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<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#comment>	"L\u2019ombre pluviom\u00E9trique est un ph\u00E9nom\u00E8ne m\u00E9t\u00E9orologique qui se produit sur le versant d'une montagne qui n'est pas soumis au flux direct des masses d'air humide. Alors que le versant au vent de la montagne est copieusement arros\u00E9 lors de l'arriv\u00E9e de masses d'air humide menant \u00E0 la formation de nuages et de pr\u00E9cipitations, le c\u00F4t\u00E9 prot\u00E9g\u00E9 des vents reste beaucoup plus au sec car l'humidit\u00E9 atmosph\u00E9rique s'est d\u00E9j\u00E0 d\u00E9pos\u00E9e sur le versant face au vent au moment o\u00F9 la masse d'air arrive. Le ph\u00E9nom\u00E8ne est parfois li\u00E9 \u00E0 l'effet de foehn et parfois \u00E0 une s\u00E9paration entre la circulation de bas niveau et celle de haut niveau pr\u00E8s d'un relief montagneux important."@fr .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/abstract>	"Sombra de chuva (em ingl\u00EAs: rain shadow), tamb\u00E9m conhecida por Chinook ou efeito F\u00F6hn, consiste em uma \u00E1rea normalmente cercada por montanhas que apresenta \u00EDndices de precipita\u00E7\u00E3o bastante inferiores \u00E0 \u00E1rea em seu entorno."@pt .
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<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Als Regenschatten (oder auch Leew\u00FCste) bezeichnet man ein Gebiet, das auf der vom Wind abgewandten Seite (Leeseite) eines Gebirges liegt. In einem solchen Gebiet gibt es eine wesentlich geringere Niederschlagsmenge als auf der gegen\u00FCberliegenden Seite des Gebirges, der Luvseite, die meist in den Genuss von Steigungsregen gelangt."@de .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Kerala> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/New_Caledonia> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://ja.dbpedia.org/resource/\u96E8\u852D> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/abstract>	"Itzal orografikoa, euri orografikoarekin lotutako fenomeno meteorologiko bat da. Aire heze korronteek (hau da, ozeanotik datozenek) oztopo topografiko bat gainditu behar dutenean (mendilerro bat, adibidez), euren hezetasunaren zati handi bat haizealdeko zatian botatzen dute, euri moduan. Airea, jada lehorra, haizebe aldetik jaisten denean, oso lehor jaisten da eta, bere berotze ahalmen txikiagoagatik, konpresio bidez berotzen da, igo aurretik zuena baino tenperatura handiagoa hartuz. Hau da basamortu askoren arrazoia, Death Valley kasu, Ozeano Baretik hezetasuna sartzea galerazten duten Mendi Harritsuen itzal orografikoaren ondorioz."@eu .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/\u00D6sterg\u00F6tland_County> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Microclimate> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Tunisia> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Oymyakon> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Cascade_Range> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Condense> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Greater_Poland> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Cuba> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Caucasus_Mountains> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/abstract>	"Pluvombro estas seka areo sur la lofa flanko de montoj. La montoj blokas la trairon de pluv-produktantaj veterosistemoj, \u0135etante \"ombron\" de sekeco malanta\u016D si. Kiel montrite per la diagramo dekstren, la varma humida aero estas \"tirita\" per la dominantaj ventoj super monto. Tiam \u011Di densigas kaj faligas precipita\u0135on kaj la seka aero movas anta\u016Den postlasante pluvombron malanta\u016D la monto."@eo .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://ml.dbpedia.org/resource/\u0D2E\u0D34\u0D28\u0D3F\u0D34\u0D7D_\u0D2A\u0D4D\u0D30\u0D26\u0D47\u0D36\u0D02> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#label>	"\uBE44\uADF8\uB298"@ko .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Regenschaduw is het droge gebied aan de lijzijde van bergketens. Hier valt beduidend minder neerslag dan aan de loefzijde, waar juist extra stuwingsneerslag valt. Het schaduweffect is over het algemeen sterker naarmate de bergen hoger zijn. Zie het lemma f\u00F6hn voor de verklaring van het ontstaan van een regenschaduw."@nl .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Andalusia> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Owens_Valley> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Latitude> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://bn.dbpedia.org/resource/\u09AC\u09C3\u09B7\u09CD\u099F\u09BF\u099A\u09CD\u099B\u09BE\u09AF\u09BC> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://sw.dbpedia.org/resource/Kivuli_cha_mvua> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://cs.dbpedia.org/resource/Sr\u00E1\u017Ekov\u00FD_st\u00EDn> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Gotland> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://he.dbpedia.org/resource/\u05DE\u05D3\u05D1\u05E8_\u05E6\u05DC_\u05D2\u05E9\u05DD> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Southern_Ocean> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<https://global.dbpedia.org/id/4uMZu> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Municipalities_of_Norway> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Great_Basin> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/abstract>	