A long-term annual water balance analysis of the Araçuaí River Basin, Brazil

2010 ◽  
Vol 20 (6) ◽  
pp. 938-946 ◽  
Author(s):  
Mariangela Garcia Praça Leite ◽  
Maria Augusta Gonçalves Fujaco
2005 ◽  
Vol 48 (1-3) ◽  
pp. 84-95 ◽  
Author(s):  
S BEREZOVSKAYA ◽  
D YANG ◽  
L HINZMAN

2008 ◽  
Author(s):  
Gary M Chauvin ◽  
Gerald N Flerchinger ◽  
Timothy E Link ◽  
Danny Marks ◽  
Adam H Winstral

2013 ◽  
Vol 7 (3) ◽  
pp. 354-359

Estimation of annual water balance is critical for water management and developmental planning in the area of Anthemountas river basin. In the framework of LIFE04/ENV/GR/000099 project and in continuance to prior projects in the area, the average annual water balance was estimated using the annual precipitation and water consumption. The statistic relationship between elevation and precipitation measured at different stations in the greater area, was applied to the Digital Elevation Model (DEM) (accuracy 20X20m) and the spatial distribution of annual precipitation is calculated for the Anthemountas river basin. Consumption of underground water was analytically calculated based on the different types of agricultural activities as annually reported by the Ministry of Agriculture. The Domestic water consumption was also calculated. Evaportranspiration is estimated analytically using two different methods (Thorthwaite’s and Turk’s). Both methods gave similar results. Moreover the spatial distribution of infiltration and runoff coefficients were calculated taking into consideration the different geological features, since they determine the maximum value of the infiltration coefficient, and the CORINE land coverage classification assuming no infiltration at builded areas. All the above were calculated and presented in raster format using the ESRI ArcGIS 9 environment. The correlation between the negative water balance and the drop of the underground water level, as this was pictured through underground water level measurements in the past decade, was discussed and evaluated. To further understand the relationship between the negative water balance and the spatial distribution of the underground water level drop, the most consuming wells in the Anthemountas river basin are distributed and categorized based on consumption estimates. Future work should assess more precise land coverage dataset in order to produce spatial distribution of evaportranspiration. At the same time, precise precipitation datasets, that will be produced by the meteorological monitoring network, that is to be established in the LIFE04/ENV/GR/000099 project framework, will provide more accurate estimates of precipitation distribution. This will lead to the determination of more accurate estimates for both infiltration and runoff in the basin. Data monitoring, assessment and water balance estimation are valuable tools in a step-by-step procedure towards the achievement of sustainable use of water in the river basin of Anthemountas.


2021 ◽  
Vol 36 ◽  
pp. 100837
Author(s):  
Mou Leong Tan ◽  
Yi Lin Tew ◽  
Kwok Pan Chun ◽  
Narimah Samat ◽  
Shazlyn Milleana Shaharudin ◽  
...  

2009 ◽  
Vol 65 (1) ◽  
pp. 69-76 ◽  
Author(s):  
Tomoyoshi HIROTA ◽  
Yukiyoshi IWATA ◽  
Manabu NEMOTO ◽  
Takahiro HAMASAKI ◽  
Ryoji SAMESHIMA ◽  
...  

2021 ◽  
Author(s):  
Renata Romanowicz ◽  
Emilia Karamuz ◽  
Jaroslaw Napiorkowski ◽  
Tesfaye Senbeta

<div> <p>Water balance modelling is often applied in studies of climate and human impacts on water resources. Annual water balance is usually derived based on precipitation, discharge and temperature observations under an assumption of negligible changes in annual water storage in a catchment. However, that assumption might be violated during very dry or very wet years. In this study we apply groundwater level measurements to improve water balance modelling in nine sub-catchments of the River Vistula basin starting from the river sources downstream. Annual and inter-annual water balance is studied using a Budyko framework to assess actual evapotranspiration and total water supply. We apply the concept of effective precipitation to account for possible losses due to water interception by vegetation. Generalised Likelihood Uncertainty Estimation GLUE is used to account for parameter and structural model uncertainty, together with the application of eight Budyko-type equations. Seasonal water balance models show large errors for winter seasons while summer and annual water balance models follow the Budyko framework. The dryness index is much smaller in winter than in summer for all sub-catchments. The spatial variability of water balance modelling errors indicate an increasing uncertainty of model predictions with an increase in catchment size. The results show that the added information on storage changes in the catchments provided by groundwater level observations largely improves model accuracy. The results also indicate the need to model groundwater level variability depending on external factors such as precipitation and evapotranspiration and human interventions. The modelling tools developed will be used to assess future water balance in the River Vistula basin under different water management scenarios and climate variability.</p> </div>


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