{"id":3758,"date":"2010-03-22T14:18:06","date_gmt":"2010-03-22T13:18:06","guid":{"rendered":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=3758"},"modified":"2010-03-30T22:49:52","modified_gmt":"2010-03-30T20:49:52","slug":"snezne-razmere-na-zaplani-21-marca-2010","status":"publish","type":"post","link":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=3758","title":{"rendered":"Sne\u00c5\u00bene razmere na Zaplani 21.marca 2010"},"content":{"rendered":"

V leto\u00c5\u00a1nji meteorolo\u00c5\u00a1ki pomladi vladajo na Zaplani tipi\u00c4\u008dne sne\u00c5\u00bene razmere. Na kratko bi jih lahko opisali kot spomladansko-zimski kontrasti, saj je v splo\u00c5\u00a1nem sneg \u00c5\u00bee skopnel, na prisojnih pobo\u00c4\u008djih so iz zemlje pokukali prvi znanilci pomladi, medtem ko je v osojnih legah, \u00c5\u00a1e posebno pa v mrazi\u00c5\u00a1\u00c4\u008dih, snega \u00c5\u00a1e vedno veliko. Take razmere se pojavljajo po zimah, kakr\u00c5\u00a1na je bila leto\u00c5\u00a1nja, torej z dovolj sne\u00c5\u00benih padavin. V milih zimah pade malo sne\u00c5\u00benih padavin in tako se\u00c2\u00a0tudi v mrazi\u00c5\u00a1\u00c4\u008dih ne more nabrati toliko snega, da bi se lahko zadr\u00c5\u00beeval \u00c5\u00a1e\u00c2\u00a0v pozni pomladi.<\/p>\n

19.marec je bil zadnji dan, ko se je lahko na Zaplani \u00c5\u00a1e govorilo o strnjeni sne\u00c5\u00beni odeji.\u00c2\u00a020.marca je bila v okolici meteorolo\u00c5\u00a1ke postaje Zaplana \u00c5\u00bee manj kot polovica\u00c2\u00a0povr\u00c5\u00a1ine pokrita s snegom. \u00c4\u0152eprav je bilo na merilnem mestu \u00c5\u00a1e 10cm snega, je \u00c5\u00a1lo le za sne\u00c5\u00bene krpe. Na Loga\u00c5\u00a1kem polju je sneg skopnel\u00c2\u00a0\u00c5\u00bee kak\u00c5\u00a1en dan ali dva pred tem. Mrazi\u00c5\u00a1\u00c4\u008de Dolinca je kazalo klasi\u00c4\u008dno pomladno podobo. Prisoje so bile kopne \u00c5\u00bee ve\u00c4\u008d dni, na osojah pa je vztrajala \u00c5\u00a1e relativno debela sne\u00c5\u00bena odeja.<\/p>\n

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Mrazi\u00c5\u00a1\u00c4\u008de Dolinca je zaradi svojih karakteristik znano po nizkih jutranjih temperaturah, sne\u00c5\u00bene razmere pa so bolj\u00c5\u00a1e v nekaterih globjih in sen\u00c4\u008dnih mrazi\u00c5\u00a1\u00c4\u008dih. Eno takih je sosednje\u00c2\u00a0mrazi\u00c5\u00a1\u00c4\u008de pod \u00c4\u008debelnjakom. 21.marca zjutraj\u00c2\u00a0je bilo v tem mrazi\u00c5\u00a1\u00c4\u008du \u00c5\u00a1e 62cm snega.<\/p>\n

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Kljub nizki\u00c2\u00a0nadmorski vi\u00c5\u00a1ini 489m po sne\u00c5\u00benih razmerah \u00c5\u00a1e bolj izstopa mrazi\u00c5\u00a1\u00c4\u008de Globoka dolina v bli\u00c5\u00beini Jezerca, kjer od 21.marca tudi potekajo meritve temperatur. Tega dne je bilo v tem\u00c2\u00a0globokem in z gozdom pora\u00c5\u00a1\u00c4\u008denem mrazi\u00c5\u00a1\u00c4\u008du 60-75cm snega.<\/p>\n

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Tudi na uravnanih in odprtih\u00c2\u00a0legah izven mrazi\u00c5\u00a1\u00c4\u008da je bilo snega glede na bli\u00c5\u00benjo okolico \u00c5\u00a1e veliko. Glede na vi\u00c5\u00a1ino snega je tako ponekod vladala prava zima…<\/p>\n

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…medtem ko\u00c2\u00a0so se \u00c4\u008drni\u00c2\u00a0telohi in spomladanski \u00c5\u00beafrani ve\u00c4\u008dinoma\u00c2\u00a0\u00c5\u00bee lahko mirno\u00c2\u00a0spogledovali z\u00c2\u00a0umikajo\u00c4\u008do se\u00c2\u00a0sne\u00c5\u00beno odejo.<\/p>\n

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Sne\u00c5\u00bena odeja, ki se\u00c2\u00a0je na Zaplani zadr\u00c5\u00beevala vse od 2.januarja, je torej pove\u00c4\u008dini skopnela. Prave zime je nepreklicno konec, kar pa ne pomeni, da v aprilu ne more pasti \u00c5\u00a1e veliko mokrega snega, ki bi se v primeru no\u00c4\u008dnega zmrzovanja zadr\u00c5\u00beal nekaj dni. Nenazadnje je pomenljiv podatek, da se je v obdobju 2002-2006 aprilski sneg\u00c2\u00a0na Zaplani pojavil \u00c4\u008disto vsako leto in da so bila\u00c2\u00a0pravzaprav\u00c2\u00a0zadnja tri leta brez aprilskega snega posebnost glede na dolgoletne statistike.<\/p>\n","protected":false},"excerpt":{"rendered":"

V leto\u00c5\u00a1nji meteorolo\u00c5\u00a1ki pomladi vladajo na Zaplani tipi\u00c4\u008dne sne\u00c5\u00bene razmere. Na kratko bi jih lahko opisali kot spomladansko-zimski kontrasti, saj je v splo\u00c5\u00a1nem sneg \u00c5\u00bee skopnel, na prisojnih pobo\u00c4\u008djih so iz zemlje pokukali prvi znanilci pomladi, medtem ko je v osojnih legah, \u00c5\u00a1e posebno pa v mrazi\u00c5\u00a1\u00c4\u008dih, snega \u00c5\u00a1e vedno veliko. Take razmere se pojavljajo […]<\/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\/3758"}],"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=3758"}],"version-history":[{"count":21,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/3758\/revisions"}],"predecessor-version":[{"id":3788,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/3758\/revisions\/3788"}],"wp:attachment":[{"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=3758"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=3758"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=3758"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}