027\u6162\u6CE2\u3002\u5927\u5C3A\u5EA6\u5929\u6C14\u8FC7\u7A0B\u4E0E\u5927\u6C14\u957F\u6CE2\u5173\u7CFB\u5341\u5206\u5BC6\u5207\uFF0C\u6240\u4EE5\u7F57\u65AF\u8D1D\u6CE2\u5728\u5927\u5C3A\u5EA6\u6C14\u8C61\u7814\u7A76\u4E2D\uFF0C\u5360\u6709\u5341\u5206\u91CD\u8981\u7684\u5730\u4F4D\u3002 \u7F57\u65AF\u8D1D\u6CE2\u7684\u5F62\u6210\uFF0C\u4E0E\u5730\u8F6C\u53C2\u6570\u968F\u7EAC\u5EA6\u7684\u53D8\u5316\u6709\u5173\uFF0C\u5373\u03B2\u6548\u5E94\uFF08, or simply beta\uFF09\u6240\u5F15\u8D77\u3002"@zh . . "Fale Rossby\u2019ego (fale planetarne, ang. Rossby waves) \u2013 fale zwi\u0105zane z ruchem wielkoskalowym w atmosferze lub oceanie. Ich dynamika zwi\u0105zana jest ze zmian\u0105 si\u0142y Coriolisa wraz z szeroko\u015Bci\u0105 geograficzn\u0105."@pl . . . . . . "Onda di Rossby"@it . . . . . . . . . . . . . . "Fale Rossby\u2019ego (fale planetarne, ang. Rossby waves) \u2013 fale zwi\u0105zane z ruchem wielkoskalowym w atmosferze lub oceanie. Ich dynamika zwi\u0105zana jest ze zmian\u0105 si\u0142y Coriolisa wraz z szeroko\u015Bci\u0105 geograficzn\u0105."@pl . . . . . . . . "Gelombang Rossby"@in . . "En Rossbyv\u00E5g eller planetarisk v\u00E5g \u00E4r en storskalig v\u00E5g mellan tv\u00E5 n\u00E4stan parallella skikt som \u00E4r n\u00E4stan vinkelr\u00E4ta mot en rotationsaxel. Rossbyv\u00E5gor upptr\u00E4der i jordens atmosf\u00E4r och i haven d\u00E4r de bildas genom Corioliseffektens variationer p\u00E5 olika latituder. Deras l\u00E4ngd kan uppg\u00E5 till omkring 5\u201310 000 kilometer. Rossbyv\u00E5gor i atmosf\u00E4ren beskrevs och f\u00F6rklarades f\u00F6rsta g\u00E5ngen 1939 av Carl-Gustaf Rossby. Barotropiska Rossbyv\u00E5gor, som fortplantar sig snabbast, och baroklina Rossbyv\u00E5gor, som bara r\u00F6r sig med n\u00E5gra centimeter per sekund eller mindre, har olika vertikal struktur."@sv . "\u0623\u0645\u0648\u0627\u062C \u0631\u0648\u0633\u0628\u064A (\u0628\u0627\u0644\u0625\u0646\u063A\u0648\u0634\u064A\u0629: Rossby wave) \u0647\u064A \u062A\u0644\u0643 \u0627\u0644\u0623\u0645\u0648\u0627\u062C \u0627\u0644\u0628\u0627\u0644\u063A \u0639\u062F\u062F\u0647\u0627 3-6 \u0623\u0645\u0648\u0627\u062C \u0627\u0644\u062A\u064A \u062A\u062A\u0634\u0643\u0644 \u0641\u064A \u0627\u0644\u0631\u064A\u0627\u062D \u0627\u0644\u063A\u0631\u0628\u064A\u0629 \u0627\u0644\u0639\u0644\u0648\u064A\u0629 \u0630\u0627\u062A \u0627\u0644\u062D\u0631\u0643\u0629 \u0627\u0644\u0645\u0648\u062C\u064A\u0629\u060C \u0648\u0642\u062F \u0633\u0645\u064A\u062A \u062A\u0644\u0643 \u0627\u0644\u0623\u0645\u0648\u0627\u062C \u0628\u0623\u0645\u0648\u0627\u062C \u0631\u0648\u0633\u0628\u064A \u0646\u0633\u0628\u0629 \u0625\u0644\u0649 \u0645\u0643\u062A\u0634\u0641 \u0627\u0644\u062D\u0631\u0643\u0629 \u0627\u0644\u0631\u064A\u062D\u064A\u0629 \u0627\u0644\u0639\u0644\u064A\u0627 \u0627\u0644\u0645\u0648\u062C\u064A\u0629 \u0648\u0647\u0648 \u0639\u0627\u0644\u0645 \u0627\u0644\u0623\u0631\u0635\u0627\u062F \u0627\u0644\u0633\u0648\u064A\u062F\u064A \u0643\u0627\u0631\u0644 \u062C\u0648\u0633\u062A\u0627\u0641 \u0631\u0648\u0633\u0628\u064A."