{"id":756,"date":"2009-07-05T22:24:12","date_gmt":"2009-07-05T20:24:12","guid":{"rendered":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=756"},"modified":"2011-11-07T10:40:40","modified_gmt":"2011-11-07T09:40:40","slug":"zled-5-januarja-2008","status":"publish","type":"post","link":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=756","title":{"rendered":"\u00c5\u00bdled 5.januarja 2008"},"content":{"rendered":"<p style=\"text-align: justify;\">V povezavi z plitvim obmo\u00c4\u008djem nizkega zra\u00c4\u008dnega pritiska nad severnim Sredozemljem je nad Slovenijo pihal vla\u00c5\u00been in topel ju\u00c5\u00beni veter. Vi\u00c5\u00a1je lege je prevetrilo \u00c5\u00bee dan prej, napovedi so obetale dotok toplega zraka v vi\u00c5\u00a1inah, medtem ko naj bi v ni\u00c5\u00bejih legah \u00c5\u00a1e vedno vztrajal dotok hladnega zraka iz vzhoda. Ker so bile napovedane \u00c5\u00a1e padavine, je obstajala nevarnost \u00c5\u00beledenja. Napovedi pa so bile preve\u00c4\u008d optimisti\u00c4\u008dne glede hitre otoplitve. Na Zaplani se je \u00c4\u008dez dan otoplilo samo do -1,5\u00c2\u00b0C, ob\u00c4\u008dasno je rosilo. Na uradni avtomatski meteorolo\u00c5\u00a1ki postaji Otlica (965m) na robu Trnovskega gozda se je ogrelo celo do +4\u00c2\u00b0C! Padavin je bilo proti ve\u00c4\u008deru vse ve\u00c4\u008d in \u00c5\u00beled se je na Zaplani debelil. \u00c4\u0152rni Vrh je veter prevetril okoli 19:00 zve\u00c4\u008der in temperatura se je hitro dvignila. V dolo\u00c4\u008denem trenutku je bila na zasebni postaji v \u00c4\u0152rnem Vrhu temperatura +4,4\u00c2\u00b0C, na Zaplani pa isto\u00c4\u008dasno -1,2\u00c2\u00b0C. \u00c5\u00a0ele ob 1:00 zjutraj je temperatura na Zaplani dosegla ledi\u00c5\u00a1\u00c4\u008de, a jugozahodnik je zapihal \u00c5\u00a1ele ob 5:00 zjutraj. Temperatura se je ob obratu vetra hitro dvignila do +4\u00c2\u00b0C. Po nekaterih informacijah je nastal \u00c5\u00beled debeline 2cm, morda je bil kasneje ob dodatkih padavinah \u00c5\u00a1e debelej\u00c5\u00a1i. Tudi \u00c4\u008de upo\u00c5\u00a1tevamo spodnjo mejo je bil to eden debelej\u00c5\u00a1ih primerkov\u00c2\u00a0\u00c5\u00beleda v zadnjih letih in je primerljiv z \u00c5\u00beledom februarja 2004.<\/p>\n<p style=\"text-align: justify;\">Ob opisani situaciji se je zelo lepo pokazalo, kako je jugozahodnik z otoplitvijo po\u00c4\u008dasi napredoval proti Zaplani. Da je na Zaplani tako pozno zapihal veter gre zasluga stabilne temperaturne inverzije in lege v zavetrju visokih kra\u00c5\u00a1kih planot Hru\u00c5\u00a1ice in Trnovskega gozda. Prevladovali so vetrovi ju\u00c5\u00benih smeri, ob tem pa je za Zaplano zna\u00c4\u008dilno izrazito zati\u00c5\u00a1je. Dolgo \u00c4\u008dasa vztraja prizemni vzhodni veter, ki na Zaplano dovaja hladnej\u00c5\u00a1i zrak. Kako bi si sicer razlagali dejstvo, da je bilo 5.januarja zve\u00c4\u008der v Postojni +6\u00c2\u00b0C, Ilirski Bistrici +8\u00c2\u00b0C, na Babnem Polju +4\u00c2\u00b0C, Otlici in \u00c4\u0152rnem Vrhu +4\u00c2\u00b0C, a na Zaplani -1\u00c2\u00b0C?<\/p>\n","protected":false},"excerpt":{"rendered":"<p>V povezavi z plitvim obmo\u00c4\u008djem nizkega zra\u00c4\u008dnega pritiska nad severnim Sredozemljem je nad Slovenijo pihal vla\u00c5\u00been in topel ju\u00c5\u00beni veter. Vi\u00c5\u00a1je lege je prevetrilo \u00c5\u00bee dan prej, napovedi so obetale dotok toplega zraka v vi\u00c5\u00a1inah, medtem ko naj bi v ni\u00c5\u00bejih legah \u00c5\u00a1e vedno vztrajal dotok hladnega zraka iz vzhoda. Ker so bile napovedane \u00c5\u00a1e [&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\/756"}],"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=756"}],"version-history":[{"count":4,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/756\/revisions"}],"predecessor-version":[{"id":6400,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/756\/revisions\/6400"}],"wp:attachment":[{"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=756"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=756"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=756"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}