{"id":7516,"date":"2012-07-24T21:42:23","date_gmt":"2012-07-24T19:42:23","guid":{"rendered":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=7516"},"modified":"2012-08-26T11:38:17","modified_gmt":"2012-08-26T09:38:17","slug":"sredina-junija-ob-14-uri-na-nadmorski-visini-489-m-temperatura-zraka-5-c","status":"publish","type":"post","link":"http:\/\/www.slometeo.net\/zaplana\/blog\/?p=7516","title":{"rendered":"Sredina junija ob 14. uri na nadmorski vi\u00c5\u00a1ini 489 m &#8211; temperatura zraka 5 \u00c2\u00b0C"},"content":{"rendered":"<p style=\"text-align: justify;\">V mrazi\u00c5\u00a1\u00c4\u008dih je najni\u00c5\u00beja temperatura zraka kot posledica radiacijskega ohlajanja dose\u00c5\u00beena v no\u00c4\u008dnih ali zgodnjih jutranjih urah, medtem ko je sredi dneva v njih navadno\u00c2\u00a0podobno\u00c2\u00a0ali celo\u00c2\u00a0bolj toplo kot v njihovi\u00c2\u00a0okolici. 13. junija\u00c2\u00a0\u00c4\u008dez dan\u00c2\u00a0pa\u00c2\u00a0je bil v enem izmed mrazi\u00c5\u00a1\u00c4\u008d na Zaplani zabele\u00c5\u00been zanimiv pojav ohladitve zaradi to\u00c4\u008de.<\/p>\n<p style=\"text-align: justify;\">Ob nevihtah\u00c2\u00a0zajame vremensko postajo Zaplana (566 m)\u00c2\u00a0in dve bli\u00c5\u00benji mrazi\u00c5\u00a1\u00c4\u008di\u00c2\u00a0enaka zra\u00c4\u008dna masa. Temperatura se povsod uskladi, saj hladen zrak zaradi mo\u00c4\u008dnej\u00c5\u00a1ega vetra in\u00c2\u00a0padavin zapolni tudi najglobje kotanje. Temperatura med vremensko postajo Zaplana in mrazi\u00c5\u00a1\u00c4\u008di\u00c2\u00a0se pogosto precej razlikuje, najhitreje pa se uskladi v\u00c2\u00a0primeru kak\u00c5\u00a1ne nevihte. To je vidno na spodnjem grafikonu, ki ka\u00c5\u00bee razmere ob\u00c2\u00a0obi\u00c4\u008dajni nevihti z de\u00c5\u00bejem.<\/p>\n<p style=\"text-align: center;\"><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2012\/07\/graf9jul2012.gif\" target=\"_blank\" rel=\"lightbox[7516]\"><img decoding=\"async\" loading=\"lazy\" class=\"aligncenter size-thumbnail wp-image-7521\" title=\"graf9jul2012\" src=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2012\/07\/graf9jul2012-130x73.gif\" alt=\"\" width=\"130\" height=\"73\" srcset=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2012\/07\/graf9jul2012-130x73.gif 130w, http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2012\/07\/graf9jul2012.gif 636w\" sizes=\"(max-width: 130px) 100vw, 130px\" \/><\/a><em>Enaka temperatura zraka na vseh treh merilnih mestih ob popoldanski\u00c2\u00a0nevihti 9. julija 2012.<\/em><\/p>\n<p style=\"text-align: justify;\">V\u00c2\u00a0zgornjem primeru\u00c2\u00a0predstavlja manj\u00c5\u00a1o posebnost\u00c2\u00a0zgolj\u00c2\u00a0mrazi\u00c5\u00a1\u00c4\u008de\u00c2\u00a0Globoka dolina, v katerem\u00c2\u00a0je bilo zaradi zaprtosti in zasen\u00c4\u008denosti hladneje \u00c5\u00bee pred samo\u00c2\u00a0nevihto, pa tudi po nevihti\u00c2\u00a0ohlajeni zrak se je v mrazi\u00c5\u00a1\u00c4\u008du obdr\u00c5\u00beal dlje \u00c4\u008dasa. Zato sta se ostali\u00c2\u00a0dve merilni mesti\u00c2\u00a0po temperaturi\u00c2\u00a0za kraj\u00c5\u00a1i \u00c4\u008das\u00c2\u00a0izena\u00c4\u008dili z Globoko dolino, nato pa se\u00c2\u00a0z ogrevanjem od nje\u00c2\u00a0ponovno oddaljili.<\/p>\n<p style=\"text-align: justify;\">Nevihta 13. junija 2012 se je razlikovala od zgoraj omenjene nevihte po to\u00c4\u008di, ki je pokrivala tla. Iz naslednjega\u00c2\u00a0grafikona je razvidno, kako je temperatura po nevihti\u00c2\u00a0v mrazi\u00c5\u00a1\u00c4\u008du\u00c2\u00a0Dolinca in \u00c5\u00a1e posebej v Globoki dolini padla ni\u00c5\u00beje kot na vremenski postaji Zaplana.