Spatial Flow and Outflow Distribution in the Una Basin

Aida Korjenić

doi:doi:10.11648/j.hyd.20180602.12

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Spatial Flow and Outflow Distribution in the Una Basin

Aida Korjenić

Published in Hydrology (Volume 6, Issue 2)

Received: 27 April 2018 Accepted: 17 May 2018 Published: 4 July 2018

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Abstract

The need and importance of studying the water regime in higher and mountainous areas, as well as hypsometric zoning are extremely large in regional and spatial planning. The aspect of spatial regionalization has enabled the understanding of the distribution of water in the basin itself. Based on that, a wider picture of the state of this distribution was obtained in some regional units. Getting involved in solving issues related to gaining values of the river regime’s certain elements by hypsometric zones in the Una basin, the basic parameter which it was started from, was determining the value of precipitation amount. For assessment of flow and specific outflow and height, the relation has been applied: precipitation – elevation – area of hypsometric zones – evapotranspiration. Depending on the area they occupy, in the structure of specific outflows and flows, one can clearly distinguish three zones, up to 400 m altitude, the second hypsometric zone from 400 m up to 1400 m, and the third zone above 1400 m altitude. To determine the water height distribution, there have been used the hypsography of the basin and regional specific outflow dependence on average elevation of the basin. Processing all parameters relevant for studying in this paper is done in the ArcGIS software package. The obtained results of this research are very important and can be applied for the needs of agriculture, water management, urbanism and tourism of this part of Bosnia and Herzegovina.

Published in	Hydrology (Volume 6, Issue 2)
DOI	10.11648/j.hyd.20180602.12
Page(s)	53-60
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2018. Published by Science Publishing Group

Keywords

Flow, Specific Outflow, Precipitation, Hypsometric Zoning, Una, GIS

References

[1]	A. Korjenić, E. Temimović, A. Banda, and Sivac, A., “Basic Characteristics of The Pluviometric Regime in The Una River Basin”, International Journal of Research – Granthaalayah, 6 (2), pp. 234–245, 2018.
[2]	A. Korjenić, “The Una River - physical-geographical conditions of hypsometric zoning waters in the basin”, doctoral dissertations, Sarajevo: Faculty of Science, Department of Geography, University of Sarajevo, 2015, pp. 38.
[3]	A. Korjenić, “Isohyet and evapotranspiration elements in wather regime of the river Una”, Acta geographica Bosniae et Herzegovinae, Vol. 1, No. 1, Sarajevo: Association of Geographers in B&H, pp. 114–123, 2014.
[4]	S. Mustafić, “Spatial Distribution of Runoff in Temstica River Basin”, Beograd: Bulletin of The Serbian Geographical Society, Vol. LXXXVI - No 2, pp. 45–52.
[5]	M. Ocokoljić, “Height zoning water in the basin of the Velika Morava and some aspects of their protection”, Special edition, Vol. 64, Beograd: Serbian Geographical Society, 1987.
[6]	Y. M. Semenov, “Landscape planning: The applied branch in complex physical geography”, Geography and Natural Resources, Vol. 38, No. 4, Pleiades Publishing, Ltd., 2017, pp. 319–323.
[7]	I. Žigić, F. Skopljak, H. Hrvatović, D. Pašić-Škripić, “Hydrogeological regionization of the terrain in the Una River Basin on the territory of the Federation of Bosnia and Herzegovina”, Proceedings book, Tuzla: Faculty of Mining and Geology, University of Tuzla, 2010.
[8]	M. F. Rahaman, C. S. Jahan, R. Arefin, Q. H. Mazumder, “Morphometric Analysis of Major Watersheds in Barind Tract, Bangladesh: A Remote Sensing and GIS - Based Approach for Water Resource Management”, Hydrology. Vol. 5, No. 6, 2017, pp. 86-95. doi: 10.11648/j.hyd.20170506.12.
[9]	A. Korjenić, A. Sivac, Š. Okerić, “Geological Characteristics and Density of the Una Water System as a Factor of Spatial Planning, B&H”, Journal of International Environmental Application & Science, Vol. 12, No. 1, pp. 63–72, 2017.
[10]	A. Korjenić, S. Herenda, “The influence of Geological Field Structure on Water Quality in the Selected Source of the Ljubija Area, B&H”, Journal of International Environmental Application & Science, Vol. 11, No. 2, pp. 180–185, 2016.

