Spatial temporal variability of maximum flow in Slănic, Teleajen and Prahova River Basins

The present study analyzes the spatial temporal variation of maximum flow in Slănic Teleajen and Prahova river basins (upper basin). Maximum flow rates were analyzed in relation to the threshold values corresponding to the Defence Levels respectively the maximum flow which determines exceeding Warni...

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Main Author: Manolache Andreea-Violeta
Format: Article
Language:English
Published: Alexandru Ioan Cuza University Press, Iasi, Romania 2017-06-01
Series:Present Environment and Sustainable Development
Subjects:
Online Access:http://www.degruyter.com/view/j/pesd.2017.11.issue-1/pesd-2017-0019/pesd-2017-0019.xml?format=INT
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spelling doaj-52db5037669f4d3186619a463b7a63712020-12-02T18:01:44ZengAlexandru Ioan Cuza University Press, Iasi, RomaniaPresent Environment and Sustainable Development 2284-78202017-06-0111120921810.1515/pesd-2017-0019pesd-2017-0019Spatial temporal variability of maximum flow in Slănic, Teleajen and Prahova River BasinsManolache Andreea-Violeta0National Institute of Hydrology and Water Management, 97 București-Ploiești St., Sector 1, BucharestThe present study analyzes the spatial temporal variation of maximum flow in Slănic Teleajen and Prahova river basins (upper basin). Maximum flow rates were analyzed in relation to the threshold values corresponding to the Defence Levels respectively the maximum flow which determines exceeding Warning and Flooding Levels. The series of major floods events, selected on the basis of the threshold values mentioned above, were then statistically analyzed to determine trends (Mann-Kendall test) and the variations in the level of frequency, analysis which was applied seasonally and annually. The analysis made revealed that trends in terms of maximum flow rates in the Prahova upper basin were generally negative (decreasing), statistically significant for the February, May, July, August and the annual average, while in Slanic river basin, the trend was mostly positive, statistically significant for October.http://www.degruyter.com/view/j/pesd.2017.11.issue-1/pesd-2017-0019/pesd-2017-0019.xml?format=INTmaximum flowriver basinsdefence levelsflood
collection DOAJ
language English
format Article
sources DOAJ
author Manolache Andreea-Violeta
spellingShingle Manolache Andreea-Violeta
Spatial temporal variability of maximum flow in Slănic, Teleajen and Prahova River Basins
Present Environment and Sustainable Development
maximum flow
river basins
defence levels
flood
author_facet Manolache Andreea-Violeta
author_sort Manolache Andreea-Violeta
title Spatial temporal variability of maximum flow in Slănic, Teleajen and Prahova River Basins
title_short Spatial temporal variability of maximum flow in Slănic, Teleajen and Prahova River Basins
title_full Spatial temporal variability of maximum flow in Slănic, Teleajen and Prahova River Basins
title_fullStr Spatial temporal variability of maximum flow in Slănic, Teleajen and Prahova River Basins
title_full_unstemmed Spatial temporal variability of maximum flow in Slănic, Teleajen and Prahova River Basins
title_sort spatial temporal variability of maximum flow in slănic, teleajen and prahova river basins
publisher Alexandru Ioan Cuza University Press, Iasi, Romania
series Present Environment and Sustainable Development
issn 2284-7820
publishDate 2017-06-01
description The present study analyzes the spatial temporal variation of maximum flow in Slănic Teleajen and Prahova river basins (upper basin). Maximum flow rates were analyzed in relation to the threshold values corresponding to the Defence Levels respectively the maximum flow which determines exceeding Warning and Flooding Levels. The series of major floods events, selected on the basis of the threshold values mentioned above, were then statistically analyzed to determine trends (Mann-Kendall test) and the variations in the level of frequency, analysis which was applied seasonally and annually. The analysis made revealed that trends in terms of maximum flow rates in the Prahova upper basin were generally negative (decreasing), statistically significant for the February, May, July, August and the annual average, while in Slanic river basin, the trend was mostly positive, statistically significant for October.
topic maximum flow
river basins
defence levels
flood
url http://www.degruyter.com/view/j/pesd.2017.11.issue-1/pesd-2017-0019/pesd-2017-0019.xml?format=INT
work_keys_str_mv AT manolacheandreeavioleta spatialtemporalvariabilityofmaximumflowinslanicteleajenandprahovariverbasins
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