{"id":4335,"date":"2010-07-06T22:31:00","date_gmt":"2010-07-06T20:31:00","guid":{"rendered":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=4335"},"modified":"2010-07-17T15:18:29","modified_gmt":"2010-07-17T13:18:29","slug":"nevihta-6-julija-2010","status":"publish","type":"post","link":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=4335","title":{"rendered":"Nevihta 6.julija 2010"},"content":{"rendered":"

V popoldanskih urah je obmo\u00c4\u008dje\u00c2\u00a0Zaplane pre\u00c5\u00a1la nevihta z nalivi in\u00c2\u00a0mo\u00c4\u008dnim vetrom. Zaradi gozda se je lahko sli\u00c5\u00a1al nevihtni pi\u00c5\u00a1, ki se je\u00c2\u00a0bli\u00c5\u00beal iz zahoda. Pri prvih, tudi najmo\u00c4\u008dnej\u00c5\u00a1ih sunkih vetra je pri\u00c4\u008delo mo\u00c4\u008dno de\u00c5\u00beevati, ker pa je \u00c5\u00a1lo za velik\u00c2\u00a0nevihtni sistem oz. skupek ve\u00c4\u008dih neviht\u00c2\u00a0Mesoscale Convective System (MCS) v velikosti skoraj pol Slovenije je pri njegovem po\u00c4\u008dasnem umikanju \u00c5\u00a1e pol ure umirjeno de\u00c5\u00beevalo. Iz smeri Vrhnike je bil nad Zaplano oz. njenim delom Planina nad Vrhniko\u00c2\u00a0viden shelf cloud<\/a>, oblak zna\u00c4\u008dilen za nevihte in\u00c2\u00a0ki\u00c2\u00a0je povezan\u00c2\u00a0s sunkovitimi vetrovi oz. iztokom hladnej\u00c5\u00a1ega zraka iz notranjosti nevihte. Avtomatska meteorolo\u00c5\u00a1ka postaja Zaplana je zabele\u00c5\u00beila 19,4mm de\u00c5\u00beja, med de\u00c5\u00bejem pa ni bila opa\u00c5\u00beena to\u00c4\u008da\u00c2\u00a0ali sodra. Elektronski de\u00c5\u00beemer je na svoji severozahodni strani\u00c2\u00a0nekoliko zastrt z drevjem, ki ob zares mo\u00c4\u008dnih vetrovih vpliva na izmerjeno koli\u00c4\u008dino padavin. Ob nevihti je zapihal severozahodni veter s hitrostjo 38,2km\/h, zaradi redkih merilnih intervalov vetromera pa\u00c2\u00a0so zagotovo\u00c2\u00a0ostali nezabele\u00c5\u00beeni \u00c5\u00a1e\u00c2\u00a0mo\u00c4\u008dnej\u00c5\u00a1i sunki vetra.\u00c2\u00a0Ker se je pri\u00c4\u008dakovalo prihod neviht ravno\u00c2\u00a0iz zahodne smeri in mo\u00c4\u008dan nevihtni pi\u00c5\u00a1 iz severozahoda je bil na bli\u00c5\u00benjo in bolj odprto\u00c2\u00a0lokacijo postavljen tudi klasi\u00c4\u008dni de\u00c5\u00beemer. Lokacija se je za meritve padavin\u00c2\u00a0ob tej nevihti izkazala za pomemben faktor, saj je na podlagi klasi\u00c4\u008dnega de\u00c5\u00beemera in meritev z menzuro padlo\u00c2\u00a022,8mm de\u00c5\u00beja. Ve\u00c4\u008d padavin je na podlagi slik meteorolo\u00c5\u00a1kega\u00c2\u00a0radarja in okoli\u00c5\u00a1kih zasebnih\u00c2\u00a0vremenskih postaj\u00c2\u00a0padlo na Zgornji Zaplani in v okolici Vrhnike. Veter je povzro\u00c4\u008dil preglavice v Logatcu, kjer\u00c2\u00a0je\u00c2\u00a0podrl nekaj\u00c2\u00a0dreves in razkril dva objekta. Po lastnem ogledu pa ni bilo opaziti \u00c5\u00a1kode na severnem in zahodnem robu Loga\u00c5\u00a1kega polja,\u00c2\u00a0vsaj eno drevo pa se je, predvsem zaradi slabe prira\u00c5\u00a1\u00c4\u008denosti lesa,\u00c2\u00a0podrlo v bli\u00c5\u00beini Miznega Dola na Zgornji Zaplani.\u00c2\u00a0Zaradi bli\u00c5\u00benjega udara strele na obmo\u00c4\u008dju meteorolo\u00c5\u00a1ke postaje za kraj\u00c5\u00a1i \u00c4\u008das ni bilo elektrike, zaradi mo\u00c4\u008dnih razelektritev pa je\u00c2\u00a0prenehal delovati tudi vetromer, na katerem je bil zato potreben ro\u00c4\u008dni poseg.<\/p>\n

<\/embed><\/object><\/a><\/p>\n

Viri podatkov:<\/p>\n

– podatki z zasebnih meteorolo\u00c5\u00a1kih postaj<\/p>\n

– Uprava RS za za\u00c5\u00a1\u00c4\u008dito in re\u00c5\u00a1evanje<\/p>\n

– Vremensko dru\u00c5\u00a1tvo ZEVS<\/p>\n","protected":false},"excerpt":{"rendered":"

V popoldanskih urah je obmo\u00c4\u008dje\u00c2\u00a0Zaplane pre\u00c5\u00a1la nevihta z nalivi in\u00c2\u00a0mo\u00c4\u008dnim vetrom. Zaradi gozda se je lahko sli\u00c5\u00a1al nevihtni pi\u00c5\u00a1, ki se je\u00c2\u00a0bli\u00c5\u00beal iz zahoda. Pri prvih, tudi najmo\u00c4\u008dnej\u00c5\u00a1ih sunkih vetra je pri\u00c4\u008delo mo\u00c4\u008dno de\u00c5\u00beevati, ker pa je \u00c5\u00a1lo za velik\u00c2\u00a0nevihtni sistem oz. skupek ve\u00c4\u008dih neviht\u00c2\u00a0Mesoscale Convective System (MCS) v velikosti skoraj pol Slovenije je pri […]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","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\/4335"}],"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=4335"}],"version-history":[{"count":24,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/4335\/revisions"}],"predecessor-version":[{"id":4349,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/4335\/revisions\/4349"}],"wp:attachment":[{"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=4335"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=4335"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=4335"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}