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Decadal Spatial-Temporal Variations in the Spatial Pattern of Anomalies of Extreme Precipitation Thresholds (Case Study: Northwest Iran)

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dc.contributor Háskóli Íslands
dc.contributor University of Iceland
dc.contributor.author Rousta, Iman
dc.contributor.author Nasserzadeh, Mohammad
dc.contributor.author Jalali, Masoud
dc.contributor.author Haghighi, Esmaeil
dc.contributor.author Olafsson, Haraldur
dc.contributor.author Ashrafi, Saeide
dc.contributor.author Doostkamian, Mehdi
dc.contributor.author Ghasemi, Ali
dc.date.accessioned 2017-10-05T13:28:14Z
dc.date.available 2017-10-05T13:28:14Z
dc.date.issued 2017-08-03
dc.identifier.citation Rousta, I.; Nasserzadeh, M.H.; Jalali, M.; Haghighi, E.; Ólafsson, H.; Ashrafi, S.; Doostkamian, M.; Ghasemi, A. Decadal Spatial-Temporal Variations in the Spatial Pattern of Anomalies of Extreme Precipitation Thresholds (Case Study: Northwest Iran). Atmosphere 2017, 8, 135. doi:10.3390/atmos8080135
dc.identifier.issn 2073-4433
dc.identifier.uri https://hdl.handle.net/20.500.11815/426
dc.description.abstract This study focused on decadalvariations of extreme precipitation thresholds within a 50-year period (1961–2010) for 250 stations of Iran’s northwest. The 99th percentile was used as the threshold of extreme precipitation. In order to analyze threshold cycles and spatial autocorrelation pattern dominating extreme precipitation thresholds, spectral analysis and Gi (known as HOTSPOT) were used respectively. The results revealed that the highest threshold of extreme precipitation occurred along the Ghoosheh Dagh mountain range. Additionally, in all the five studied decades, the highest positive anomalies were observed in the same region (i.e., the Ghoosheh Dagh). The findings also showed that the intensity of positive spatial autocorrelation pattern of extreme precipitation thresholds experienced a declining trend in recent decades. At the same time, extreme precipitation weighted mean center indicated that they followed an ordered pattern during the studied period. The results of harmonic analysis demonstrated that, in all decades, short-term (2–4 years) and mid-term (4–8 years) cycles of extreme precipitation thresholds were dominated. However, especially the southwest of the studied area, the return period of extreme precipitation thresholds was as long as the studied period, a phenomenon that indicates the existence of a trend in extreme precipitation thresholds of these regions.
dc.format.extent 135
dc.language.iso en
dc.publisher MDPI AG
dc.relation.ispartofseries Atmosphere;8(8)
dc.rights info:eu-repo/semantics/openAccess
dc.subject Extreme precipitation threshold
dc.subject Anomaly
dc.subject Weighted mean center
dc.subject Gi
dc.subject Harmonic analysis
dc.subject Iran
dc.subject Veðurfarsrannsóknir
dc.subject Veðurfarsbreytingar
dc.subject Loftslagsrannsóknir
dc.title Decadal Spatial-Temporal Variations in the Spatial Pattern of Anomalies of Extreme Precipitation Thresholds (Case Study: Northwest Iran)
dc.type info:eu-repo/semantics/article
dcterms.license This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. (CC BY 4.0).
dc.description.version Peer Reviewed
dc.identifier.journal Atmosphere
dc.identifier.doi 10.3390/atmos8080135
dc.relation.url http://www.mdpi.com/2073-4433/8/8/135/pdf
dc.contributor.department Raunvísindadeild (HÍ)
dc.contributor.department Faculty of Physical Sciences (UI)
dc.contributor.school Verkfræði- og náttúruvísindasvið (HÍ)
dc.contributor.school School of Engineering and Natural Sciences (UI)


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