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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Casa Cartii de Stiinta Cluj-Napoca
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Online Access: | http://riscurisicatastrofe.reviste.ubbcluj.ro/Volume/XV_Nr_19_2_2016/pdf/7_Porcutan_89_102.pdf |
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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 |
work_keys_str_mv |
AT adrianamihaelaporcutan particularitiesofperiodswithmaximumwaterflowontheriversfromthesuceavahydrographicbasin19812005 |
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1725246434898345984 |