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dc.contributor.authorSan, Murat
dc.contributor.authorAkcay, Fatma
dc.contributor.authorLinh, Nguyen Thi Thuy
dc.contributor.authorKankal, Murat
dc.contributor.authorPham, Quoc Bao
dc.date.accessioned2021-11-09T19:49:49Z
dc.date.available2021-11-09T19:49:49Z
dc.date.issued2021
dc.identifier.issn0177-798X
dc.identifier.issn1434-4483
dc.identifier.urihttps://doi.org/10.1007/s00704-021-03574-4
dc.identifier.urihttps://hdl.handle.net/20.500.12440/4132
dc.description.abstractIt is a known fact that the size, frequency, and spatial variability of hydrometeorological variables will irregularly increase under the impact of climate change. Among the hydrometeorological variables, rainfall is one of the most important. Trend analysis is one of the most effective methods of observing the effects of climate change on rainfall. Recently, new graphical methods have been proposed as an alternative to classical trend analysis methods. Innovative Polygon Trend Analysis (IPTA), which evolved from Innovative Trend Analysis (ITA), is currently one of the proposed methods and it does not contain any assumptions. The aim of this study is to compare IPTA, ITA with the Significance Test and Mann-Kendall (MK) methods. To achieve this, the monthly total rainfall trends of 15 stations in the Vu Gia-Thu Bon River Basin (VGTBRB) of Vietnam have been examined for the period 1979-2016. The analyses show that rainfall tends to increase (decrease) in March (June) at nearly all stations. IPTA and ITA with the Significance Test are more sensitive than MK in determining the trends. While trends were detected in approximately 90% of all months in IPTA and ITA with the Significance Test, this rate was only 23% in the MK test. Although the arithmetic mean graphs in the 1-year hydrometeorological cycle are considerably regular at almost all stations, their standard deviations are relatively irregular. The most critical month for trend transitions between consecutive months for all the stations is October, which has an average trend slope of -1.35 and a trend slope ranging from -3.98 to -0.21, which shows a decreasing trend.en_US
dc.language.isoengen_US
dc.publisherSpringer Wienen_US
dc.relation.ispartofTheoretical and Applied Climatologyen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectGraphical trend methodsen_US
dc.subjectInnovative trenden_US
dc.subjectMonthly rainfallen_US
dc.subjectPolygon trenden_US
dc.subjectVietnamen_US
dc.titleInnovative and polygonal trend analyses applications for rainfall data in Vietnamen_US
dc.typearticleen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.description.wospublicationidWOS:000623702000001en_US
dc.description.scopuspublicationid2-s2.0-85101941818en_US
dc.departmentGümüşhane Üniversitesien_US
dc.authoridLinh, NTT / 0000-0001-8631-9941
dc.authoridSAN, MURAT / 0000-0001-7006-8340
dc.authoridPham, Quoc Bao / 0000-0002-0468-5962
dc.identifier.volume144en_US
dc.identifier.issue3-4en_US
dc.identifier.startpage809en_US
dc.identifier.doi10.1007/s00704-021-03574-4
dc.identifier.endpage822en_US
dc.authorwosidLinh, NTT / AAJ-2377-2020
dc.authorwosidSAN, MURAT / AAC-6221-2021
dc.authorwosidPham, Quoc Bao / AAD-5611-2020
dc.authorscopusid57219328578
dc.authorscopusid57222226657
dc.authorscopusid57211268069
dc.authorscopusid24471611900
dc.authorscopusid57208495034


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