{"id":936,"date":"2009-07-06T19:36:03","date_gmt":"2009-07-06T17:36:03","guid":{"rendered":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=936"},"modified":"2011-11-08T11:25:17","modified_gmt":"2011-11-08T10:25:17","slug":"snezne-razmere-16-marca-2009","status":"publish","type":"post","link":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=936","title":{"rendered":"Sne\u00c5\u00bene razmere 16.marca 2009"},"content":{"rendered":"<p style=\"text-align: justify;\">Od februarskega sne\u00c5\u00beenja je minilo \u00c5\u00bee precej \u00c4\u008dasa, ob mo\u00c4\u008dni odjugi z de\u00c5\u00bejem in ob vi\u00c5\u00a1jih temperaturah v marcu je sneg v okolici Zaplane skopnel tudi v osojnih legah. Ena od posledic ni\u00c5\u00bejih temperatur v mrazi\u00c5\u00a1\u00c4\u008dih je dalj\u00c5\u00a1e trajanje sne\u00c5\u00bene odeje. Spomladi, ko sneg skopni, postanejo mrazi\u00c5\u00a1\u00c4\u008da \u00c5\u00a1e posebej dobro opazen element v pokrajini. 15.marca 2009 je bilo v mrazi\u00c5\u00a1\u00c4\u008du na Spodnji Zaplani \u00c5\u00a1e 18cm pomrznjenega snega in razmere so bile povsem zimske glede na razmere v okolici.<\/p>\n<p style=\"margin-bottom: 0cm; text-align: justify;\">\u00c4\u0152eprav se zdi razlika glede na okolico izjemna, se kot ka\u00c5\u00bee vseeno ne bo ponovil april 2004, ko je bilo po Zaplani \u00c5\u00bee spomladansko vzdu\u00c5\u00a1je, medtem ko je mrazi\u00c5\u00a1\u00c4\u008de pokrivalo \u00c5\u00a1e 70cm \u00c2\u00bbbetonskega\u00c2\u00ab snega. \u00c5\u00a0e precej druga\u00c4\u008dne so bile razmere v mrazi\u00c5\u00a1\u00c4\u008dih pred dvajset in ve\u00c4\u008d leti. \u00c5\u00bde v minulih zimah se je pokazalo, da lahko nekatera mrazi\u00c5\u00a1\u00c4\u008da na Zaplani sne\u00c5\u00bena odeja pokriva skoraj pol leta in da se lahko sneg zadr\u00c5\u00bei tudi med prvomajskimi prazniki. V posameznih zimah v preteklosti pa je sneg pokrival tla verjetno tudi \u00c5\u00a1e ob koncu maja.<\/p>\n<p style=\"margin-bottom: 0cm; text-align: justify;\">Sneg se v zgoraj predstavljenem mrazi\u00c5\u00a1\u00c4\u008du zadr\u00c5\u00beuje dalj \u00c4\u008dasa kot v okolici zaradi ve\u00c4\u008d vzrokov. Kotanja ima sen\u00c4\u008dno lego, kotanjasta oblika pa omogo\u00c4\u008da zadr\u00c5\u00beevanje temperaturne inverzije in ve\u00c4\u008djo zati\u00c5\u00a1nost kotanje, ki jo zato ne prepiha vsak topel veter. Ob suhem zraku je plast zraka tik nad sne\u00c5\u00beno odejo precej hladnej\u00c5\u00a1a kot v prostem ozra\u00c4\u008dju, ker sonce dna mrazi\u00c5\u00a1\u00c4\u008da ne dose\u00c5\u00bee, se sneg ne tali prav veliko tudi v dnevih, ko temperature v okolici sicer dosegajo +15\u00c2\u00b0C. Ker se sneg tako dolgo \u00c4\u008dasa dr\u00c5\u00bei, pade novi sneg obi\u00c4\u008dajno na \u00c5\u00bee staro sne\u00c5\u00beno podlago in sne\u00c5\u00bena odeja se v mrazi\u00c5\u00a1\u00c4\u008du samo debeli in dose\u00c5\u00bee najve\u00c4\u008djo debelino obi\u00c4\u008dajno v spomladanskih mesecih.<\/p>\n<p style=\"margin-bottom: 0cm; text-align: justify;\">\n","protected":false},"excerpt":{"rendered":"<p>Od februarskega sne\u00c5\u00beenja je minilo \u00c5\u00bee precej \u00c4\u008dasa, ob mo\u00c4\u008dni odjugi z de\u00c5\u00bejem in ob vi\u00c5\u00a1jih temperaturah v marcu je sneg v okolici Zaplane skopnel tudi v osojnih legah. Ena od posledic ni\u00c5\u00bejih temperatur v mrazi\u00c5\u00a1\u00c4\u008dih je dalj\u00c5\u00a1e trajanje sne\u00c5\u00bene odeje. Spomladi, ko sneg skopni, postanejo mrazi\u00c5\u00a1\u00c4\u008da \u00c5\u00a1e posebej dobro opazen element v pokrajini. 15.marca [&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\/936"}],"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=936"}],"version-history":[{"count":7,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/936\/revisions"}],"predecessor-version":[{"id":6407,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/936\/revisions\/6407"}],"wp:attachment":[{"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=936"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=936"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=936"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}