{"id":8376,"date":"2013-02-03T22:58:22","date_gmt":"2013-02-03T21:58:22","guid":{"rendered":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=8376"},"modified":"2013-02-07T15:10:55","modified_gmt":"2013-02-07T14:10:55","slug":"snezenje-2-februarja-2013","status":"publish","type":"post","link":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=8376","title":{"rendered":"Sne\u00c5\u00beenje 2. februarja 2013"},"content":{"rendered":"

Ob raz\u00c5\u00a1iritvi hladnega zraka v vi\u00c5\u00a1inah nad obmo\u00c4\u008dje Sredozemlja je nad Genovskim zalivom nastal globok ciklon. De\u00c5\u00beju in visoki temperaturi zraka ob toplem jugozahodniku\u00c2\u00a0je sledilo sne\u00c5\u00beenje, ki je bilo na obmo\u00c4\u008dju Zaplane precej bolj izrazito od pri\u00c4\u008dakovanj. Moker in te\u00c5\u00beek\u00c2\u00a0sneg je povzro\u00c4\u008dal bistveno ve\u00c4\u008d preglavic kot suh sneg ob 6-dnevnem sne\u00c5\u00beenju v sredini januarja.<\/p>\n

Ve\u00c4\u008d padavin od pri\u00c4\u008dakovanj je padlo \u00c5\u00bee v prvem delu vremenskega poslab\u00c5\u00a1anja v no\u00c4\u008di na soboto, 2. februarja. Temperatura je zna\u00c5\u00a1ala okoli 6 \u00c2\u00b0C\u00c2\u00a0in padlo je preko 10 mm de\u00c5\u00beja, vendar se je okoli 20 cm debela\u00c2\u00a0sne\u00c5\u00bena odeja\u00c2\u00a0ohranila vse do pri\u00c4\u008detka sne\u00c5\u00beenja okoli tretje ure popoldne. Po obratu v sneg je v\u00c2\u00a0sne\u00c5\u00beni obliki padlo \u00c5\u00a1e\u00c2\u00a0dobrih 30 mm padavin. Novega snega je bilo blizu 30 cm, saj se je s prvotnih 20 cm sne\u00c5\u00bena odeja odebelila\u00c2\u00a0na 45 cm, pri \u00c4\u008demer seveda\u00c2\u00a0ne gre prezreti sprotnega posedanja sne\u00c5\u00bene odeje.<\/p>\n

\"sneg108\"<\/a>Najbolj kriti\u00c4\u008dne\u00c2\u00a0razmere so bile v no\u00c4\u008di na nedeljo, do jutra se je sneg \u00c5\u00bee vsaj deloma obletel z drevja.<\/em><\/p>\n

Snega je bilo\u00c2\u00a0ve\u00c4\u008d kot v bli\u00c5\u00benji okolici, kjer je bilo pretoplo za sne\u00c5\u00bene padavine, ali pa je bilo manj padavin\u00c2\u00a0zaradi fenskega severnega vetra. Ponekod je\u00c2\u00a0med predhodno odjugo pobralo ves sneg in novi sneg ni padal na staro sne\u00c5\u00beno podlago kot je bilo to na primeru Zaplane. V nedeljo, 3. februarja zjutraj\u00c2\u00a0je bilo na Spodnji Zaplani (566 m.n.v.)\u00c2\u00a0izmerjeno 44 cm snega, kar je bilo\u00c2\u00a0\u00c5\u00a1e enkrat toliko kot v Logatcu. Znatna razlika v vi\u00c5\u00a1ini sne\u00c5\u00bene odeje iz meseca januarja se je med\u00c2\u00a0obema\u00c2\u00a0vremenskima postajama \u00c5\u00a1e pove\u00c4\u008dala. Na uradni\u00c2\u00a0meteorolo\u00c5\u00a1ki postaji Katarina nad Ljubljano (660 m)\u00c2\u00a0v Polhograjskem hribovju je bilo zaradi\u00c2\u00a0bolj izpostavljene\u00c2\u00a0prisojne lokacije meritev izmerjeno samo 9 cm snega, v \u00c5\u00a0entjo\u00c5\u00a1tu nad Horjulom (642 m)\u00c2\u00a0pa 30 cm.<\/p>\n

\"sneg110\"<\/a>Drevje se je lahko samo\u00c2\u00a0priklonilo te\u00c5\u00bekemu\u00c2\u00a0mokremu snegu.<\/em><\/p>\n

\"sneg109\"<\/a>Moker sneg je povzro\u00c4\u008dil tudi nekaj preglavic.<\/em><\/p>\n

 <\/p>\n

Viri podatkov:<\/p>\n

– podatki z zasebnih vremenskih postaj Gornji Logatec in \u00c5\u00a0entjo\u00c5\u00a1t nad Horjulom<\/p>\n

– vremenski portal ARSO-meteo.si<\/p>\n","protected":false},"excerpt":{"rendered":"

Ob raz\u00c5\u00a1iritvi hladnega zraka v vi\u00c5\u00a1inah nad obmo\u00c4\u008dje Sredozemlja je nad Genovskim zalivom nastal globok ciklon. De\u00c5\u00beju in visoki temperaturi zraka ob toplem jugozahodniku\u00c2\u00a0je sledilo sne\u00c5\u00beenje, ki je bilo na obmo\u00c4\u008dju Zaplane precej bolj izrazito od pri\u00c4\u008dakovanj. Moker in te\u00c5\u00beek\u00c2\u00a0sneg je povzro\u00c4\u008dal bistveno ve\u00c4\u008d preglavic kot suh sneg ob 6-dnevnem sne\u00c5\u00beenju v sredini januarja. Ve\u00c4\u008d […]<\/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\/8376"}],"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=8376"}],"version-history":[{"count":24,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/8376\/revisions"}],"predecessor-version":[{"id":8427,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/8376\/revisions\/8427"}],"wp:attachment":[{"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=8376"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=8376"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=8376"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}