@ar . . . . . . "Gelombang Rossby merupakan sebuah fenomena alam yang terjadi pada lapisan atmosfer yang dapat mengindikasikan adanya potensi berkumpulnya awan hujan dengan skala yang lebih luas. Nama gelombang ini diambil dari , orang yang pertama kali mengidentifikasi dan memahami pergerakan gelombang tersebut. Biasanya awan hujan ini berkumpul di wilayah yang dilewatinya. Gelombang ini terbentuk ketika udara di kutub bergerak menuju khatulistiwa dan bertemu dengan udara tropis yang bergerak ke arah kutub. Perbedaan suhu antara hangatnya udara tropis dan dinginnya udara kutub, serta perbedaan jumlah radiasi matahari yang diterima membuat udara panas cenderung bergerak dari lintang rendah ke lintang yang lebih tinggi. Gelombang ini disebut juga gelombang planet karena pergerakannya yang secara alami memutari permukaan atmosfer Bumi. Gelombang ini juga terjadi karena adanya rotasi Bumi."@in . . "En Rossbyv\u00E5g eller planetarisk v\u00E5g \u00E4r en storskalig v\u00E5g mellan tv\u00E5 n\u00E4stan parallella skikt som \u00E4r n\u00E4stan vinkelr\u00E4ta mot en rotationsaxel. Rossbyv\u00E5gor upptr\u00E4der i jordens atmosf\u00E4r och i haven d\u00E4r de bildas genom Corioliseffektens variationer p\u00E5 olika latituder. Deras l\u00E4ngd kan uppg\u00E5 till omkring 5\u201310 000 kilometer. Rossbyv\u00E5gor i atmosf\u00E4ren beskrevs och f\u00F6rklarades f\u00F6rsta g\u00E5ngen 1939 av Carl-Gustaf Rossby. Rossbyv\u00E5gorna k\u00E4nnetecknas av att fashastigheten (v\u00E5gtopparnas hastighet) alltid \u00E4r riktad v\u00E4sterut samtidigt som deras grupphastighet (energifl\u00F6dets hastighet) kan vara riktad i vilken riktning som helst. I allm\u00E4nhet \u00E4r dock grupphastigheten hos korta v\u00E5gor riktad \u00F6sterut och hos l\u00E5nga v\u00E5gor v\u00E4sterut. Barotropiska Rossbyv\u00E5gor, som fortplantar sig snabbast, och baroklina Rossbyv\u00E5gor, som bara r\u00F6r sig med n\u00E5gra centimeter per sekund eller mindre, har olika vertikal struktur."@sv . . "Rossbyho vlna"@cs . "Gelombang Rossby merupakan sebuah fenomena alam yang terjadi pada lapisan atmosfer yang dapat mengindikasikan adanya potensi berkumpulnya awan hujan dengan skala yang lebih luas. Nama gelombang ini diambil dari , orang yang pertama kali mengidentifikasi dan memahami pergerakan gelombang tersebut. Biasanya awan hujan ini berkumpul di wilayah yang dilewatinya. Gelombang ini terbentuk ketika udara di kutub bergerak menuju khatulistiwa dan bertemu dengan udara tropis yang bergerak ke arah kutub. Perbedaan suhu antara hangatnya udara tropis dan dinginnya udara kutub, serta perbedaan jumlah radiasi matahari yang diterima membuat udara panas cenderung bergerak dari lintang rendah ke lintang yang lebih tinggi."@in . . . . . . . . "In fisica dell'atmosfera e oceanografia le onde di Rossby, dette anche onde planetarie, sono strutture che caratterizzano i moti dei fluidi geofisici a scala sinottica e planetaria. Esse si possono osservare sia in atmosfera, ad esempio nei meandri compiuti dalla corrente a getto sub-polare alle medie latitudini, sia nell'oceano, nell'evoluzione delle perturbazioni del termoclino e assumono notevole importanza in meteorologia e climatologia."