"La sombra orogr\u00E1fica es un fen\u00F3meno meteorol\u00F3gico asociado a la precipitaci\u00F3n orogr\u00E1fica. Cuando las corrientes de aire h\u00FAmedo (verbi gratia, provenientes de un oc\u00E9ano) se ven obligadas a remontar un obst\u00E1culo topogr\u00E1fico (p. ej., una cadena monta\u00F1osa), descargan parte de su humedad en forma de lluvia en el lado de barlovento. Cuando el aire, ya seco, desciende por el lado de sotavento de la monta\u00F1a, lo hace muy seco y como consecuencia de su menor capacidad calor\u00EDfica se calienta por compresi\u00F3n alcanzando mayor temperatura que antes del ascenso. Esta es la causa de la aridez de buena parte de los desiertos, como el del valle de la Muerte, consecuencia de la sombra orogr\u00E1fica de la Sierra Nevada que impide la entrada de humedad del Pac\u00EDfico."@es .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/abstract>	"A rain shadow is an area of significantly reduced rainfall behind a mountainous region, on the side facing away from prevailing winds, known as its leeward side. Evaporated moisture from water bodies (such as oceans and large lakes) is carried by the prevailing onshore breezes towards the drier and hotter inland areas. When encountering elevated landforms, the moist air is driven upslope towards the peak, where it expands, cools, and its moisture condenses and starts to precipitate. If the landforms are tall and wide enough, most of the humidity will be lost to precipitation over the windward side (also known as the rainward side) before ever making it past the top. As the air descends the leeward side of the landforms, it is compressed and heated, producing foehn winds that absorb moisture downslope and cast a broad \"shadow\" of dry climate region behind the mountain crests. This climate typically takes the form of shrub\u2013steppe, xeric shrublands or even deserts."@en .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Continental_Divide_of_the_Americas> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/San_Joaquin_Valley> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Haleakal\u0101> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Victoria,_British_Columbia> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Geelong> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Moab> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Myrtle_beech> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Evaporation> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Akureyri> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Nor\u0027west_arch> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/File:Envisat_image_of_the_southern_Caspian_Sea_ESA223952.tiff> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Alicante_(province)> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Clermont-Ferrand> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:Short_description> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Pennines> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:For> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://ast.dbpedia.org/resource/Solombra_orogr\u00E1fica> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/File:Satellite_image_of_Bolivia_in_June_2002.jpg> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Montalegre> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Kant\u014D_Plain> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#label>	"\u96E8\u852D"@ja .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://sk.dbpedia.org/resource/Zr\u00E1\u017Ekov\u00FD_tie\u0148> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#label>	"Pluvombro"@eo .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/File:Himalaya_composite.jpg> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Zernez> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Cie\u0144 opadowy \u2013 zmniejszenie ilo\u015Bci opadu na zawietrznej stronie przeszk\u00F3d terenowych \u2013 g\u00F3r, lasu itp. Przyk\u0142adem cienia opadowego mo\u017Ce by\u0107 ma\u0142a suma opad\u00F3w na Pojezierzu Wielkopolskim (500 mm) spowodowana zatrzymywaniem opad\u00F3w na wzg\u00F3rzach Pojezierza Pomorskiego (700 mm). Wp\u0142ywa na to rze\u017Aba terenu, g\u0142\u00F3wnie wysoko\u015B\u0107 nad poziomem morza. Nad najwy\u017Cszymi wzniesieniami Pojezierza Pomorskiego nast\u0119puje skroplenie pary wodnej zawartej w powietrzu nadci\u0105gaj\u0105cym znad Atlantyku i Ba\u0142tyku. Z tego powodu obfite opady wyst\u0119puj\u0105 na p\u00F3\u0142nocno-zachodnich stokach wzniesie\u0144. Po ich przeciwnej stronie sumy opad\u00F3w s\u0105 znacznie mniejsze. Wzniesienia stanowi\u0105 bowiem os\u0142on\u0119 tych teren\u00F3w przed nap\u0142ywem wilgotnych mas powietrza przynosz\u0105cych opady."@pl .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Ridge-and-Valley_Appalachians> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Olympic_Mountains> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Southern_Alps> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/South_Swedish_highlands> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Victorian_alps> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Moisture> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Kiruna> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Windbreak> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://de.dbpedia.org/resource/Regenschatten> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Western_Cape_Province> .
