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...
Main Author: | |
---|---|
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 |
id |
doaj-52db5037669f4d3186619a463b7a6371 |
---|---|
record_format |
Article |
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 |
_version_ |
1724404376547622912 |