MONTHLY AVERAGE FLOW IN RÂUL NEGRU HYDROGRAPHIC BASIN

Râul Negru hydrographic basin represents a well individualised and relatively homogenous physical-geographical unity from Braşov Depression. The flow is controlled by six hydrometric stations placed on the main collector and on two of the most powerful tributaries. Our analysis period is represented...

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Main Author: VIGH MELINDA
Format: Article
Language:English
Published: Cluj University Press 2014-03-01
Series:Aerul şi Apa: Componente ale Mediului
Subjects:
Online Access:http://aerapa.conference.ubbcluj.ro/2014/PDF/38-Vigh%20M.pdf
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spelling doaj-03b473f797c14aa997d8df424c6933972020-11-24T23:38:17ZengCluj University PressAerul şi Apa: Componente ale Mediului2067-743X2067-743X2014-03-012014286292MONTHLY AVERAGE FLOW IN RÂUL NEGRU HYDROGRAPHIC BASINVIGH MELINDA0Babeş Bolyai University, Faculty of Environmental Sciences and Engineering, Cluj - Napoca, RomaniaRâul Negru hydrographic basin represents a well individualised and relatively homogenous physical-geographical unity from Braşov Depression. The flow is controlled by six hydrometric stations placed on the main collector and on two of the most powerful tributaries. Our analysis period is represented by the last 25 years (1988 - 2012) and it’s acceptable for make pertinent conclusions. The maximum discharge month is April, that it’s placed in the high flow period: March – June. Minimum discharges appear in November - because of the lack of pluvial precipitations; in January because of high solid precipitations and because of water volume retention in ice. Extreme discharge frequencies vary according to their position: in the mountain area – small basin surface; into a depression – high basin surface. Variation coefficients point out very similar variation principles, showing a relative homogeneity of flow processes.http://aerapa.conference.ubbcluj.ro/2014/PDF/38-Vigh%20M.pdfmonthly average flowspace-time variationflow principlesoccurrence frequencyvariation coefficient
collection DOAJ
language English
format Article
sources DOAJ
author VIGH MELINDA
spellingShingle VIGH MELINDA
MONTHLY AVERAGE FLOW IN RÂUL NEGRU HYDROGRAPHIC BASIN
Aerul şi Apa: Componente ale Mediului
monthly average flow
space-time variation
flow principles
occurrence frequency
variation coefficient
author_facet VIGH MELINDA
author_sort VIGH MELINDA
title MONTHLY AVERAGE FLOW IN RÂUL NEGRU HYDROGRAPHIC BASIN
title_short MONTHLY AVERAGE FLOW IN RÂUL NEGRU HYDROGRAPHIC BASIN
title_full MONTHLY AVERAGE FLOW IN RÂUL NEGRU HYDROGRAPHIC BASIN
title_fullStr MONTHLY AVERAGE FLOW IN RÂUL NEGRU HYDROGRAPHIC BASIN
title_full_unstemmed MONTHLY AVERAGE FLOW IN RÂUL NEGRU HYDROGRAPHIC BASIN
title_sort monthly average flow in râul negru hydrographic basin
publisher Cluj University Press
series Aerul şi Apa: Componente ale Mediului
issn 2067-743X
2067-743X
publishDate 2014-03-01
description Râul Negru hydrographic basin represents a well individualised and relatively homogenous physical-geographical unity from Braşov Depression. The flow is controlled by six hydrometric stations placed on the main collector and on two of the most powerful tributaries. Our analysis period is represented by the last 25 years (1988 - 2012) and it’s acceptable for make pertinent conclusions. The maximum discharge month is April, that it’s placed in the high flow period: March – June. Minimum discharges appear in November - because of the lack of pluvial precipitations; in January because of high solid precipitations and because of water volume retention in ice. Extreme discharge frequencies vary according to their position: in the mountain area – small basin surface; into a depression – high basin surface. Variation coefficients point out very similar variation principles, showing a relative homogeneity of flow processes.
topic monthly average flow
space-time variation
flow principles
occurrence frequency
variation coefficient
url http://aerapa.conference.ubbcluj.ro/2014/PDF/38-Vigh%20M.pdf
work_keys_str_mv AT vighmelinda monthlyaverageflowinraulnegruhydrographicbasin
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