{"id":573,"date":"2009-07-03T10:26:18","date_gmt":"2009-07-03T08:26:18","guid":{"rendered":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=573"},"modified":"2011-11-06T19:08:31","modified_gmt":"2011-11-06T18:08:31","slug":"zled-21-februarja-2004","status":"publish","type":"post","link":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=573","title":{"rendered":"\u00c5\u00bdled 21.februarja 2004"},"content":{"rendered":"<p style=\"text-align: justify;\">\u00c5\u00bdled je pri\u00c4\u008del nastajati v soboto 21.februarja okoli popoldneva. Okoli 1800m visoko je bila plast pozitivnih temperatur, zaradi \u00c4\u008desar se je tam sneg spremenil v de\u00c5\u00be. Pod to mejo pa je bila vse do ni\u00c5\u00bein plast negativnih temperatur, kjer je padal podhlajen de\u00c5\u00be. Zakaj je bil ravno na Zaplani in okolici najhuj\u00c5\u00a1i \u00c5\u00beled? Vzrok je v idealni nadmorski vi\u00c5\u00a1ini. Ni\u00c5\u00beje od Zaplane (npr. Ljubljanska kotlina) je ta de\u00c5\u00be \u00c5\u00bee toliko \u00c4\u008dasa padal skozi hladnej\u00c5\u00a1e plasti, da se je spreminjal v babje p\u00c5\u00a1eno (drobna okrogla ledena zrna). V Ljubljani je nekaj \u00c4\u008dasa tudi sne\u00c5\u00beilo (isto\u00c4\u008dasno na Zaplani de\u00c5\u00beevalo in zmrzovalo), saj se topel zrak iz zahoda \u00c5\u00a1e ni prerinil nad obmo\u00c4\u008dje Ljubljane (v atmosferi nad Ljubljano v nasprotju z zahodno Slovenijo ni bilo toplej\u00c5\u00a1e plasti, zato se sneg na svoji poti proti tlom ni stalil). V vi\u00c5\u00a1jih legah (okoli 1000m visoko) je v no\u00c4\u008di na 22.februar \u00c5\u00bee pihal topel jugozahodni veter, zaradi \u00c4\u008desar je tam de\u00c5\u00beevalo pri pozitivnih temperaturah.<\/p>\n<p style=\"text-align: justify;\">V soboto 21.februarja je na Zaplani de\u00c5\u00beevalo pri -4\u00c2\u00b0C, \u00c5\u00a1e posebej pa se je \u00c5\u00beled odebelil v no\u00c4\u008di na 22.februar, ob 8:00 zjutraj je bila temperatura na Zaplani -2\u00c2\u00b0C, \u00c5\u00beled pa je po meritvah dosegel debelino do 2,5cm. Posebej hudo je bilo na Zaplani zaradi sne\u00c5\u00bene odeje, na kateri je zmrzoval de\u00c5\u00be, saj so se na Zaplani sne\u00c5\u00bene poljane spremenile v prave ledene ploskve. Jugozahodnik z otoplitvijo se je sicer spu\u00c5\u00a1\u00c4\u008dal, vendar vsaj Spodnje Zaplane ni dosegel. V nedeljo 22.februarja se je temperatura dvignila do 0,4\u00c2\u00b0C, v no\u00c4\u008di na ponedeljek pa je k sre\u00c4\u008di de\u00c5\u00beevalo pri temperaturi malo nad 0\u00c2\u00b0C, zaradi \u00c4\u008desar de\u00c5\u00be ni ve\u00c4\u008d zmrzoval (najni\u00c5\u00beja temperatura pono\u00c4\u008di je bila 0,0\u00c2\u00b0C).<\/p>\n<p style=\"text-align: center;\" align=\"justify\"><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2009\/07\/zled5.jpg\" target=\"_blank\" rel=\"lightbox[573]\"><img decoding=\"async\" loading=\"lazy\" class=\"aligncenter size-thumbnail wp-image-574\" title=\"zled5\" src=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2009\/07\/zled5-130x87.jpg\" alt=\"zled5\" width=\"130\" height=\"87\" srcset=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2009\/07\/zled5-130x87.jpg 130w, http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2009\/07\/zled5.jpg 640w\" sizes=\"(max-width: 130px) 100vw, 130px\" \/><\/a><em>\u00c5\u00bdled zlasti neprijeten, ko pade na sne\u00c5\u00beno odejo in tako nastanejo prave ledene planjave.<\/em><\/p>\n<p style=\"text-align: center;\" align=\"justify\"><em><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2009\/07\/zled4.jpg\" rel=\"lightbox[573]\"><img decoding=\"async\" loading=\"lazy\" class=\"aligncenter size-thumbnail wp-image-575\" title=\"zled4\" src=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2009\/07\/zled4-88x130.jpg\" alt=\"zled4\" width=\"88\" height=\"130\" srcset=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2009\/07\/zled4-88x130.jpg 88w, http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2009\/07\/zled4.jpg 408w\" sizes=\"(max-width: 88px) 100vw, 88px\" \/><\/a><\/em><em>Poledenele stranske ceste.<\/em><\/p>\n","protected":false},"excerpt":{"rendered":"<p>\u00c5\u00bdled je pri\u00c4\u008del nastajati v soboto 21.februarja okoli popoldneva. Okoli 1800m visoko je bila plast pozitivnih temperatur, zaradi \u00c4\u008desar se je tam sneg spremenil v de\u00c5\u00be. Pod to mejo pa je bila vse do ni\u00c5\u00bein plast negativnih temperatur, kjer je padal podhlajen de\u00c5\u00be. Zakaj je bil ravno na Zaplani in okolici najhuj\u00c5\u00a1i \u00c5\u00beled? Vzrok je [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":[],"categories":[12],"tags":[],"_links":{"self":[{"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/573"}],"collection":[{"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=573"}],"version-history":[{"count":3,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/573\/revisions"}],"predecessor-version":[{"id":577,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/573\/revisions\/577"}],"wp:attachment":[{"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=573"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=573"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=573"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}