{"id":817,"date":"2009-07-06T10:39:00","date_gmt":"2009-07-06T08:39:00","guid":{"rendered":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=817"},"modified":"2009-07-06T14:08:41","modified_gmt":"2009-07-06T12:08:41","slug":"debela-snezna-odeja-v-mraziscih-spomladi-2006","status":"publish","type":"post","link":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=817","title":{"rendered":"Dolgotrajna sne\u00c5\u00bena odeja v mrazi\u00c5\u00a1\u00c4\u008dih pozimi 2005\/2006"},"content":{"rendered":"<p style=\"text-align: justify;\">Temperature v aprilu so se dan za dnem bli\u00c5\u00beale 20\u00c2\u00b0C, pono\u00c4\u008di pa zunaj mrazi\u00c5\u00a1\u00c4\u008d ni ve\u00c4\u008d zmrzovalo (zadnji\u00c4\u008d 13.aprila). 17.aprila 2006 je bilo na Zaplani \u00c5\u00bee prav pomladno vzdu\u00c5\u00a1je, na tleh je bilo veliko trobentic, snega pa \u00c5\u00bee zdavnaj ni bilo ve\u00c4\u008d. A prav neverjeten se zdi podatek, da je bilo v bli\u00c5\u00benji kra\u00c5\u00a1ki vrta\u00c4\u008di na samo 544m vi\u00c5\u00a1ine isti dan \u00c5\u00a1e vedno ve\u00c4\u008d kot 50cm snega. Sneg se v kotanji dolgo \u00c4\u008dasa obdr\u00c5\u00bei zaradi pogoste temperaturne inverzije . Sama inverzija v tej vrta\u00c4\u008di sicer ni posebno izrazita, jutranje temperature niso tako nizke kot denimo v sosednjem mrazi\u00c5\u00a1\u00c4\u008du Dolinca, a se tu zaradi zaprtosti in ve\u00c4\u008dje globine hladen zrak dr\u00c5\u00bei \u00c5\u00a1e v pozne dopoldanske ure, sneg tako ostane dolgo \u00c4\u008dasa pomrznjen, topel jugozahodni veter ob odjugah pa kotanje pogosto niti ne dose\u00c5\u00bee. Eden od vzrokov za debelo sne\u00c5\u00beno odejo v kotanji so tudi vetrovi, ki ob sne\u00c5\u00beenju v kotanjo nanosijo nekoliko ve\u00c4\u008d snega kot drugod. V nedeljo 23.aprila je bilo v kotanji kljub zelo toplemu vremenu \u00c5\u00a1e vedno 12cm snega, sne\u00c5\u00bena odeja pa je bila na tleh \u00c5\u00bee nad 150 dni. Letos je sneg kotanjo prekrival neprekinjeno skoraj pol leta, ni pa leto\u00c5\u00a1nja pomlad ni\u00c4\u008d posebnega glede tega. Spomladi 2004 je bilo ob istem \u00c4\u008dasu v mrazi\u00c5\u00a1\u00c4\u008du ve\u00c4\u008d snega kot tokrat. Tisto leto se je sneg zadr\u00c5\u00beeval po dnu kotanje \u00c5\u00a1e za prvomajske praznike, skupno \u00c5\u00a1tevilo dni s snegom je bilo pa mogo\u00c4\u008de za nekaj dni manj\u00c5\u00a1e kot letos. To je dokaz, da za trajanje snega ni pomembna le nadmorska vi\u00c5\u00a1ina, v tem primeru bi bilo najve\u00c4\u008d snega na precej vi\u00c5\u00a1ji Ulovki, ki pa po trajanju snega posameznih kra\u00c5\u00a1kih kotanj na Spodnji Zaplani \u00c5\u00a1e zdale\u00c4\u008d ne dosega.<\/p>\n<p style=\"text-align: center;\"><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2009\/07\/sneg19.jpg\" target=\"_blank\" rel=\"lightbox[817]\"><img decoding=\"async\" loading=\"lazy\" class=\"aligncenter size-thumbnail wp-image-818\" title=\"sneg19\" src=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2009\/07\/sneg19-130x97.jpg\" alt=\"sneg19\" width=\"130\" height=\"97\" srcset=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2009\/07\/sneg19-130x97.jpg 130w, http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2009\/07\/sneg19.jpg 640w\" sizes=\"(max-width: 130px) 100vw, 130px\" \/><\/a><em>Sneg v mrazi\u00c5\u00a1\u00c4\u008du ob koncu aprila 2006.<\/em><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Temperature v aprilu so se dan za dnem bli\u00c5\u00beale 20\u00c2\u00b0C, pono\u00c4\u008di pa zunaj mrazi\u00c5\u00a1\u00c4\u008d ni ve\u00c4\u008d zmrzovalo (zadnji\u00c4\u008d 13.aprila). 17.aprila 2006 je bilo na Zaplani \u00c5\u00bee prav pomladno vzdu\u00c5\u00a1je, na tleh je bilo veliko trobentic, snega pa \u00c5\u00bee zdavnaj ni bilo ve\u00c4\u008d. A prav neverjeten se zdi podatek, da je bilo v bli\u00c5\u00benji kra\u00c5\u00a1ki vrta\u00c4\u008di [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":[],"categories":[15],"tags":[],"_links":{"self":[{"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/817"}],"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=817"}],"version-history":[{"count":4,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/817\/revisions"}],"predecessor-version":[{"id":835,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/817\/revisions\/835"}],"wp:attachment":[{"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=817"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=817"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=817"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}