<\/p>\n<p style=\"text-align: center;\"><a href=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2012\/07\/graf13jun2012.gif\" target=\"_blank\" rel=\"lightbox[7516]\"><img decoding=\"async\" loading=\"lazy\" class=\"aligncenter size-thumbnail wp-image-7522\" title=\"graf13jun2012\" src=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2012\/07\/graf13jun2012-130x71.gif\" alt=\"\" width=\"130\" height=\"71\" srcset=\"http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2012\/07\/graf13jun2012-130x71.gif 130w, http:\/\/www.slometeo.net\/zaplana\/blog\/wp-content\/uploads\/2012\/07\/graf13jun2012.gif 636w\" sizes=\"(max-width: 130px) 100vw, 130px\" \/><\/a><em>Ob nevihti s to\u00c4\u008do 13. junija 2012 je bila ohladitev izrazitej\u00c5\u00a1a v bolj zaprtih obmo\u00c4\u008djih, kot so\u00c2\u00a0mrazi\u00c5\u00a1\u00c4\u008da.<\/em><\/p>\n<p style=\"text-align: justify;\">Vzrok za tako izrazito\u00c2\u00a0ohladitev v Globoki dolini je to\u00c4\u008da. Ob taljenju je\u00c2\u00a0bistveno bolj\u00c2\u00a0vplivala na ni\u00c5\u00bejo temperatura zraka v zaprti in zati\u00c5\u00a1ni Globoki dolini kot pa v plitvem mrazi\u00c5\u00a1\u00c4\u008du Dolinca in na\u00c2\u00a0reliefno povsem odprti vremenski postaji Zaplana. Na vremenski postaji Zaplana je\u00c2\u00a0to\u00c4\u008da ohlajala plast zraka tik nad tlemi, v mrazi\u00c5\u00a1\u00c4\u008du Dolinca\u00c2\u00a0je njen vpliv segal malo vi\u00c5\u00a1je (za 1 \u00c2\u00b0C ni\u00c5\u00beja temperatura), v\u00c2\u00a0Globoki dolini pa je zaradi manj\u00c5\u00a1ega volumna mrazi\u00c5\u00a1\u00c4\u008da (zraka) ta vpliv segel najvi\u00c5\u00a1je. 4,8 \u00c2\u00b0C\u00c2\u00a0ob 14. uri sredi junija na nadmorski vi\u00c5\u00a1ini komaj 489 m je vsekakor omembe vreden mraz! Za primerjavo povejmo, da se je na 800 m visoki Ulovki, ki jo je nevihta sicer\u00c2\u00a0nekoliko zgre\u00c5\u00a1ila, ohladilo le do 10,6 \u00c2\u00b0C.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>V mrazi\u00c5\u00a1\u00c4\u008dih je najni\u00c5\u00beja temperatura zraka kot posledica radiacijskega ohlajanja dose\u00c5\u00beena v no\u00c4\u008dnih ali zgodnjih jutranjih urah, medtem ko je sredi dneva v njih navadno\u00c2\u00a0podobno\u00c2\u00a0ali celo\u00c2\u00a0bolj toplo kot v njihovi\u00c2\u00a0okolici. 13. junija\u00c2\u00a0\u00c4\u008dez dan\u00c2\u00a0pa\u00c2\u00a0je bil v enem izmed mrazi\u00c5\u00a1\u00c4\u008d na Zaplani zabele\u00c5\u00been zanimiv pojav ohladitve zaradi to\u00c4\u008de. Ob nevihtah\u00c2\u00a0zajame vremensko postajo Zaplana (566 m)\u00c2\u00a0in dve bli\u00c5\u00benji [&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\/7516"}],"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=7516"}],"version-history":[{"count":22,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/7516\/revisions"}],"predecessor-version":[{"id":7711,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=\/wp\/v2\/posts\/7516\/revisions\/7711"}],"wp:attachment":[{"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=7516"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=7516"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/www.slometeo.net\/zaplana\/blog\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=7516"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}