{"id":8796,"date":"2013-05-05T20:37:29","date_gmt":"2013-05-05T18:37:29","guid":{"rendered":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=8796"},"modified":"2013-05-05T20:56:28","modified_gmt":"2013-05-05T18:56:28","slug":"podatki-iz-mrazisc-3-maj-2013","status":"publish","type":"post","link":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=8796","title":{"rendered":"Podatki iz mrazi\u00c5\u00a1\u00c4\u008d, 3. maj 2013"},"content":{"rendered":"<p style=\"text-align: justify;\">Tekom minule zime v mrazi\u00c5\u00a1\u00c4\u008dih Zaplane ni bilo izjemno nizkih temperatur in podobno je bilo tudi v najnovej\u00c5\u00a1em spomladanskem merilnem nizu, ki ga je zaznamovala predvsem debela in dolgotrajna sne\u00c5\u00bena odeja v zaprtih mrazi\u00c5\u00a1\u00c4\u008dih. Ta je bila posledica izdatnih sne\u00c5\u00benih padavin pozimi in v zgodnji pomladi ter relativno suhega aprila.<\/p>\n<p style=\"text-align: justify;\">V obdobju med 13. marcem in 3. majem so bile jasne no\u00c4\u008di brez vetra redke in \u00c5\u00a1e te so se pojavljale v \u00c4\u008dasu manj mrzle zra\u00c4\u008dne mase. V mrazi\u00c5\u00a1\u00c4\u008du Dolinca je bila najni\u00c5\u00beja temperatura -15,5 \u00c2\u00b0C izmerjena 16. marca. Na vremenski postaji Zaplana 21 m nad dnom mrazi\u00c5\u00a1\u00c4\u008da Dolinca se je v omenjeni no\u00c4\u008di ohladilo do -9,5 \u00c2\u00b0C. Temperaturna razlika med mrazi\u00c5\u00a1\u00c4\u008dem in okolico tako ni bila posebno velika. Temperatura se je v mrazi\u00c5\u00a1\u00c4\u008du globoko spustila \u00c5\u00a1e 28. marca sredi no\u00c4\u008di (-14,6 \u00c2\u00b0C), v nadaljevanju pa so bile no\u00c4\u008dne temperature \u00c5\u00bee precej vi\u00c5\u00a1je. V merilnem obdobju se je temperatura nazadnje spustila pod ledi\u00c5\u00a1\u00c4\u008de 26. aprila, ko je bilo -0,8 \u00c2\u00b0C. 1. maja je bila ob vzhodnem vetru v mrazi\u00c5\u00a1\u00c4\u008du izmerjena najvi\u00c5\u00a1ja temperatura 27,1 \u00c2\u00b0C, na zgornji meteorolo\u00c5\u00a1ki postaji Zaplana pa 25,2 \u00c2\u00b0C.<\/p>\n<p style=\"text-align: justify;\">Zaradi dinami\u00c4\u008dnega vremena s pogostimi padavinami, kakr\u00c5\u00a1no je vladalo v minulih mesecih, pa najbolj zanimivi izmerjeni podatki ne prihajajo iz Dolince, temve\u00c4\u008d iz precej globjega mrazi\u00c5\u00a1\u00c4\u008da Globoka dolina pri Jezercu. Po sne\u00c5\u00beeni zimi in prvi tretjini pomladi je Globoko dolino \u00c5\u00a1e ve\u00c4\u008dji del aprila pokrivala meter debela sne\u00c5\u00bena odeja, ki \u00c5\u00a1e do 5. maja zjutraj ni povsem skopnela. Sneg v Dolinci je pobralo tri tedne prej, mrazi\u00c5\u00a1\u00c4\u008de pod sedanjim \u00c4\u008debelnjakom pa je bilo zasne\u00c5\u00beeno do konca aprila. Dolgo v pomlad zasne\u00c5\u00beeno dno Globoke doline je imelo velik vpliv na temperaturo zraka v tej kra\u00c5\u00a1ki kotanji.<\/p>\n<p style=\"text-align: center;\"><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2013\/05\/grafglobokaapril2013.gif\" target=\"_blank\" rel=\"lightbox[8796]\"><img decoding=\"async\" loading=\"lazy\" class=\"aligncenter size-thumbnail wp-image-8795\" alt=\"grafglobokaapril2013\" src=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2013\/05\/grafglobokaapril2013-130x67.gif\" width=\"130\" height=\"67\" srcset=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2013\/05\/grafglobokaapril2013-130x67.gif 130w, http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2013\/05\/grafglobokaapril2013-800x417.gif 800w\" sizes=\"(max-width: 130px) 100vw, 130px\" \/><\/a><em>Potek temperature zraka v mrazi\u00c5\u00a1\u00c4\u008du Globoka dolina v primerjavi z vremensko postajo Zaplana spomladi 2013.<\/em><\/p>\n<p style=\"text-align: justify;\">Kot je razvidno iz grafikona je temperatura zraka sledila temperaturi sne\u00c5\u00bene odeje, ki zna\u00c5\u00a1a okoli 0 \u00c2\u00b0C. V za\u00c4\u008detku obdobja je temperatura zraka tudi podnevi vztrajala okoli ledi\u00c5\u00a1\u00c4\u008da, v nadaljevanju pa se je temperatura pribli\u00c5\u00beala ledi\u00c5\u00a1\u00c4\u008du le \u00c5\u00a1e pono\u00c4\u008di. Vpliv sne\u00c5\u00bene odeje je dobro viden 16. in 17. marca, ko se je ob otoplitvi v mrazi\u00c5\u00a1\u00c4\u008du hitro segrelo do 0 \u00c2\u00b0C, nad to vrednostjo pa zaradi vpliva mrzlega snega temperatura ni segla. Nizka nadmorska vi\u00c5\u00a1ina mrazi\u00c5\u00a1\u00c4\u008da se pozna v dneh okoli 25. marca, ko je bilo mrazi\u00c5\u00a1\u00c4\u008de ob vetrovnem in s tem preme\u00c5\u00a1anem ozra\u00c4\u008dju toplej\u00c5\u00a1e od vremenske postaje Zaplana. 18. aprila \u00c4\u008dez dan pa je bila med vremensko postajo Zaplana in mrazi\u00c5\u00a1\u00c4\u008dem zabele\u00c5\u00beena temperaturna razlika kar 19,2 \u00c2\u00b0C. Tak\u00c5\u00a1na temperaturna razlika na obmo\u00c4\u008dju Zaplane \u00c5\u00a1e ni bila izmerjena.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tekom minule zime v mrazi\u00c5\u00a1\u00c4\u008dih Zaplane ni bilo izjemno nizkih temperatur in podobno je bilo tudi v najnovej\u00c5\u00a1em spomladanskem merilnem nizu, ki ga je zaznamovala predvsem debela in dolgotrajna sne\u00c5\u00bena odeja v zaprtih mrazi\u00c5\u00a1\u00c4\u008dih. Ta je bila posledica izdatnih sne\u00c5\u00benih padavin pozimi in v zgodnji pomladi ter relativno suhega aprila. V obdobju med 13. marcem [&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\/8796"}],"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=8796"}],"version-history":[{"count":41,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/8796\/revisions"}],"predecessor-version":[{"id":8837,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/8796\/revisions\/8837"}],"wp:attachment":[{"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=8796"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=8796"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=8796"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}