Please use this identifier to cite or link to this item: https://physrep.ff.bg.ac.rs/handle/123456789/1119
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dc.contributor.authorUnkašević, Miroslavaen
dc.contributor.authorMališic, Jovanen
dc.contributor.authorTošić, Ivanaen
dc.date.accessioned2022-07-12T18:19:35Z-
dc.date.available2022-07-12T18:19:35Z-
dc.date.issued1999-01-01en
dc.identifier.issn1350-4827en
dc.identifier.urihttps://physrep.ff.bg.ac.rs/handle/123456789/1119-
dc.description.abstract'Koshava' is a gusty wind of moderate to strong intensity, blowing from a south-easterly direction, over Serbia, Romania and Bulgaria. It is caused by the interaction between the synoptic circulation and the orography of the Carpathian and the Balkan mountains. This paper analyses wind data from an area where the influence the 'Koshava' wind is high during periods of maximum duration of 'Koshava'. The focus of the paper is the examination of urban and suburban effects on 'Koshava' and the correlation between the instantaneous maximum wind speed and the hourly mean values. Various empirical distributions are fitted to the daily maximum wind speed and the best fit for each season and site is proposed. The vertical structure of the lower troposphere above a suburban site during the longest period of consecutive days of 'Koshava', which occurred in January and February 1972, is considered.en
dc.relation.ispartofMeteorological Applicationsen
dc.titleSome aspects of the wind 'Koshava' in the lower troposphere over Belgradeen
dc.typeArticleen
dc.identifier.doi10.1017/S1350482799000997en
dc.identifier.scopus2-s2.0-0041706684en
dc.identifier.urlhttps://api.elsevier.com/content/abstract/scopus_id/0041706684en
dc.relation.issue1en
dc.relation.volume6en
dc.relation.firstpage69en
dc.relation.lastpage79en
item.openairetypeArticle-
item.cerifentitytypePublications-
item.fulltextNo Fulltext-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.grantfulltextnone-
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