@it . "Rossby wave"@en . "\uB85C\uC2A4\uBE44 \uD30C\uB3D9(Rossby wave) \uB610\uB294 \uD589\uC131\uC758 \uD30C\uB3D9\uC740 \uACE0\uC704\uB3C4 \uBC14\uB78C\uC758 \uAC70\uB300\uD55C \uAD6C\uBE44\uCE68\uC73C\uB85C \uAE30\uD6C4\uC5D0 \uC8FC\uC694\uD55C \uC601\uD5A5\uC774 \uC788\uB2E4. \uADF8\uB4E4\uC740 \uC704\uB3C4\uC5D0 \uB530\uB77C \uCF54\uB9AC\uC62C\uB9AC \uD6A8\uACFC\uB0B4\uC758 \uBCC0\uD654\uC5D0 \uB530\uB77C \uC720\uBC1C\uB41C\uB2E4. \uD30C\uB3D9\uC740 \uCC98\uC74C 1939\uB144\uC5D0 \uCE74\uB97C\uAD6C\uC2A4\uD0C0\uD504 \uB85C\uC2A4\uBE44\uC5D0 \uC758\uD574 \uD655\uC778\uB418\uC5C8\uB294\uB370 \uADF8\uB294 \uACC4\uC18D\uD558\uC5EC \uADF8\uB4E4\uC758 \uC6C0\uC9C1\uC784\uC744 \uC124\uBA85\uD558\uB824\uACE0 \uD558\uC600\uB2E4. \uB85C\uC2A4\uBE44 \uD30C\uB3D9\uC740 \uB0B4\uBD80\uD30C\uB3D9\uC758 \uBD80\uBD84\uC9D1\uD569\uC774\uB2E4. \uB85C\uC2A4\uBE44 \uD30C\uB3D9\uC758 \uD2B9\uC9D5\uC740 \uADF8 \uC704\uC0C1 \uC18D\uB3C4\uB85C \uADF8\uAC83\uC740 \uD56D\uC0C1 \uC11C\uD5A5 \uC131\uBD84\uC744 \uC9C0\uB2CC\uB2E4. \uADF8\uB7EC\uB098 \uD30C\uB3D9\uC758 \uAD70\uC18D\uB3C4\uB294 \uC5D0\uB108\uC9C0 \uD50C\uB7ED\uC2A4\uC640 \uAD00\uB828\uC788\uC73C\uBA70 \uC784\uC758\uC758 \uBC29\uD5A5\uC77C \uC218 \uC788\uB2E4. \uC77C\uBC18\uC801\uC73C\uB85C \uB354 \uC9E7\uC740 \uD30C\uB3D9\uC740 \uB3D9\uD5A5\uC758 \uAD70 \uC18D\uB3C4\uB97C \uC9C0\uB2C8\uBA70 \uAE34 \uD30C\uC7A5\uC740 \uC11C\uD5A5\uC758 \uAD70\uC18D\uB3C4\uB97C \uC9C0\uB2CC\uB2E4. \uAE30\uC555 \uB85C\uC2A4\uBE44 \uD30C\uB3D9\uC774\uB77C\uB294 \uC6A9\uC5B4\uB294 \uADF8\uB4E4\uC758 \uC218\uC9C1 \uAD6C\uC870\uB97C \uAD6C\uBD84\uD558\uAE30 \uC704\uD574 \uC0AC\uC6A9\uB41C\uB2E4. \uBC14\uB85C\uD2B8\uB85C\uD53D \uB85C\uC2A4\uBE44 \uD30C\uB3D9\uC740 \uC218\uC9C1\uC73C\uB85C\uB294 \uBCC0\uD558\uC9C0 \uC54A\uACE0 \uC81C\uC77C \uBE60\uB978 \uC804\uD30C \uC18D\uB3C4\uB97C \uC9C0\uB2CC\uB2E4. \uBC14\uB85C\uD074\uB9AC\uB2C9 \uD30C\uB3D9 \uBAA8\uB4DC\uB294 \uB354 \uB290\uB9AC\uBA70 \uCD08\uB2F9 \uC218\uC13C\uD2F0\uBBF8\uD130 \uC774\uD558\uC758 \uC18D\uB825\uC744 \uC9C0\uB2CC\uB2E4."@ko . "Rossby-golven, planetaire golven of lange golven zijn grootschalige bewegingen in hetzij oceanen, hetzij in de atmosfeer die ontstaan ten gevolge van het natuurlijk herstel van het Corioliseffect, een effect waarvan de sterkte afhankelijk is van de breedtegraad. De golven zijn in 1939 ontdekt door en sindsdien genoemd naar Carl-Gustaf Rossby."@nl . . . "Les ondes de Rossby ou ondes plan\u00E9taires sont des mouvements ondulatoires de la circulation atmosph\u00E9rique ou oc\u00E9anique de grande longueur d'onde dont l'initiation est due \u00E0 la variation de la force de Coriolis selon la latitude. Elles sont un sous-ensemble des ondes inertielles, identifi\u00E9es en 1939 par Carl-Gustaf Rossby dans l'atmosph\u00E8re. Ce dernier travailla \u00E0 la th\u00E9orie pour les expliquer."@fr . . . . . "\u30ED\u30B9\u30D3\u30FC\u6CE2"@ja . "Rossby-golven, planetaire golven of lange golven zijn grootschalige bewegingen in hetzij oceanen, hetzij in de atmosfeer die ontstaan ten gevolge van het natuurlijk herstel van het Corioliseffect, een effect waarvan de sterkte afhankelijk is van de breedtegraad. De golven zijn in 1939 ontdekt door en sindsdien genoemd naar Carl-Gustaf Rossby."