Particularities of periods with maximum water flow on the rivers from the Suceava hydrographic basin (1981–2005)

Suceava river basin gets its tributaries from the eastern slopes of the northern group of the Eastern Romanian Carpathians, situated under the influence of Baltic air masses, which bring rainfalls and cold weather, felt into the water flow regime of rivers in the region studied. This water flow reg...

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Main Author: ADRIANA MIHAELA PORCUȚAN
Format: Article
Language:English
Published: Casa Cartii de Stiinta Cluj-Napoca 2016-11-01
Series:Riscuri şi Catastrofe
Subjects:
Online Access:http://riscurisicatastrofe.reviste.ubbcluj.ro/Volume/XV_Nr_19_2_2016/pdf/7_Porcutan_89_102.pdf
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spelling doaj-80bed6908fcc42da8c4c0244887ea0582020-11-25T00:50:49ZengCasa Cartii de Stiinta Cluj-NapocaRiscuri şi Catastrofe1584-52732069-76942016-11-0120161989102Particularities of periods with maximum water flow on the rivers from the Suceava hydrographic basin (1981–2005)ADRIANA MIHAELA PORCUȚAN0Faculty of Geography, “Babeş-Bolyai” University, Cluj-Napoca, Romania Suceava river basin gets its tributaries from the eastern slopes of the northern group of the Eastern Romanian Carpathians, situated under the influence of Baltic air masses, which bring rainfalls and cold weather, felt into the water flow regime of rivers in the region studied. This water flow regime varies from month to month, with the maximum flow having the most important role in the restoration of underground water reserves. This study examines the temporal (frequency, duration and intensity) and quantitative (volume and flow) parameters of periods with maximum flow, at monthly and seasonal level, revealing the differences in the water flow regime induced by the relief’s morphometric particularities (altitude, fragmentation degree, exhibition). For the evaluation of mentioned parameters was appealed to the TML 2.1 extension from the HydroOffice software package, which uses quantitative thresholds, depending on which it is set the appearance, and disappearance of periods with maximum flow.http://riscurisicatastrofe.reviste.ubbcluj.ro/Volume/XV_Nr_19_2_2016/pdf/7_Porcutan_89_102.pdfmaximum flowquantitative thresholdfrequencyfloods
collection DOAJ
language English
format Article
sources DOAJ
author ADRIANA MIHAELA PORCUȚAN
spellingShingle ADRIANA MIHAELA PORCUȚAN
Particularities of periods with maximum water flow on the rivers from the Suceava hydrographic basin (1981–2005)
Riscuri şi Catastrofe
maximum flow
quantitative threshold
frequency
floods
author_facet ADRIANA MIHAELA PORCUȚAN
author_sort ADRIANA MIHAELA PORCUȚAN
title Particularities of periods with maximum water flow on the rivers from the Suceava hydrographic basin (1981–2005)
title_short Particularities of periods with maximum water flow on the rivers from the Suceava hydrographic basin (1981–2005)
title_full Particularities of periods with maximum water flow on the rivers from the Suceava hydrographic basin (1981–2005)
title_fullStr Particularities of periods with maximum water flow on the rivers from the Suceava hydrographic basin (1981–2005)
title_full_unstemmed Particularities of periods with maximum water flow on the rivers from the Suceava hydrographic basin (1981–2005)
title_sort particularities of periods with maximum water flow on the rivers from the suceava hydrographic basin (1981–2005)
publisher Casa Cartii de Stiinta Cluj-Napoca
series Riscuri şi Catastrofe
issn 1584-5273
2069-7694
publishDate 2016-11-01
description Suceava river basin gets its tributaries from the eastern slopes of the northern group of the Eastern Romanian Carpathians, situated under the influence of Baltic air masses, which bring rainfalls and cold weather, felt into the water flow regime of rivers in the region studied. This water flow regime varies from month to month, with the maximum flow having the most important role in the restoration of underground water reserves. This study examines the temporal (frequency, duration and intensity) and quantitative (volume and flow) parameters of periods with maximum flow, at monthly and seasonal level, revealing the differences in the water flow regime induced by the relief’s morphometric particularities (altitude, fragmentation degree, exhibition). For the evaluation of mentioned parameters was appealed to the TML 2.1 extension from the HydroOffice software package, which uses quantitative thresholds, depending on which it is set the appearance, and disappearance of periods with maximum flow.
topic maximum flow
quantitative threshold
frequency
floods
url http://riscurisicatastrofe.reviste.ubbcluj.ro/Volume/XV_Nr_19_2_2016/pdf/7_Porcutan_89_102.pdf
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