{"id":12448,"date":"2016-01-06T10:27:05","date_gmt":"2016-01-06T09:27:05","guid":{"rendered":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=12448"},"modified":"2016-01-11T15:23:44","modified_gmt":"2016-01-11T14:23:44","slug":"zled-5-januarja-2016","status":"publish","type":"post","link":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=12448","title":{"rendered":"\u00c5\u00bdled 5. januarja 2016"},"content":{"rendered":"<p style=\"text-align: justify;\">\u00c5\u00bdled ni pogost, vendar je na Zaplani zna\u00c4\u008dilen pojav. Polo\u00c5\u00beaj Zaplane ob robu Ljubljanske kotline omogo\u00c4\u008da pogosto \u00c5\u00beledne razmere ko pri tleh z vzhodnikom doteka hladen zrak, v vi\u00c5\u00a1inah pa z jugozahodnikom toplej\u00c5\u00a1i zrak. Posebnost Zaplane je v dejstvu, da ima ob \u00c5\u00beledenju pogosto ni\u00c5\u00bejo temperaturo zraka od preostalega dela Notranjske, hkrati pa se nad obmo\u00c4\u008djem Zaplane v vi\u00c5\u00a1inah \u00c5\u00a1e \u00c4\u008dutijo vplivi toplej\u00c5\u00a1ih zra\u00c4\u008dnih mas iznad Sredozemlja. Proti osrednji Sloveniji je lahko pri tleh \u00c5\u00a1e hladneje, kjer pa v vi\u00c5\u00a1inah navadno ni ve\u00c4\u008d toliko toplej\u00c5\u00a1ega zraka. Prevladuje tudi ni\u00c5\u00beja nadmorska vi\u00c5\u00a1ina in de\u00c5\u00be pogosteje zmrzne \u00c5\u00bee v ozra\u00c4\u008dju, \u00c5\u00a1e pred stikom s tlemi. S tem je \u00c5\u00beled na teh obmo\u00c4\u008djih redkej\u00c5\u00a1i.<\/p>\n<p style=\"text-align: justify;\">Sredi dneva, 5. januarja, se je pojavila za \u00c4\u008das \u00c5\u00beledenja zna\u00c4\u008dilna me\u00c5\u00a1anica padavin. Sprva je padal sneg v obliki ledenih zrn, nato obi\u00c4\u008dajen sneg in prehodno so padale velike krpe mokrega snega. Vse to je bila posledica me\u00c5\u00a1anja dveh razli\u00c4\u008dno toplih zra\u00c4\u008dnih mas v vi\u00c5\u00a1inah. Problemati\u00c4\u008dna toplej\u00c5\u00a1a plast zraka se je nahajala v vi\u00c5\u00a1inah med 700 in 1000 m. Med sneg se je pri\u00c4\u008delo vse bolj me\u00c5\u00a1ati rosenje in na Zaplani je ob stalno negativni temperaturi zraka nastajal \u00c5\u00beled. Na izpostavljenih predmetih je nastala do 0,5 cm debela ledena obloga.<\/p>\n<p>&nbsp;<\/p>\n<p style=\"text-align: center;\"><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2016\/01\/zled21.jpg\" target=\"_blank\" rel=\"attachment wp-att-12514\" rel=\"lightbox[12448]\"><img decoding=\"async\" loading=\"lazy\" class=\"aligncenter wp-image-12514\" src=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2016\/01\/zled21.jpg\" alt=\"zled21\" width=\"380\" height=\"289\" srcset=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2016\/01\/zled21.jpg 668w, http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2016\/01\/zled21-130x99.jpg 130w\" sizes=\"(max-width: 380px) 100vw, 380px\" \/><\/a><em>\u00c5\u00bdled na Spodnji Zaplani, jutro 6. januarja.<\/em><\/p>\n<p>&nbsp;<\/p>\n<p style=\"text-align: justify;\">Najve\u00c4\u008d de\u00c5\u00beja je bilo na obmo\u00c4\u008dju med Logatcem in Postojno, kjer pa se je temperatura dvignila nad ni\u00c4\u008dlo. Na Zaplani je bilo po drugi strani padavin le za vzorec, a je temperatura zaradi hladnega prizemnega vzhodnika ves \u00c4\u008das vztrajala pod ledi\u00c5\u00a1\u00c4\u008dem. V primeru obilnej\u00c5\u00a1ih padavin bi bil ledeni oklep debelej\u00c5\u00a1i.<\/p>\n<p>&nbsp;<\/p>\n<p>Dopolnjen seznam zabele\u00c5\u00beenih pojavov \u00c5\u00beledenja na Zaplani<\/p>\n<ul>\n<li><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=2644\" target=\"_blank\">7. &#8211; 9.1.1996<\/a><\/li>\n<li><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=502\" target=\"_blank\">22. &#8211; 23.12.1996 in 3.1.1997<\/a><\/li>\n<li>18. &#8211; 19.12.1997<\/li>\n<li><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=573\" target=\"_blank\">21. &#8211; 22.2.2004<\/a><\/li>\n<li><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=614\" target=\"_blank\">16. &#8211; 17.12.2004<\/a><\/li>\n<li>12.12.2005<\/li>\n<li><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=640\" target=\"_blank\">1.1.2006<\/a><\/li>\n<li><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=660\" target=\"_blank\">28. &#8211; 29.1.2006<\/a><\/li>\n<li><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/?s=%C5%BEled+2007\" target=\"_blank\">24.12.2007<\/a><\/li>\n<li><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=5327\" target=\"_blank\">5.1.2008<\/a><\/li>\n<li><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=450\" target=\"_blank\">29. in 30.11.2008<\/a><\/li>\n<li>1.1.2009<\/li>\n<li>14.1.2009<\/li>\n<li>22.12.2009<\/li>\n<li><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=3015\" target=\"_blank\">9.1.2010<\/a><\/li>\n<li>1.12.2010<\/li>\n<li>6.12.2010<\/li>\n<li><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=5327\" target=\"_blank\">13. in 16.2.2011<\/a><\/li>\n<li><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=8554\" target=\"_blank\">18.3.2013<\/a><\/li>\n<li><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=10106\" target=\"_blank\">31.1. &#8211; 5.2.2014<\/a><\/li>\n<li>27.11.2014 (nad 700 m)<\/li>\n<li>2. &#8211; 3.12.2014 (nad 700 m)<\/li>\n<li><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=12448\" target=\"_blank\">5.1.2016<\/a><\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>\u00c5\u00bdled ni pogost, vendar je na Zaplani zna\u00c4\u008dilen pojav. Polo\u00c5\u00beaj Zaplane ob robu Ljubljanske kotline omogo\u00c4\u008da pogosto \u00c5\u00beledne razmere ko pri tleh z vzhodnikom doteka hladen zrak, v vi\u00c5\u00a1inah pa z jugozahodnikom toplej\u00c5\u00a1i zrak. Posebnost Zaplane je v dejstvu, da ima ob \u00c5\u00beledenju pogosto ni\u00c5\u00bejo temperaturo zraka od preostalega dela Notranjske, hkrati pa se nad [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","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\/12448"}],"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=12448"}],"version-history":[{"count":20,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/12448\/revisions"}],"predecessor-version":[{"id":12516,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/12448\/revisions\/12516"}],"wp:attachment":[{"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=12448"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=12448"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=12448"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}