@nl . . . . . . "Rossby-golf"@nl . "Rossby waves, also known as planetary waves, are a type of inertial wave naturally occurring in rotating fluids. They were first identified by Sweden-born American meteorologist Carl-Gustaf Arvid Rossby. They are observed in the atmospheres and oceans of planets owing to the rotation of the planet. Atmospheric Rossby waves on Earth are giant meanders in high-altitude winds that have a major influence on weather. These waves are associated with pressure systems and the jet stream. Oceanic Rossby waves move along the thermocline: the boundary between the warm upper layer and the cold deeper part of the ocean."@en . . . . . . "Ondas de Rossby (ou planet\u00E1rias) s\u00E3o meandros gigantes nas correntes de fluidos de propor\u00E7\u00E3o planet\u00E1ria. Em atmosferas planet\u00E1rias, as ondas de Rossby formam-se devido a varia\u00E7\u00E3o do efeito Coriolis com a latitude. Estas ondas foram primeiramente identificadas na atmosfera terrestre em 1939 por , que passou a explicar o seu movimento. As ondas de Rossby s\u00E3o um subconjunto das ."@pt . . . . . . . "438602"^^ . "\u5927\u6C17\u4E2D\u306E\u30ED\u30B9\u30D3\u30FC\u6CE2\uFF08\u30ED\u30B9\u30D3\u30FC\u306F\u3001Rossby wave\uFF09\u306F\u3001\u5927\u9678\u30FB\u6D77\u6D0B\u306E\u6E29\u5EA6\u5DEE\u3084\u5730\u5F62\u306E\u9AD8\u4F4E\u5DEE\u306A\u3069\u306B\u3088\u3063\u3066\u5927\u6C17\u304C\u63FA\u3059\u3076\u3089\u308C\u3066\u751F\u3058\u308B\u81EA\u7531\u632F\u52D5\u306E\u6CE2\u306E\u4E00\u3064\u3067\u3001\u5730\u7403\u5927\u6C17\u3001\u3067\u898B\u3089\u308C\u308B\u5927\u6C17\u6CE2\u3067\u3042\u308B\u3002\u307E\u305F\u3001\u30ED\u30B9\u30D3\u30FC\u6CE2\u306F\u3092\u3068\u3059\u308B\u6CE2\u3067\u3042\u308B\u3002\u30AB\u30FC\u30EB\uFF1D\u30B0\u30B9\u30BF\u30D5\u30FB\u30ED\u30B9\u30D3\u30FC\u306B\u3088\u3063\u3066\u767A\u898B\u3055\u308C\u305F\u3053\u3068\u304B\u3089\u3053\u306E\u540D\u304C\u3042\u308B\u3002 \u60D1\u661F\u306E\u81EA\u8EE2\u306B\u4F34\u3046\u56DE\u8EE2\u304C\u3042\u308B\u7DEF\u5EA6\u306B\u53CA\u307C\u3059\u52B9\u679C\uFF08\u60D1\u661F\u6E26\u5EA6\uFF09\u304C\u5317\u307B\u3069\u5927\u304D\u304F\uFF08\u5317\u6975\u3067\u6700\u5927\u5024\u3001\u5357\u6975\u3067\u6700\u5C0F\u5024\u3001\u8D64\u9053\u4E0A\u30670\uFF09\u3001\u4F4E\u6C17\u5727\u306E\u897F\u5074\u3067\u306F\u5317\u304B\u3089\u5357\u306B\u5927\u304D\u306A\uFF08\u4F4E\u6C17\u5727\u6027\u306E\uFF09\u60D1\u661F\u6E26\u5EA6\u304C\u3001\u6771\u5074\u3067\u306F\u5357\u304B\u3089\u5317\u306B\u5C0F\u3055\u306A\u60D1\u661F\u6E26\u5EA6\u304C\u904B\u3070\u308C\u3066\u304F\u308B\u305F\u3081\u3001\u30ED\u30B9\u30D3\u30FC\u6CE2\u306E\u4F4D\u76F8\u304C\u897F\u306B\u305A\u308C\u3001\u6771\u897F\u65B9\u5411\u3078\u306F\u4F4D\u76F8\u304C\u897F\u306B\u4F1D\u64AD\u3059\u308B\u3002\u30ED\u30B9\u30D3\u30FC\u6CE2\u306E\u30A8\u30CD\u30EB\u30AE\u30FC\u306E\u4F1D\u64AD\u306B\u4F34\u3044\u3001\u9AD8\u4F4E\u6C17\u5727\u306E\u30D1\u30BF\u30FC\u30F3\u304C\u4EA4\u4E92\u306B\u898B\u3089\u308C\u308B\u3002\u3053\u306E\u30D1\u30BF\u30FC\u30F3\u306F\u30C6\u30EC\u30B3\u30CD\u30AF\u30B7\u30E7\u30F3\u3068\u3057\u3066\u3082\u77E5\u3089\u308C\u308B\u3002 \u30C1\u30D9\u30C3\u30C8\u9AD8\u539F\u30FB\u30D2\u30DE\u30E9\u30E4\u5C71\u8108\u3084\u30ED\u30C3\u30AD\u30FC\u5C71\u8108\u306A\u3069\u306E\u5927\u898F\u6A21\u5C71\u584A\u3067\u5F37\u5236\u3055\u308C\u3066\u751F\u3058\u305F\u30ED\u30B9\u30D3\u30FC\u6CE2\u306B\u3088\u3063\u3066\u4E2D\u7DEF\u5EA6\u306E\u5927\u6C17\u306E\u6D41\u308C\u304C\u5909\u308F\u308A\u3001\u306E\u5206\u5E03\u306B\u5F71\u97FF\u3059\u308B\u3002\u307E\u305F\u3001\u5927\u898F\u6A21\u5C71\u584A\u3067\u5F37\u5236\u3055\u308C\u3066\u751F\u3058\u305F\u30ED\u30B9\u30D3\u30FC\u6CE2\u306E\u30A8\u30CD\u30EB\u30AE\u30FC\u306F\u925B\u76F4\u306B\u3082\u4F1D\u64AD\u3059\u308B\u3068\u3044\u3046\u7279\u5FB4\u3092\u6301\u3063\u3066\u3044\u308B\u305F\u3081\u3001\u5BFE\u6D41\u570F\u304B\u3089\u6210\u5C64\u570F\u306B\u4F1D\u64AD\u3057\u3001\u6210\u5C64\u570F\u3067\u7815\u6CE2\u3057\u3066\u6210\u5C64\u570F\u7A81\u7136\u6607\u6E29\u306E\u5F15\u304D\u91D1\u3068\u306A\u308B\u3068\u8003\u3048\u3089\u308C\u3066\u3044\u308B\u3002 \u8D64\u9053\u4ED8\u8FD1\u3067\u306F\u3001\u306E\u89E3\u306E1\u3064\u3068\u3057\u3066\u3001\u30ED\u30B9\u30D3\u30FC\u6CE2\u306E\u89E3\u304C\u77E5\u3089\u308C\u308B\u3002\u6D77\u6D0B\u3067\u306E\u30ED\u30B9\u30D3\u30FC\u6CE2\u306F\u6E29\u5EA6\u8E8D\u5C64\u3092\u4E0A\u4E0B\u3055\u305B\u3001\u897F\u9032\u3059\u308B\u30ED\u30B9\u30D3\u30FC\u6CE2\u3068\u6771\u9032\u3059\u308B\u30B1\u30EB\u30D3\u30F3\u6CE2\u304C\u9023\u52D5\u3057\u3066ENSO\u306E\u30B5\u30A4\u30AF\u30EB\u3092\u5F15\u304D\u8D77\u3053\u3059\u3002"@ja . "Tonnta ar sc\u00E1la domhanda a bhaineann leis an scairdsruth sa d\u00E1 leathsf\u00E9ar, ainmnithe as an meit\u00E9areola\u00ED Sualannach-Mheirice\u00E1nach C. G. Rossby (1898-1957). De thoradh rothl\u00FA an Domhain f\u00E9in (a chuilitheacht), athr\u00FA fh\u00F3rsa Coriolis le domhanleithead, sraontar na scairdsruthanna, a bh\u00EDonn aniar sa d\u00E1 leathsf\u00E9ar, \u00F3 thuaidh i dtreo an Mhoil oiread ar leith, agus ansin \u00F3 dheas i dtreo an mhe\u00E1nchiorcail. Tarla\u00EDonn an t-athr\u00FA treo seo sa sraonadh 3-5 bhabhta is an scairdsruth ag timpeall\u00FA an Domhain."@ga . "Rossby waves, also known as planetary waves, are a type of inertial wave naturally occurring in rotating fluids. They were first identified by Sweden-born American meteorologist Carl-Gustaf Arvid Rossby. They are observed in the atmospheres and oceans of planets owing to the rotation of the planet. Atmospheric Rossby waves on Earth are giant meanders in high-altitude winds that have a major influence on weather. These waves are associated with pressure systems and the jet stream. Oceanic Rossby waves move along the thermocline: the boundary between the warm upper layer and the cold deeper part of the ocean."