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APA Style

Aida Korjenić. (2018). Spatial Flow and Outflow Distribution in the Una Basin. Hydrology, 6(2), 53-60. https://doi.org/10.11648/j.hyd.20180602.12

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ACS Style

Aida Korjenić. Spatial Flow and Outflow Distribution in the Una Basin. Hydrology. 2018, 6(2), 53-60. doi: 10.11648/j.hyd.20180602.12

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AMA Style

Aida Korjenić. Spatial Flow and Outflow Distribution in the Una Basin. Hydrology. 2018;6(2):53-60. doi: 10.11648/j.hyd.20180602.12

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@article{10.11648/j.hyd.20180602.12,
  author = {Aida Korjenić},
  title = {Spatial Flow and Outflow Distribution in the Una Basin},
  journal = {Hydrology},
  volume = {6},
  number = {2},
  pages = {53-60},
  doi = {10.11648/j.hyd.20180602.12},
  url = {https://doi.org/10.11648/j.hyd.20180602.12},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.hyd.20180602.12},
  abstract = {The need and importance of studying the water regime in higher and mountainous areas, as well as hypsometric zoning are extremely large in regional and spatial planning. The aspect of spatial regionalization has enabled the understanding of the distribution of water in the basin itself. Based on that, a wider picture of the state of this distribution was obtained in some regional units. Getting involved in solving issues related to gaining values of the river regime’s certain elements by hypsometric zones in the Una basin, the basic parameter which it was started from, was determining the value of precipitation amount. For assessment of flow and specific outflow and height, the relation has been applied: precipitation – elevation – area of hypsometric zones – evapotranspiration. Depending on the area they occupy, in the structure of specific outflows and flows, one can clearly distinguish three zones, up to 400 m altitude, the second hypsometric zone from 400 m up to 1400 m, and the third zone above 1400 m altitude. To determine the water height distribution, there have been used the hypsography of the basin and regional specific outflow dependence on average elevation of the basin. Processing all parameters relevant for studying in this paper is done in the ArcGIS software package. The obtained results of this research are very important and can be applied for the needs of agriculture, water management, urbanism and tourism of this part of Bosnia and Herzegovina.},
 year = {2018}
}

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TY  - JOUR
T1  - Spatial Flow and Outflow Distribution in the Una Basin
AU  - Aida Korjenić
Y1  - 2018/07/04
PY  - 2018
N1  - https://doi.org/10.11648/j.hyd.20180602.12
DO  - 10.11648/j.hyd.20180602.12
T2  - Hydrology
JF  - Hydrology
JO  - Hydrology
SP  - 53
EP  - 60
PB  - Science Publishing Group
SN  - 2330-7617
UR  - https://doi.org/10.11648/j.hyd.20180602.12
AB  - The need and importance of studying the water regime in higher and mountainous areas, as well as hypsometric zoning are extremely large in regional and spatial planning. The aspect of spatial regionalization has enabled the understanding of the distribution of water in the basin itself. Based on that, a wider picture of the state of this distribution was obtained in some regional units. Getting involved in solving issues related to gaining values of the river regime’s certain elements by hypsometric zones in the Una basin, the basic parameter which it was started from, was determining the value of precipitation amount. For assessment of flow and specific outflow and height, the relation has been applied: precipitation – elevation – area of hypsometric zones – evapotranspiration. Depending on the area they occupy, in the structure of specific outflows and flows, one can clearly distinguish three zones, up to 400 m altitude, the second hypsometric zone from 400 m up to 1400 m, and the third zone above 1400 m altitude. To determine the water height distribution, there have been used the hypsography of the basin and regional specific outflow dependence on average elevation of the basin. Processing all parameters relevant for studying in this paper is done in the ArcGIS software package. The obtained results of this research are very important and can be applied for the needs of agriculture, water management, urbanism and tourism of this part of Bosnia and Herzegovina.
VL  - 6
IS  - 2
ER  -