<http://dbpedia.org/resource/Rain_shadow>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Ghat_satellite_view.jpg> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Beed> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Wales> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Mountain> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Limagne> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Darling_Scarp> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Peneda-Ger\u00EAs_National_Park> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Rize> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Great_Southern_(Western_Australia)> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Anatolian_Plateau> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Morocco> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Asheville> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Judaean_Desert> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Forez> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Sweden> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Appalachian_temperate_rainforest> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Sierra_Nevada> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Santa_Cruz_Mountains> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Cairns_Region> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Bakersfield,_California> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#label>	"Sr\u00E1\u017Ekov\u00FD st\u00EDn"@cs .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Rocky_Mountains> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://es.dbpedia.org/resource/Sombra_orogr\u00E1fica> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/New_Zealand> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Mongolia> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Omeo> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Baltic_Sea> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Japanese_Alps> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Ocean> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Kalmar_County> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Trade_winds> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#comment>	"\u0414\u043E\u0436\u0434\u0435\u0432\u0430\u0301\u044F \u0442\u0435\u043D\u044C \u2014 \u0440\u0435\u0433\u0438\u043E\u043D \u0441 \u043E\u0442\u043D\u043E\u0441\u0438\u0442\u0435\u043B\u044C\u043D\u043E \u043D\u0438\u0437\u043A\u0438\u043C \u043A\u043E\u043B\u0438\u0447\u0435\u0441\u0442\u0432\u043E\u043C \u0430\u0442\u043C\u043E\u0441\u0444\u0435\u0440\u043D\u044B\u0445 \u043E\u0441\u0430\u0434\u043A\u043E\u0432 \u043F\u043E \u0441\u0440\u0430\u0432\u043D\u0435\u043D\u0438\u044E \u0441 \u043E\u043A\u0440\u0443\u0436\u0430\u044E\u0449\u0435\u0439 \u043C\u0435\u0441\u0442\u043D\u043E\u0441\u0442\u044C\u044E, \u043D\u0430\u0445\u043E\u0434\u044F\u0449\u0438\u0439\u0441\u044F \u043D\u0430 \u0433\u043E\u0440\u043D\u043E\u0433\u043E \u0445\u0440\u0435\u0431\u0442\u0430 \u0438\u043B\u0438 \u0434\u0440\u0443\u0433\u043E\u0433\u043E \u0433\u0435\u043E\u0433\u0440\u0430\u0444\u0438\u0447\u0435\u0441\u043A\u043E\u0433\u043E \u043E\u0431\u044A\u0435\u043A\u0442\u0430, \u043A\u043E\u0442\u043E\u0440\u044B\u0439 \u0437\u0430\u0434\u0435\u0440\u0436\u0438\u0432\u0430\u0435\u0442 \u043F\u0440\u043E\u0434\u0432\u0438\u0436\u0435\u043D\u0438\u0435 \u0434\u043E\u0436\u0434\u0435\u0432\u044B\u0445 \u043E\u0431\u043B\u0430\u043A\u043E\u0432, \u043A\u0430\u043A \u0431\u044B \u043E\u0442\u0431\u0440\u0430\u0441\u044B\u0432\u0430\u044F \u00AB\u0441\u0443\u0445\u0443\u044E \u0442\u0435\u043D\u044C\u00BB."@ru .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#label>	"Regenschaduw"@nl .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Ethiopian_Highlands> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/File:Vista_satelital_de_la_cordillera_Cant\u00E1brica_en_toda_su_extensi\u00F3n,_se\u00F1alada_mediante_un_recuadro_rojo.jpg> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://hu.dbpedia.org/resource/Es\u0151\u00E1rny\u00E9k> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Piedmont> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#label>	"Ombra pluviometrica"@it .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Patagonian_Desert> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://th.dbpedia.org/resource/\u0E1E\u0E37\u0E49\u0E19\u0E17\u0E35\u0E48\u0E2D\u0E31\u0E1A\u0E1D\u0E19> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Cuyo_(Argentina)> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Oslo> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Apennines> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Sr\u00E1\u017Ekov\u00FD st\u00EDn je meteorologick\u00FD jev vznikl\u00FD p\u016Fsoben\u00EDm horsk\u00FDch celk\u016F, kter\u00E9 znemo\u017E\u0148uj\u00ED p\u0159en\u00E1\u0161et p\u0159evl\u00E1daj\u00EDc\u00EDm v\u011Btr\u016Fm vlhkost. Obla\u010Dnost se na n\u00E1v\u011Btrn\u00E9 stran\u011B hor zachyt\u00ED a zde tak\u00E9 spadne v\u011Bt\u0161ina sr\u00E1\u017Eek. Z\u00E1v\u011Btrn\u00E1 strana je pak podstatn\u011B su\u0161\u0161\u00ED. P\u0159\u00EDkladem sr\u00E1\u017Ekov\u00E9ho st\u00EDnu je nap\u0159\u00EDklad m\u011Bsto Lima v z\u00E1v\u011Btrn\u00E9 poloze And nebo Tibetsk\u00E1 n\u00E1horn\u00ED plo\u0161ina. V \u010Cesku je tento jev typick\u00FD pro doln\u00ED Pooh\u0159\u00ED a Pod\u0159ipsko v z\u00E1v\u011Btrn\u00E9 poloze Kru\u0161n\u00FDch hor a pro Dyjsko-svrateck\u00FD \u00FAval st\u00EDn\u011Bn\u00FD \u010Ceskomoravskou vrchovinou. Pr\u016Fm\u011Brn\u00E9 ro\u010Dn\u00ED sr\u00E1\u017Eky se v t\u011Bchto oblastech pohybuj\u00ED pod 500 mm (Tu\u0161imice 420 mm, Lib\u011Bdice 415 mm)."@cs .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Chihuahuan_Desert> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Kahoolawe> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Ridge> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Nicola_River> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Chilean_Coast_Range> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Troms\u00F8> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Australian_Capital_Territory> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Narrogin,_Western_Australia> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://ru.dbpedia.org/resource/\u0414\u043E\u0436\u0434\u0435\u0432\u0430\u044F_\u0442\u0435\u043D\u044C> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Sierra_Nevada_de_Santa_Marta> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Djibouti> .
