. . . . . . . . "Dwd"@cs . "sub-arktick\u00E9m"@cs . . . . . "subpol\u00E1rn\u00ED"@cs . . . . . "Dsd"@cs . . . . "subpol\u00E1rn\u00EDch oblastech"@cs . "subpol\u00E1rn\u00EDm p\u00E1su"@cs . "Dfd"@cs . . . . . "48"^^ . . . . . "Dsc"@cs . . . . "7229"^^ . "Dfc"@cs . . "subpol\u00E1rn\u00EDch"@cs . . . "subarktick\u00E9 podneb\u00ED"@cs . "Subpol\u00E1rn\u00ED podneb\u00ED"@cs . "subarktick\u00E9m"@cs . . . "Subpol\u00E1rn\u00ED podneb\u00ED"@cs . . "1017659"^^ . . . "15916966"^^ . "Dwc"@cs . . "subpol\u00E1rn\u00ED p\u00E1s"@cs . "subarktick\u00E9 klimatick\u00E9"@cs . . . . "Subpol\u00E1rn\u00ED podneb\u00ED (n\u011Bkdy subarktick\u00E9 podneb\u00ED, subpol\u00E1rn\u00ED nebo bore\u00E1ln\u00ED z\u00F3na) je typ podneb\u00ED charakteristick\u00FD dlouhou, obvykle velmi mrazivou zimou a kr\u00E1tk\u00FDm chladn\u00FDm nebo m\u00EDrn\u00FDm l\u00E9tem. Nach\u00E1z\u00ED se na velk\u00E9 \u010D\u00E1sti pevniny, mezi 50. a\u017E 70. stupn\u011Bm severn\u00ED \u0161\u00ED\u0159ky v subarktick\u00E9m p\u00E1su, daleko od p\u016Fsoben\u00ED tepl\u00FDch oce\u00E1nsk\u00FDch proud\u016F. Toto podneb\u00ED p\u0159edstavuje podle K\u00F6ppenovy klasifikace podneb\u00ED Dfc, Dwc, Dsc, Dfd, Dwd a Dsd.Na severu le\u017E\u00ED hlavn\u011B na \u00FAzem\u00ED Kanady, Skandin\u00E1vie a Ruska, kde tvo\u0159\u00ED rozhran\u00ED lesotundry a tajgy. Na jihu ale v\u00EDce ne\u017E z 90 % zab\u00EDr\u00E1 \u00FAzem\u00ED Tich\u00E9ho, Indick\u00E9ho a Atlantsk\u00E9ho oce\u00E1nu. A na zbytku plochy le\u017E\u00ED na \u010D\u00E1sti Severn\u00ED Ameriky a na n\u011Bkolika souostrov\u00EDch u Austr\u00E1lie. Subpol\u00E1rn\u00ED p\u00E1s tak\u00E9 lemuje ob\u011B pol\u00E1rn\u00ED oblasti v pruz\u00EDch \u0161irok\u00FDch kolem 1 000 km. Tyto oblasti jsou z\u00F3ny, ve kter\u00FDch se m\u00EDs\u00ED vlastnosti m\u00EDrn\u00E9ho s pol\u00E1rn\u00EDm p\u00E1sem. Lze jej tak\u00E9 klasifikovat ve velmi mal\u00FDch oblastech, ve vysok\u00FDch nadmo\u0159sk\u00FDch v\u00FD\u0161k\u00E1ch ve St\u0159edomo\u0159\u00ED, v \u00CDr\u00E1nu, T\u00E1d\u017Eikist\u00E1nu, Turecku, v severoz\u00E1padn\u00ED \u010D\u00E1sti USA (v\u00FDchodn\u00ED Washington, v\u00FDchodn\u00ED Oregon, a Idaho), kde je ozna\u010Dov\u00E1no jako Dsc se such\u00FDm tepl\u00FDm klimatem."@cs . . . . . . . . . . . . "subpol\u00E1rn\u00EDho podneb\u00ED"@cs . . . . . . "Subpol\u00E1rn\u00ED podneb\u00ED (n\u011Bkdy subarktick\u00E9 podneb\u00ED, subpol\u00E1rn\u00ED nebo bore\u00E1ln\u00ED z\u00F3na) je typ podneb\u00ED charakteristick\u00FD dlouhou, obvykle velmi mrazivou zimou a kr\u00E1tk\u00FDm chladn\u00FDm nebo m\u00EDrn\u00FDm l\u00E9tem. Nach\u00E1z\u00ED se na velk\u00E9 \u010D\u00E1sti pevniny, mezi 50. a\u017E 70. stupn\u011Bm severn\u00ED \u0161\u00ED\u0159ky v subarktick\u00E9m p\u00E1su, daleko od p\u016Fsoben\u00ED tepl\u00FDch oce\u00E1nsk\u00FDch proud\u016F."@cs . . "subarktick\u00FDch oblast\u00ED"@cs . "subpol\u00E1rn\u00EDmu podneb\u00ED"@cs . "subpol\u00E1rn\u00ED podneb\u00ED"@cs . "subarktick\u00E9"@cs . . .