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Aida Korjenić

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APA Style

Aida Korjenić. (2018). Spatial Flow and Outflow Distribution in the Una Basin. Hydrology, 6(2), 53-60. https://doi.org/10.11648/j.hyd.20180602.12

Copy | Download

ACS Style

Aida Korjenić. Spatial Flow and Outflow Distribution in the Una Basin. Hydrology. 2018, 6(2), 53-60. doi: 10.11648/j.hyd.20180602.12

Copy | Download

AMA Style

Aida Korjenić. Spatial Flow and Outflow Distribution in the Una Basin. Hydrology. 2018;6(2):53-60. doi: 10.11648/j.hyd.20180602.12

Copy | Download

@article{10.11648/j.hyd.20180602.12,
  author = {Aida Korjenić},
  title = {Spatial Flow and Outflow Distribution in the Una Basin},
  journal = {Hydrology},
  volume = {6},
  number = {2},
  pages = {53-60},
  doi = {10.11648/j.hyd.20180602.12},
  url = {https://doi.org/10.11648/j.hyd.20180602.12},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.hyd.20180602.12},
  abstract = {The need and importance of studying the water regime in higher and mountainous areas, as well as hypsometric zoning are extremely large in regional and spatial planning. The aspect of spatial regionalization has enabled the understanding of the distribution of water in the basin itself. Based on that, a wider picture of the state of this distribution was obtained in some regional units. Getting involved in solving issues related to gaining values of the river regime’s certain elements by hypsometric zones in the Una basin, the basic parameter which it was started from, was determining the value of precipitation amount. For assessment of flow and specific outflow and height, the relation has been applied: precipitation – elevation – area of hypsometric zones – evapotranspiration. Depending on the area they occupy, in the structure of specific outflows and flows, one can clearly distinguish three zones, up to 400 m altitude, the second hypsometric zone from 400 m up to 1400 m, and the third zone above 1400 m altitude. To determine the water height distribution, there have been used the hypsography of the basin and regional specific outflow dependence on average elevation of the basin. Processing all parameters relevant for studying in this paper is done in the ArcGIS software package. The obtained results of this research are very important and can be applied for the needs of agriculture, water management, urbanism and tourism of this part of Bosnia and Herzegovina.},
 year = {2018}
}

Copy | Download

TY  - JOUR
T1  - Spatial Flow and Outflow Distribution in the Una Basin
AU  - Aida Korjenić
Y1  - 2018/07/04
PY  - 2018
N1  - https://doi.org/10.11648/j.hyd.20180602.12
DO  - 10.11648/j.hyd.20180602.12
T2  - Hydrology
JF  - Hydrology
JO  - Hydrology
SP  - 53
EP  - 60
PB  - Science Publishing Group
SN  - 2330-7617
UR  - https://doi.org/10.11648/j.hyd.20180602.12
AB  - The need and importance of studying the water regime in higher and mountainous areas, as well as hypsometric zoning are extremely large in regional and spatial planning. The aspect of spatial regionalization has enabled the understanding of the distribution of water in the basin itself. Based on that, a wider picture of the state of this distribution was obtained in some regional units. Getting involved in solving issues related to gaining values of the river regime’s certain elements by hypsometric zones in the Una basin, the basic parameter which it was started from, was determining the value of precipitation amount. For assessment of flow and specific outflow and height, the relation has been applied: precipitation – elevation – area of hypsometric zones – evapotranspiration. Depending on the area they occupy, in the structure of specific outflows and flows, one can clearly distinguish three zones, up to 400 m altitude, the second hypsometric zone from 400 m up to 1400 m, and the third zone above 1400 m altitude. To determine the water height distribution, there have been used the hypsography of the basin and regional specific outflow dependence on average elevation of the basin. Processing all parameters relevant for studying in this paper is done in the ArcGIS software package. The obtained results of this research are very important and can be applied for the needs of agriculture, water management, urbanism and tourism of this part of Bosnia and Herzegovina.
VL  - 6
IS  - 2
ER  -

Copy | Download