<http://dbpedia.org/resource/Rain_shadow>	<http://purl.org/dc/terms/subject>	<http://dbpedia.org/resource/Category:Hydrology> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Sogn> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Category:Hydrology> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://no.dbpedia.org/resource/Regnskygge> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/abstract>	"\u96E8\u5F71\u6216\u96E8\u5F71\u533A\u662F\u6307\u8F83\u5C0F\u7684\u5730\u533A\uFF0C\u5982\u5C71\u8109\u7684\u5E72\u71E5\u533A\u57DF\u3002\u4F8B\u5982\uFF0C\u4E2D\u52A0\u5DDE\u4E1C\u90E8\u7684\u4F4D\u5904\u5185\u534E\u8FBE\u5C71\u8109\u7684\u96E8\u5F71\u4E2D\u3002\u800C\u5F62\u6210\u96E8\u5F71\u7684\u5730\u7406\u73B0\u8C61\u53EB\u96E8\u5F71\u6548\u5E94\u3002\u96E8\u5F71\u6548\u5E94\u51FA\u73B0\u5728\u80CC\u98CE\u5761\u3002 \u6D77\u6D0B\u7684\u6696\u6E7F\u6C14\u6D41\u88AB\u5730\u5F62\u963B\u6321\uFF0C\u8FCE\u98CE\u5761\u5F62\u6210\u5730\u5F62\u96E8\uFF1B\u56E0\u6C34\u5206\u51CF\u5C11\uFF0C\u6C14\u6D41\u4E0B\u964D\u65F6\u6C14\u6E29\u5347\u9AD8\uFF0C\u76F8\u5BF9\u6E7F\u5EA6\u964D\u4F4E\uFF0C\u56E0\u800C\u4E91\u96E8\u5C11\u89C1\uFF0C\u964D\u6C34\u91CF\u660E\u663E\u51CF\u5C11\uFF0C\u80CC\u98CE\u9762\u5F62\u6210\u96E8\u5F71\u3002\u901A\u5E38\u60C5\u51B5\u4E0B\uFF0C\u4E0B\u964D\u7684\u7A7A\u6C14\u4E5F\u4F1A\u56E0\u4E3A\u7EDD\u70ED\u538B\u7F29\u800C\u5728\u5C71\u7684\u80CC\u98CE\u9762\u53D8\u6696\u5F62\u6210\u711A\u98CE\uFF08\u5FB7\u8A9E\uFF1AF\u00F6hn\uFF09\uFF0C\u4ECE\u800C\u5438\u6536\u66F4\u591A\u6C34\u5206 \u3002"@zh .
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<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#comment>	"La sombra orogr\u00E1fica es un fen\u00F3meno meteorol\u00F3gico asociado a la precipitaci\u00F3n orogr\u00E1fica. Cuando las corrientes de aire h\u00FAmedo (verbi gratia, provenientes de un oc\u00E9ano) se ven obligadas a remontar un obst\u00E1culo topogr\u00E1fico (p. ej., una cadena monta\u00F1osa), descargan parte de su humedad en forma de lluvia en el lado de barlovento. Cuando el aire, ya seco, desciende por el lado de sotavento de la monta\u00F1a, lo hace muy seco y como consecuencia de su menor capacidad calor\u00EDfica se calienta por compresi\u00F3n alcanzando mayor temperatura que antes del ascenso."@es .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Gulf_Stream> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/abstract>	"L'ombra pluviometrica (o effetto rainshadow o anche zona a scarse precipitazioni) \u00E8 un fenomeno meteorologico che si manifesta sul versante delle montagne o di altri ostacoli geografici, opposto ai venti prevalenti. Le montagne ostruiscono il passaggio dei sistemi nuvolosi che determinano le precipitazioni, impedendo che le stesse si verifichino sul versante opposto."@it .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Prevailing_winds> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Arakan_Mountains> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Sombra de chuva (em ingl\u00EAs: rain shadow), tamb\u00E9m conhecida por Chinook ou efeito F\u00F6hn, consiste em uma \u00E1rea normalmente cercada por montanhas que apresenta \u00EDndices de precipita\u00E7\u00E3o bastante inferiores \u00E0 \u00E1rea em seu entorno."@pt .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Pluvombro estas seka areo sur la lofa flanko de montoj. La montoj blokas la trairon de pluv-produktantaj veterosistemoj, \u0135etante \"ombron\" de sekeco malanta\u016D si. Kiel montrite per la diagramo dekstren, la varma humida aero estas \"tirita\" per la dominantaj ventoj super monto. Tiam \u011Di densigas kaj faligas precipita\u0135on kaj la seka aero movas anta\u016Den postlasante pluvombron malanta\u016D la monto."@eo .
