Please use this identifier to cite or link to this item: https://physrep.ff.bg.ac.rs/handle/123456789/1269
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dc.contributor.authorHarpa, Gabriela Victoriaen
dc.contributor.authorCroitoru, Adina Elizaen
dc.contributor.authorĐurđević, Vladimiren
dc.contributor.authorHorvath, Csabaen
dc.date.accessioned2022-07-12T18:49:03Z-
dc.date.available2022-07-12T18:49:03Z-
dc.date.issued2019-12-01en
dc.identifier.issn0899-8418en
dc.identifier.urihttps://physrep.ff.bg.ac.rs/handle/123456789/1269-
dc.description.abstractThis paper presents the results of a study focused on the projected changes in extreme precipitation indices in Romania during three future periods: 2021–2040, 2041–2070, and 2071–2100. We investigated changes in future climate based on historical and modelled data sets of daily precipitation. We compared the values calculated for the three future periods with those obtained for the historical reference period 1961–1990. The historical observation data recorded at 30 weather stations and data extracted from six regional climate model outputs (ALADIN53, CCLM4-8-17, RACMO22E, RCA4, REMO2009, and WRF331F) under moderate (RCP4.5) and pessimistic (RCP8.5) scenarios were employed. Five indices established by the Expert Team for Climate Change Detection Monitoring and Indices were analysed: consecutive dry days, consecutive wet days, heavy precipitation days, very heavy precipitation days, and annual total wet-day precipitation. The series of indices were generated using ClimPACT2 software. Based on bias correction methods, the quality of the modelled data considerably increased, and the errors obtained for the daily precipitation varied in the range of ±0.05 to ±1.22 mm/day. The main findings revealed an increase in three of the extreme precipitation indices based on all models considered compared to the historical period. The most important increase (more than 50%) compared to the historical period was detected in the frequency of very heavy precipitation days and the annual total wet-day precipitation. They were followed by the heavy precipitation days index. The consecutive dry days index indicated mainly no change or a slow decrease, while inconsistencies among the results of regional climate models were detected for the consecutive wet days index. For all indices except the consecutive dry days index, the ALADIN53 and WRF331F models provided the highest projected values for both scenarios. The dispersion of values obtained as model output for each location was higher for RCP8.5 than for RCP4.5.en
dc.relation.ispartofInternational Journal of Climatologyen
dc.subjectClimPACT2en
dc.subjectextreme precipitation indicesen
dc.subjectfuture changesen
dc.subjectmodelled dataen
dc.subjectRomaniaen
dc.titleFuture changes in five extreme precipitation indices in the lowlands of Romaniaen
dc.typeArticleen
dc.identifier.doi10.1002/joc.6183en
dc.identifier.scopus2-s2.0-85068029714en
dc.identifier.urlhttps://api.elsevier.com/content/abstract/scopus_id/85068029714en
dc.relation.issue15en
dc.relation.volume39en
dc.relation.firstpage5720en
dc.relation.lastpage5740en
item.openairetypeArticle-
item.cerifentitytypePublications-
item.fulltextNo Fulltext-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.grantfulltextnone-
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