Podobno kot prva je bila vremensko nestanovitna tudi druga polovica meteorolo\u00c5\u00a1kega poletja. Kljub temu se je na obmo\u00c4\u008dju Zaplane zaradi odsotnosti ploh in neviht, ki so sicer zajemale bli\u00c5\u00benjo okolico, lokalno krepila su\u00c5\u00a1nost. Prehod izrazitej\u00c5\u00a1e hladne fronte brez padavin bi ob hkratnem stopnjevanju su\u00c5\u00a1e predstavljal pomemben dejavnik za pojav jutranjega mraza v mrazi\u00c5\u00a1\u00c4\u008dih.<\/p>\n
Do prehoda tak\u00c5\u00a1ne fronte ni pri\u00c5\u00a1lo, v \u00c4\u008dasu su\u00c5\u00a1e je bila zra\u00c4\u008dna masa topla in v mrazi\u00c5\u00a1\u00c4\u008dih se ni ohladilo pod 0 \u00c2\u00b0C, kar se je zgodilo drugo poletje zapored in tretji\u00c4\u008d v zgodovini meritev, ki v mrazi\u00c5\u00a1\u00c4\u008du Dolinca (545 m) potekajo \u00c5\u00bee vse od leta 2004. V Dolinci je bila najni\u00c5\u00beja temperatura druge polovice minulega poletja, 2,4 \u00c2\u00b0C, izmerjena 28. avgusta. Na vremenski postaji Zaplana, 21 m nad mrazi\u00c5\u00a1\u00c4\u008dem, se je v isti no\u00c4\u008di ohladilo na 8,6 \u00c2\u00b0C. Poleg omenjene najni\u00c5\u00beje temperature se je pod 5 \u00c2\u00b0C ohladilo \u00c5\u00a1e dvakrat, 29. avgusta (2,8 \u00c2\u00b0C) in 30. avgusta (3,9 \u00c2\u00b0C). Najve\u00c4\u008dje temperaturne razlike med dnevom in no\u00c4\u008djo so bile v zadnji dekadi avgusta, zna\u00c5\u00a1ale so okrog 24 \u00c2\u00b0C. Najbolj vro\u00c4\u008de je bilo v mrazi\u00c5\u00a1\u00c4\u008du 1. avgusta (32,8 \u00c2\u00b0C), ko je bilo podobno vro\u00c4\u008de tudi na zgornji vremenski postaji Zaplana (32,5 \u00c2\u00b0C). Podrobnej\u00c5\u00a1i podatki iz mrazi\u00c5\u00a1\u00c4\u008d Dolinca in Dvoj\u00c4\u008dek (v zimskem \u00c4\u008dasu) ter Ulovke so na voljo v posodobljeni rubriki mrazi\u00c5\u00a1\u00c4\u008da<\/a>.<\/p>\n <\/p>\n","protected":false},"excerpt":{"rendered":" Podobno kot prva je bila vremensko nestanovitna tudi druga polovica meteorolo\u00c5\u00a1kega poletja. Kljub temu se je na obmo\u00c4\u008dju Zaplane zaradi odsotnosti ploh in neviht, ki so sicer zajemale bli\u00c5\u00benjo okolico, lokalno krepila su\u00c5\u00a1nost. Prehod izrazitej\u00c5\u00a1e hladne fronte brez padavin bi ob hkratnem stopnjevanju su\u00c5\u00a1e predstavljal pomemben dejavnik za pojav jutranjega mraza v mrazi\u00c5\u00a1\u00c4\u008dih. Do prehoda […]<\/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\/15316"}],"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=15316"}],"version-history":[{"count":18,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/15316\/revisions"}],"predecessor-version":[{"id":15334,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/15316\/revisions\/15334"}],"wp:attachment":[{"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=15316"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=15316"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=15316"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}