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<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#label>	"\u0414\u043E\u0436\u0434\u0435\u0432\u0430\u044F \u0442\u0435\u043D\u044C"@ru .
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<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#comment>	"\u96E8\u9670\uFF08\u3046\u3044\u3093\u3001rain shadow\uFF09\u3068\u306F\u3001\u96E8\u96F2\u3092\u542B\u3093\u3060\u98A8\u304C\u5C71\u3092\u8D8A\u3048\u308B\u969B\u306B\u3001\u98A8\u4E0A\u5074\u3067\u96E8\u304C\u964D\u308A\u3001\u98A8\u4E0B\u5074\u306F\u300C\u9670\u300D\u3068\u306A\u3063\u3066\u4E7E\u71E5\u3059\u308B\u73FE\u8C61\u3002\u7279\u306B\u3001\u98A8\u4E0B\u306B\u304A\u3044\u3066\u96E8\u91CF\u304C\u5C11\u306A\u304F\u306A\u308B\u73FE\u8C61\u3092\u6307\u3057\u3066\u300C\u96E8\u9670\u300D\u3068\u547C\u3076\u3053\u3068\u304C\u591A\u3044\u3002\u307E\u305F\u65E5\u672C\u3067\u306F\u3001\u51AC\u5B63\u306E\u592A\u5E73\u6D0B\u5074\u3067\u767A\u751F\u3059\u308B\u96E8\u9670\u306B\u3042\u305F\u308B\u73FE\u8C61\u3092\u3001\u304B\u3089\u3063\u98A8\u3068\u547C\u3076\u3002"@ja .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/abstract>	"Als Regenschatten (oder auch Leew\u00FCste) bezeichnet man ein Gebiet, das auf der vom Wind abgewandten Seite (Leeseite) eines Gebirges liegt. In einem solchen Gebiet gibt es eine wesentlich geringere Niederschlagsmenge als auf der gegen\u00FCberliegenden Seite des Gebirges, der Luvseite, die meist in den Genuss von Steigungsregen gelangt. Im Regenschatten von Gebirgen sind deswegen oft W\u00FCsten anzutreffen, die Regenschattenw\u00FCsten. Beispielsweise liegt das Hochland von Tibet im Regenschatten des Himalayagebirges, die Rangipo Desert in Neuseeland im Regenschatten der drei Vulkane Mount Ruapehu, Mount Ngauruhoe und Mount Tongariro; die Atacama, die trockenste W\u00FCste der Erde, liegt im Regenschatten der Anden."@de .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://pl.dbpedia.org/resource/Cie\u0144_opadowy> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#label>	"Sombra de chuva"@pt .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Adiabatic_process> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Vista_satelital_de_la_cordillera_Cant\u00E1brica_en_toda_su_extensi\u00F3n,_se\u00F1alada_mediante_un_recuadro_rojo.jpg> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://zh.dbpedia.org/resource/\u96E8\u5F71> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Gilgit> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#comment>	"A rain shadow is an area of significantly reduced rainfall behind a mountainous region, on the side facing away from prevailing winds, known as its leeward side. Evaporated moisture from water bodies (such as oceans and large lakes) is carried by the prevailing onshore breezes towards the drier and hotter inland areas. When encountering elevated landforms, the moist air is driven upslope towards the peak, where it expands, cools, and its moisture condenses and starts to precipitate. If the landforms are tall and wide enough, most of the humidity will be lost to precipitation over the windward side (also known as the rainward side) before ever making it past the top. As the air descends the leeward side of the landforms, it is compressed and heated, producing foehn winds that absorb moistur"@en .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Forks,_Washington> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/abstract>	"Regnskugga \u00E4r en efterf\u00F6ljd av orografisk nederb\u00F6rd.[k\u00E4lla beh\u00F6vs] Fr\u00E5n havet p\u00E5 ett bergs lovartssida f\u00F6r vindarna med sig f\u00F6r\u00E5ngat vatten. Vattnet kondenseras sedan och det resulterar i nederb\u00F6rd p\u00E5 bergets lovartssida samtidigt som luften tvingas \u00F6ver berget. P\u00E5 l\u00E4sidan sjunker sedan luften ned\u00E5t och v\u00E4rms, vilket g\u00F6r luften torr. En effekt av detta \u00E4r att omr\u00E5det p\u00E5 l\u00E4sidan om berget d\u00E5 f\u00E5r ett mycket torrare och nederb\u00F6rdsfattigare klimat."@sv .