@en . . . . . . . . "\uB85C\uC2A4\uBE44 \uD30C\uB3D9"@ko . . . . . . . "\uB85C\uC2A4\uBE44 \uD30C\uB3D9(Rossby wave) \uB610\uB294 \uD589\uC131\uC758 \uD30C\uB3D9\uC740 \uACE0\uC704\uB3C4 \uBC14\uB78C\uC758 \uAC70\uB300\uD55C \uAD6C\uBE44\uCE68\uC73C\uB85C \uAE30\uD6C4\uC5D0 \uC8FC\uC694\uD55C \uC601\uD5A5\uC774 \uC788\uB2E4. \uADF8\uB4E4\uC740 \uC704\uB3C4\uC5D0 \uB530\uB77C \uCF54\uB9AC\uC62C\uB9AC \uD6A8\uACFC\uB0B4\uC758 \uBCC0\uD654\uC5D0 \uB530\uB77C \uC720\uBC1C\uB41C\uB2E4. \uD30C\uB3D9\uC740 \uCC98\uC74C 1939\uB144\uC5D0 \uCE74\uB97C\uAD6C\uC2A4\uD0C0\uD504 \uB85C\uC2A4\uBE44\uC5D0 \uC758\uD574 \uD655\uC778\uB418\uC5C8\uB294\uB370 \uADF8\uB294 \uACC4\uC18D\uD558\uC5EC \uADF8\uB4E4\uC758 \uC6C0\uC9C1\uC784\uC744 \uC124\uBA85\uD558\uB824\uACE0 \uD558\uC600\uB2E4. \uB85C\uC2A4\uBE44 \uD30C\uB3D9\uC740 \uB0B4\uBD80\uD30C\uB3D9\uC758 \uBD80\uBD84\uC9D1\uD569\uC774\uB2E4. \uB85C\uC2A4\uBE44 \uD30C\uB3D9\uC758 \uD2B9\uC9D5\uC740 \uADF8 \uC704\uC0C1 \uC18D\uB3C4\uB85C \uADF8\uAC83\uC740 \uD56D\uC0C1 \uC11C\uD5A5 \uC131\uBD84\uC744 \uC9C0\uB2CC\uB2E4. \uADF8\uB7EC\uB098 \uD30C\uB3D9\uC758 \uAD70\uC18D\uB3C4\uB294 \uC5D0\uB108\uC9C0 \uD50C\uB7ED\uC2A4\uC640 \uAD00\uB828\uC788\uC73C\uBA70 \uC784\uC758\uC758 \uBC29\uD5A5\uC77C \uC218 \uC788\uB2E4. \uC77C\uBC18\uC801\uC73C\uB85C \uB354 \uC9E7\uC740 \uD30C\uB3D9\uC740 \uB3D9\uD5A5\uC758 \uAD70 \uC18D\uB3C4\uB97C \uC9C0\uB2C8\uBA70 \uAE34 \uD30C\uC7A5\uC740 \uC11C\uD5A5\uC758 \uAD70\uC18D\uB3C4\uB97C \uC9C0\uB2CC\uB2E4. \uAE30\uC555 \uB85C\uC2A4\uBE44 \uD30C\uB3D9\uC774\uB77C\uB294 \uC6A9\uC5B4\uB294 \uADF8\uB4E4\uC758 \uC218\uC9C1 \uAD6C\uC870\uB97C \uAD6C\uBD84\uD558\uAE30 \uC704\uD574 \uC0AC\uC6A9\uB41C\uB2E4. \uBC14\uB85C\uD2B8\uB85C\uD53D \uB85C\uC2A4\uBE44 \uD30C\uB3D9\uC740 \uC218\uC9C1\uC73C\uB85C\uB294 \uBCC0\uD558\uC9C0 \uC54A\uACE0 \uC81C\uC77C \uBE60\uB978 \uC804\uD30C \uC18D\uB3C4\uB97C \uC9C0\uB2CC\uB2E4. \uBC14\uB85C\uD074\uB9AC\uB2C9 \uD30C\uB3D9 \uBAA8\uB4DC\uB294 \uB354 \uB290\uB9AC\uBA70 \uCD08\uB2F9 \uC218\uC13C\uD2F0\uBBF8\uD130 \uC774\uD558\uC758 \uC18D\uB825\uC744 \uC9C0\uB2CC\uB2E4."@ko . "Rossby-Wellen, auch als planetarische Wellen bezeichnet, sind gro\u00DFr\u00E4umige Wellenbewegungen im Ozean oder der Erdatmosph\u00E4re. Das den planetaren Wellen zugrunde liegende physikalische Prinzip ist die Erhaltung der potentiellen Vortizit\u00E4t. Wenn ein Fl\u00FCssigkeitsteilchen in der Luft oder dem Wasser an der Oberfl\u00E4che einer rotierenden Kugel nicht parallel zur Rotationsachse verschoben wird, wird es durch die Coriolisbeschleunigung abgelenkt, deren Parameter von der geografischen Breite abh\u00E4ngt. Die sich \u00E4ndernde potentielle Vortizit\u00E4t ruft eine r\u00FCckstellende Kraft hervor, die proportional zur Verschiebung aus der Ausgangslage des Teilchens ist. Dies f\u00FChrt zu einer meridionalen Schwingung mit einer westw\u00E4rts gerichteten Phasengeschwindigkeit."@de . "19297"^^ . . "Las ondas de Rossby barotr\u00F3picas, denominadas as\u00ED por Carl-Gustaf Rossby que las identific\u00F3 en 1939, son oscilaciones que se producen en los fluidos geof\u00EDsicos (oc\u00E9ano y atm\u00F3sfera) y que tienen su origen en el principio de conservaci\u00F3n de la .