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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Cluj University Press
2014-03-01
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Online Access: | http://aerapa.conference.ubbcluj.ro/2014/PDF/38-Vigh%20M.pdf |
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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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1725517214379933696 |