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Black_Sea> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://fr.dbpedia.org/resource/Ombre_pluviom\u00E9trique> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Okanagan_Valley> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/San_Jose,_California> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/property/wikiPageUsesTemplate>	<http://dbpedia.org/resource/Template:Citation_needed> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Sonoran_Desert> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Kuyavia> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://ca.dbpedia.org/resource/Ombra_orogr\u00E0fica> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/1999/02/22-rdf-syntax-ns#type>	<http://dbpedia.org/ontology/Place> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Hispaniola> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Landform> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Tristan_da_Cunha> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#label>	"Regenschatten"@de .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/abstract>	"Sr\u00E1\u017Ekov\u00FD st\u00EDn je meteorologick\u00FD jev vznikl\u00FD p\u016Fsoben\u00EDm horsk\u00FDch celk\u016F, kter\u00E9 znemo\u017E\u0148uj\u00ED p\u0159en\u00E1\u0161et p\u0159evl\u00E1daj\u00EDc\u00EDm v\u011Btr\u016Fm vlhkost. Obla\u010Dnost se na n\u00E1v\u011Btrn\u00E9 stran\u011B hor zachyt\u00ED a zde tak\u00E9 spadne v\u011Bt\u0161ina sr\u00E1\u017Eek. Z\u00E1v\u011Btrn\u00E1 strana je pak podstatn\u011B su\u0161\u0161\u00ED. P\u0159\u00EDkladem sr\u00E1\u017Ekov\u00E9ho st\u00EDnu je nap\u0159\u00EDklad m\u011Bsto Lima v z\u00E1v\u011Btrn\u00E9 poloze And nebo Tibetsk\u00E1 n\u00E1horn\u00ED plo\u0161ina. V \u010Cesku je tento jev typick\u00FD pro doln\u00ED Pooh\u0159\u00ED a Pod\u0159ipsko v z\u00E1v\u011Btrn\u00E9 poloze Kru\u0161n\u00FDch hor a pro Dyjsko-svrateck\u00FD \u00FAval st\u00EDn\u011Bn\u00FD \u010Ceskomoravskou vrchovinou. Pr\u016Fm\u011Brn\u00E9 ro\u010Dn\u00ED sr\u00E1\u017Eky se v t\u011Bchto oblastech pohybuj\u00ED pod 500 mm (Tu\u0161imice 420 mm, Lib\u011Bdice 415 mm)."@cs .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Skj\u00E5k> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Atacama_Desert> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#comment>	"\u0414\u043E\u0449\u043E\u0432\u0430 \u0442\u0456\u043D\u044C \u2014 \u0440\u0435\u0433\u0456\u043E\u043D \u0441\u0443\u0445\u043E\u0434\u043E\u043B\u0443 \u0456\u0437 \u043D\u0438\u0437\u044C\u043A\u043E\u044E \u043A\u0456\u043B\u044C\u043A\u0456\u0441\u0442\u044E \u043E\u043F\u0430\u0434\u0456\u0432 (\u043F\u043E\u0440\u0456\u0432\u043D\u044F\u043D\u043E \u0437 \u043D\u0430\u0432\u043A\u043E\u043B\u0438\u0448\u043D\u044C\u043E\u044E \u043C\u0456\u0441\u0446\u0435\u0432\u0456\u0441\u0442\u044E), \u0440\u043E\u0437\u0442\u0430\u0448\u043E\u0432\u0430\u043D\u0438\u0439 \u0456\u0437 \u043F\u0456\u0434\u0432\u0456\u0442\u0440\u044F\u043D\u043E\u0433\u043E \u0431\u043E\u043A\u0443 \u0433\u0456\u0440\u0441\u044C\u043A\u043E\u0433\u043E \u0445\u0440\u0435\u0431\u0442\u0430 \u0430\u0431\u043E \u0456\u043D\u0448\u043E\u0457 \u0433\u0435\u043E\u0433\u0440\u0430\u0444\u0456\u0447\u043D\u043E\u0457 \u043E\u0441\u043E\u0431\u043B\u0438\u0432\u043E\u0441\u0442\u0456, \u0449\u043E \u043E\u0431\u0443\u043C\u043E\u0432\u043B\u044E\u0454 \u043D\u0430\u043F\u0440\u044F\u043C \u0432\u0456\u0442\u0440\u0443. \u0413\u043E\u0440\u0438 \u0431\u043B\u043E\u043A\u0443\u044E\u0442\u044C \u043F\u0440\u043E\u0445\u0456\u0434 \u0434\u043E\u0449\u043E\u0432\u0438\u0445 \u043F\u043E\u0432\u0456\u0442\u0440\u044F\u043D\u0438\u0445 \u043C\u0430\u0441, \u0437\u0430\u0442\u0456\u043D\u044E\u044E\u0447\u0438 \u043F\u0440\u0438\u043B\u0435\u0433\u043B\u0456 \u0442\u0435\u0440\u0438\u0442\u043E\u0440\u0456\u0457 \u0432\u0456\u0434 \u0437\u0432\u043E\u043B\u043E\u0436\u0435\u043D\u043D\u044F, \u0449\u043E \u043F\u0440\u0438\u0437\u0432\u043E\u0434\u0438\u0442\u044C \u0434\u043E \u043F\u043E\u0441\u0443\u0445\u0438."@uk .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Adiabatic_compression> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Eastern_Washington> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#label>	"Ombre pluviom\u00E9trique"@fr .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Verkhoyansk> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#comment>	"L'ombra pluviometrica (o effetto rainshadow o anche zona a scarse precipitazioni) \u00E8 un fenomeno meteorologico che si manifesta sul versante delle montagne o di altri ostacoli geografici, opposto ai venti prevalenti. Le montagne ostruiscono il passaggio dei sistemi nuvolosi che determinano le precipitazioni, impedendo che le stesse si verifichino sul versante opposto."@it .
