Please use this identifier to cite or link to this item: https://physrep.ff.bg.ac.rs/handle/123456789/1133
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dc.contributor.authorTošić, Ivanaen
dc.contributor.authorUnkašević, Miroslavaen
dc.date.accessioned2022-07-12T18:19:37Z-
dc.date.available2022-07-12T18:19:37Z-
dc.date.issued2005-01-01en
dc.identifier.issn0177-798Xen
dc.identifier.urihttps://physrep.ff.bg.ac.rs/handle/123456789/1133-
dc.description.abstractPrecipitation is a very variable climatic element. It is highly variable, both spatially and temporally at different scales (interannual and intra-annual). The search for cyclicity in the climatic record can resolve some of the complexities of the atmospheric system. This paper takes the example of the Belgrade precipitation series (1889-2000) to illustrate how trend and spectral analysis can provide information on climate variability as expressed through this particular variable. The annual, seasonal and monthly precipitation series of the Belgrade-Observatory station were analyzed by means of the Mann-Kendall test and the spectral analysis. The power spectra were calculated using the autocorrelation spectral analysis, the maximum entropy spectral analysis and the multitaper method. The influence of large-scale phenomena such as the El-Niño Southern Oscillation (ENSO) and the North Atlantic Oscillation (NAO) on the Belgrade precipitation series was investigated. © Springer-Verlag 2004.en
dc.relation.ispartofTheoretical and Applied Climatologyen
dc.titleAnalysis of precipitation series for Belgradeen
dc.typeArticleen
dc.identifier.doi10.1007/s00704-004-0076-1en
dc.identifier.scopus2-s2.0-14044266201en
dc.identifier.urlhttps://api.elsevier.com/content/abstract/scopus_id/14044266201en
dc.relation.issue1en
dc.relation.volume80en
dc.relation.firstpage67en
dc.relation.lastpage77en
item.openairetypeArticle-
item.cerifentitytypePublications-
item.fulltextNo Fulltext-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.grantfulltextnone-
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