\u200B La propagaci\u00F3n de la fase de las ondas de Rossby es siempre hacia el oeste aun cuando la energ\u00EDa (velocidad de grupo) puede ser hacia el este (ondas cortas) o el oeste (ondas largas). Las ondas de Rossby se conocen tambi\u00E9n en geof\u00EDsica como ondas planetarias. Estas ondas est\u00E1n relacionadas con sistemas de presi\u00F3n (diferencias de presi\u00F3n en la superficie del oc\u00E9ano) y corrientes en chorro.\u200B Las ondas de Rossby oce\u00E1nicas se desplazan por la termoclina, la frontera entre la capa superior templada y la parte fr\u00EDa profunda del oc\u00E9ano."@es . . "In fisica dell'atmosfera e oceanografia le onde di Rossby, dette anche onde planetarie, sono strutture che caratterizzano i moti dei fluidi geofisici a scala sinottica e planetaria. Esse si possono osservare sia in atmosfera, ad esempio nei meandri compiuti dalla corrente a getto sub-polare alle medie latitudini, sia nell'oceano, nell'evoluzione delle perturbazioni del termoclino e assumono notevole importanza in meteorologia e climatologia."@it . . . . . . . . "Rossby-Welle"@de . . . "Rossbyho vlna je v\u00FDb\u011B\u017Eek tekutiny, kter\u00FD vznik\u00E1 v atmosf\u00E9\u0159e \u010Di v oce\u00E1nu - obecn\u011B na planet\u00E1ch, pochopiteln\u011B a p\u0159edev\u0161\u00EDm v\u010Detn\u011B Zem\u011B. Poprv\u00E9 ji v atmosf\u00E9\u0159e popsal Carl-Gustav Arvid Rossby roku 1939. Jsou d\u016Fsledkem zachov\u00E1n\u00ED vorticity potenci\u00E1lu a ovliv\u0148ov\u00E1ny Coriolisovou silou. Rossbyho vlny jsou dob\u0159e pozorovateln\u00E9 na tzv. tryskov\u00E9m proud\u011Bn\u00ED."@cs . "\u5927\u6C17\u4E2D\u306E\u30ED\u30B9\u30D3\u30FC\u6CE2\uFF08\u30ED\u30B9\u30D3\u30FC\u306F\u3001Rossby wave\uFF09\u306F\u3001\u5927\u9678\u30FB\u6D77\u6D0B\u306E\u6E29\u5EA6\u5DEE\u3084\u5730\u5F62\u306E\u9AD8\u4F4E\u5DEE\u306A\u3069\u306B\u3088\u3063\u3066\u5927\u6C17\u304C\u63FA\u3059\u3076\u3089\u308C\u3066\u751F\u3058\u308B\u81EA\u7531\u632F\u52D5\u306E\u6CE2\u306E\u4E00\u3064\u3067\u3001\u5730\u7403\u5927\u6C17\u3001\u3067\u898B\u3089\u308C\u308B\u5927\u6C17\u6CE2\u3067\u3042\u308B\u3002\u307E\u305F\u3001\u30ED\u30B9\u30D3\u30FC\u6CE2\u306F\u3092\u3068\u3059\u308B\u6CE2\u3067\u3042\u308B\u3002\u30AB\u30FC\u30EB\uFF1D\u30B0\u30B9\u30BF\u30D5\u30FB\u30ED\u30B9\u30D3\u30FC\u306B\u3088\u3063\u3066\u767A\u898B\u3055\u308C\u305F\u3053\u3068\u304B\u3089\u3053\u306E\u540D\u304C\u3042\u308B\u3002 \u60D1\u661F\u306E\u81EA\u8EE2\u306B\u4F34\u3046\u56DE\u8EE2\u304C\u3042\u308B\u7DEF\u5EA6\u306B\u53CA\u307C\u3059\u52B9\u679C\uFF08\u60D1\u661F\u6E26\u5EA6\uFF09\u304C\u5317\u307B\u3069\u5927\u304D\u304F\uFF08\u5317\u6975\u3067\u6700\u5927\u5024\u3001\u5357\u6975\u3067\u6700\u5C0F\u5024\u3001\u8D64\u9053\u4E0A\u30670\uFF09\u3001\u4F4E\u6C17\u5727\u306E\u897F\u5074\u3067\u306F\u5317\u304B\u3089\u5357\u306B\u5927\u304D\u306A\uFF08\u4F4E\u6C17\u5727\u6027\u306E\uFF09\u60D1\u661F\u6E26\u5EA6\u304C\u3001\u6771\u5074\u3067\u306F\u5357\u304B\u3089\u5317\u306B\u5C0F\u3055\u306A\u60D1\u661F\u6E26\u5EA6\u304C\u904B\u3070\u308C\u3066\u304F\u308B\u305F\u3081\u3001\u30ED\u30B9\u30D3\u30FC\u6CE2\u306E\u4F4D\u76F8\u304C\u897F\u306B\u305A\u308C\u3001\u6771\u897F\u65B9\u5411\u3078\u306F\u4F4D\u76F8\u304C\u897F\u306B\u4F1D\u64AD\u3059\u308B\u3002\u30ED\u30B9\u30D3\u30FC\u6CE2\u306E\u30A8\u30CD\u30EB\u30AE\u30FC\u306E\u4F1D\u64AD\u306B\u4F34\u3044\u3001\u9AD8\u4F4E\u6C17\u5727\u306E\u30D1\u30BF\u30FC\u30F3\u304C\u4EA4\u4E92\u306B\u898B\u3089\u308C\u308B\u3002\u3053\u306E\u30D1\u30BF\u30FC\u30F3\u306F\u30C6\u30EC\u30B3\u30CD\u30AF\u30B7\u30E7\u30F3\u3068\u3057\u3066\u3082\u77E5\u3089\u308C\u308B\u3002 \u30C1\u30D9\u30C3\u30C8\u9AD8\u539F\u30FB\u30D2\u30DE\u30E9\u30E4\u5C71\u8108\u3084\u30ED\u30C3\u30AD\u30FC\u5C71\u8108\u306A\u3069\u306E\u5927\u898F\u6A21\u5C71\u584A\u3067\u5F37\u5236\u3055\u308C\u3066\u751F\u3058\u305F\u30ED\u30B9\u30D3\u30FC\u6CE2\u306B\u3088\u3063\u3066\u4E2D\u7DEF\u5EA6\u306E\u5927\u6C17\u306E\u6D41\u308C\u304C\u5909\u308F\u308A\u3001\u306E\u5206\u5E03\u306B\u5F71\u97FF\u3059\u308B\u3002\u307E\u305F\u3001\u5927\u898F\u6A21\u5C71\u584A\u3067\u5F37\u5236\u3055\u308C\u3066\u751F\u3058\u305F\u30ED\u30B9\u30D3\u30FC\u6CE2\u306E\u30A8\u30CD\u30EB\u30AE\u30FC\u306F\u925B\u76F4\u306B\u3082\u4F1D\u64AD\u3059\u308B\u3068\u3044\u3046\u7279\u5FB4\u3092\u6301\u3063\u3066\u3044\u308B\u305F\u3081\u3001\u5BFE\u6D41\u570F\u304B\u3089\u6210\u5C64\u570F\u306B\u4F1D\u64AD\u3057\u3001\u6210\u5C64\u570F\u3067\u7815\u6CE2\u3057\u3066\u6210\u5C64\u570F\u7A81\u7136\u6607\u6E29\u306E\u5F15\u304D\u91D1\u3068\u306A\u308B\u3068\u8003\u3048\u3089\u308C\u3066\u3044\u308B\u3002 \u6D77\u6D0B\u306B\u304A\u3044\u3066\u306F\u3001\u6D77\u5CB8\u4ED8\u8FD1\u306A\u3069\u6D77\u5E95\u306B\u52FE\u914D\u304C\u898B\u3089\u308C\u308B\u5834\u5408\u3001\u3053\u308C\u304C\u30D9\u30FC\u30BF\u52B9\u679C\u306E\u5F79\u5272\u3092\u679C\u305F\u3059\u3002\u3053\u306E\u305F\u3081\u3001\u7B49\u6DF1\u7DDA\u306B\u6CBF\u3063\u305F\u30ED\u30B9\u30D3\u30FC\u6CE2\u304C\u5B58\u5728\u3057\u3001\u6DF1\u5EA6\u306E\u4F4E\u3044\u65B9\u3092\u53F3\u624B\u5074\u306B\u898B\u308B\u3088\u3046\u306B\u9032\u884C\u3059\u308B\u3002\u7279\u306B\u3001\u6D77\u5CB8\u4ED8\u8FD1\u306E\u30ED\u30B9\u30D3\u30FC\u6CE2\u306F\u3001\u9678\u68DA\u6CE2(continental shelf wave)\u3068\u547C\u3070\u308C\u3001\u6C34\u4F4D\u306E\u6607\u964D\u3068\u3057\u3066\u89B3\u6E2C\u3055\u308C\u308B\u3002 \u8D64\u9053\u4ED8\u8FD1\u3067\u306F\u3001\u306E\u89E3\u306E1\u3064\u3068\u3057\u3066\u3001\u30ED\u30B9\u30D3\u30FC\u6CE2\u306E\u89E3\u304C\u77E5\u3089\u308C\u308B\u3002\u6D77\u6D0B\u3067\u306E\u30ED\u30B9\u30D3\u30FC\u6CE2\u306F\u6E29\u5EA6\u8E8D\u5C64\u3092\u4E0A\u4E0B\u3055\u305B\u3001\u897F\u9032\u3059\u308B\u30ED\u30B9\u30D3\u30FC\u6CE2\u3068\u6771\u9032\u3059\u308B\u30B1\u30EB\u30D3\u30F3\u6CE2\u304C\u9023\u52D5\u3057\u3066ENSO\u306E\u30B5\u30A4\u30AF\u30EB\u3092\u5F15\u304D\u8D77\u3053\u3059\u3002"@ja . . . . "\u0412\u043E\u043B\u043D\u044B \u0420\u043E\u0441\u0441\u0431\u0438"@ru . . . . . . . "Les ondes de Rossby ou ondes plan\u00E9taires sont des mouvements ondulatoires de la circulation atmosph\u00E9rique ou oc\u00E9anique de grande longueur d'onde dont l'initiation est due \u00E0 la variation de la force de Coriolis selon la latitude. Elles sont un sous-ensemble des ondes inertielles, identifi\u00E9es en 1939 par Carl-Gustaf Rossby dans l'atmosph\u00E8re. Ce dernier travailla \u00E0 la th\u00E9orie pour les expliquer."@fr . . . .