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<http://dbpedia.org/resource/Rain_shadow>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/The_Great_Barrier_Reef,_Australia_-_Envisat.jpg> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Gap,_Hautes-Alpes> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/North_American_Cordillera> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Sea_breeze> .
<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://pt.dbpedia.org/resource/Sombra_de_chuva> .
<http://dbpedia.org/resource/Rain_shadow>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Algeria.A2002118.1040.250m.jpg> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Dasht-i-Lut> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Humidity> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Vancouver_Island> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Szwajcaria_Kaszubska> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://xmlns.com/foaf/0.1/depiction>	<http://commons.wikimedia.org/wiki/Special:FilePath/Satellite_image_of_Bolivia_in_June_2002.jpg> .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/File:A_virtually_cloudless_image_of_Madagascar_ESA230211.jpg> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/abstract>	"\u96E8\u9670\uFF08\u3046\u3044\u3093\u3001rain shadow\uFF09\u3068\u306F\u3001\u96E8\u96F2\u3092\u542B\u3093\u3060\u98A8\u304C\u5C71\u3092\u8D8A\u3048\u308B\u969B\u306B\u3001\u98A8\u4E0A\u5074\u3067\u96E8\u304C\u964D\u308A\u3001\u98A8\u4E0B\u5074\u306F\u300C\u9670\u300D\u3068\u306A\u3063\u3066\u4E7E\u71E5\u3059\u308B\u73FE\u8C61\u3002\u7279\u306B\u3001\u98A8\u4E0B\u306B\u304A\u3044\u3066\u96E8\u91CF\u304C\u5C11\u306A\u304F\u306A\u308B\u73FE\u8C61\u3092\u6307\u3057\u3066\u300C\u96E8\u9670\u300D\u3068\u547C\u3076\u3053\u3068\u304C\u591A\u3044\u3002\u307E\u305F\u65E5\u672C\u3067\u306F\u3001\u51AC\u5B63\u306E\u592A\u5E73\u6D0B\u5074\u3067\u767A\u751F\u3059\u308B\u96E8\u9670\u306B\u3042\u305F\u308B\u73FE\u8C61\u3092\u3001\u304B\u3089\u3063\u98A8\u3068\u547C\u3076\u3002"@ja .
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<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Una ombra orogr\u00E0fica \u00E9s una zona seca situada darrere d'una muntanya o una serralada. Les muntanyes impedeixen que el vent humit arribe a aquest terreny i, en conseq\u00FC\u00E8ncia, les pluges i la vegetaci\u00F3 hi s\u00F3n escasses."@ca .
<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Category:Mountain_meteorology> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Windward> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2002/07/owl#sameAs>	<http://bg.dbpedia.org/resource/\u0412\u0430\u043B\u0435\u0436\u043D\u0430_\u0441\u044F\u043D\u043A\u0430> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/California> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#comment>	"Regnskugga \u00E4r en efterf\u00F6ljd av orografisk nederb\u00F6rd.[k\u00E4lla beh\u00F6vs] Fr\u00E5n havet p\u00E5 ett bergs lovartssida f\u00F6r vindarna med sig f\u00F6r\u00E5ngat vatten. Vattnet kondenseras sedan och det resulterar i nederb\u00F6rd p\u00E5 bergets lovartssida samtidigt som luften tvingas \u00F6ver berget. P\u00E5 l\u00E4sidan sjunker sedan luften ned\u00E5t och v\u00E4rms, vilket g\u00F6r luften torr. En effekt av detta \u00E4r att omr\u00E5det p\u00E5 l\u00E4sidan om berget d\u00E5 f\u00E5r ett mycket torrare och nederb\u00F6rdsfattigare klimat."@sv .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/abstract>	"Regenschaduw is het droge gebied aan de lijzijde van bergketens. Hier valt beduidend minder neerslag dan aan de loefzijde, waar juist extra stuwingsneerslag valt. Het schaduweffect is over het algemeen sterker naarmate de bergen hoger zijn. Zie het lemma f\u00F6hn voor de verklaring van het ontstaan van een regenschaduw. Bekende voorbeelden zijn: de Gobiwoestijn, Death Valley, de Atacamawoestijn en de Tatacoa-woestijn met een dubbele regenschaduw. Ook in West-Europa komt het verschijnsel voor, al is het minder sterk omdat de bergketens meestal niet zo hoog zijn. Zo valt er in de Elzas betrekkelijk weinig neerslag, ca. 500\u2013600 mm per jaar. Ten westen van deze streek liggen de Vogezen, die een deel van de regen uit depressies uit het westen opvangen."@nl .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/abstract>	"Cie\u0144 opadowy \u2013 zmniejszenie ilo\u015Bci opadu na zawietrznej stronie przeszk\u00F3d terenowych \u2013 g\u00F3r, lasu itp. Przyk\u0142adem cienia opadowego mo\u017Ce by\u0107 ma\u0142a suma opad\u00F3w na Pojezierzu Wielkopolskim (500 mm) spowodowana zatrzymywaniem opad\u00F3w na wzg\u00F3rzach Pojezierza Pomorskiego (700 mm). Wp\u0142ywa na to rze\u017Aba terenu, g\u0142\u00F3wnie wysoko\u015B\u0107 nad poziomem morza. Nad najwy\u017Cszymi wzniesieniami Pojezierza Pomorskiego nast\u0119puje skroplenie pary wodnej zawartej w powietrzu nadci\u0105gaj\u0105cym znad Atlantyku i Ba\u0142tyku. Z tego powodu obfite opady wyst\u0119puj\u0105 na p\u00F3\u0142nocno-zachodnich stokach wzniesie\u0144. Po ich przeciwnej stronie sumy opad\u00F3w s\u0105 znacznie mniejsze. Wzniesienia stanowi\u0105 bowiem os\u0142on\u0119 tych teren\u00F3w przed nap\u0142ywem wilgotnych mas powietrza przynosz\u0105cych opady."@pl .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Isobaric_process> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/wikiPageWikiLink>	<http://dbpedia.org/resource/Basin_and_Range_Province> .
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<http://dbpedia.org/resource/Rain_shadow>	<http://www.w3.org/2000/01/rdf-schema#label>	"Ombra orogr\u00E0fica"@ca .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/abstract>	"Una ombra orogr\u00E0fica \u00E9s una zona seca situada darrere d'una muntanya o una serralada. Les muntanyes impedeixen que el vent humit arribe a aquest terreny i, en conseq\u00FC\u00E8ncia, les pluges i la vegetaci\u00F3 hi s\u00F3n escasses."@ca .
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<http://dbpedia.org/resource/Rain_shadow>	<http://dbpedia.org/ontology/abstract>	"L\u2019ombre pluviom\u00E9trique est un ph\u00E9nom\u00E8ne m\u00E9t\u00E9orologique qui se produit sur le versant d'une montagne qui n'est pas soumis au flux direct des masses d'air humide. Alors que le versant au vent de la montagne est copieusement arros\u00E9 lors de l'arriv\u00E9e de masses d'air humide menant \u00E0 la formation de nuages et de pr\u00E9cipitations, le c\u00F4t\u00E9 prot\u00E9g\u00E9 des vents reste beaucoup plus au sec car l'humidit\u00E9 atmosph\u00E9rique s'est d\u00E9j\u00E0 d\u00E9pos\u00E9e sur le versant face au vent au moment o\u00F9 la masse d'air arrive. Le ph\u00E9nom\u00E8ne est parfois li\u00E9 \u00E0 l'effet de foehn et parfois \u00E0 une s\u00E9paration entre la circulation de bas niveau et celle de haut niveau pr\u00E8s d'un relief montagneux important. \u00AB Ombre \u00BB est employ\u00E9 par analogie parce que le versant au vent de la montagne fait \u00E9cran \u00E0 la pluie pour le versant moins arros\u00E9. L'expression est relativement r\u00E9cente (en anglais rain shadow) mais reconnue par l'Organisation m\u00E9t\u00E9orologique mondiale. Les climatologues lui pr\u00E9f\u00E8rent souvent la notion plus g\u00E9n\u00E9rale de climat d'abri, qui englobe les multiples effets, pluviom\u00E9triques et autres, que produit ce positionnement topographique."@fr .
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