Estimation of the groundwater balance of a mountainous basin based on long-term streamflow data: a case study of the Tao’er River Basin, China

2021 ◽  
Vol 80 (20) ◽  
Author(s):  
Weifei Yang ◽  
Changlai Xiao ◽  
Zhihao Zhang ◽  
Xiujuan Liang ◽  
Zhang Fang
Author(s):  
Heinz Dieter FILL ◽  
Irani Dos SANTOS ◽  
Cristovão FERNANDES ◽  
André TOCZECK ◽  
Mariana Fiorin De OLIVEIRA

O presente trabalho estabelece o balanço hídrico mensal da bacia do rio Barigüi para o período de 1985 a 2000, determinando para cada mês o armazenamento ativo de água na bacia. Foi utilizado um método de ajuste de evapotranspiração calculado com dados meteorológicos observados fora da bacia em análise. Para a evapotranspiração utilizaram-se estimativas médias de longo prazo da diferença entre precipitação e deflúvio, que foram ajustadas adotando a proporcionalidade entre armazenamento na bacia e evapotranspiração real. A contribuição do despejo de esgoto doméstico foi estimada a partir de dados demográficos sobre a população residente na bacia. Os fluxos de água subterrânea para dentro e fora da bacia foram desprezados. Os resultados obtidos foram coerentes com estudos similares realizados na mesma região e mostram uma precipitação média no período de 1.251 mm e um deflúvio médio de 751 mm com um coeficiente de escoamento médio de 0,50. Water balance of the Barigüi river basin in Paraná State - Brazil Abstract This paper consolidates the water balance of the Barigui River in the Metropolitan Area of Curitiba for the period of time 1985-2000, defining for each month the watershed storage. It is proposed an evapotranspiration approximation based upon meteorological data measured close to the watershed. Evapotranspiration is estimated using long term averages of the differences between precipitation and streamflow data adjusted by assuming that storage and real evapotranspiration are proportional. The sewage contribution was estimated by watershed demographic data. The results are consistent with similar studies and show an average precipitation amplitude of 1251 mm and streamflow of 751 mm over the period analyzed.


2014 ◽  
Vol 73 ◽  
pp. 192-200 ◽  
Author(s):  
P.J. García Nieto ◽  
E. García-Gonzalo ◽  
J.R. Alonso Fernández ◽  
C. Díaz Muñiz

2021 ◽  
Vol 250 ◽  
pp. 105380
Author(s):  
Célia Soares de Brito ◽  
Richarde Marques da Silva ◽  
Celso Augusto Guimarães Santos ◽  
Reginaldo Moura Brasil Neto ◽  
Victor Hugo Rabelo Coelho

2013 ◽  
Vol 17 (5) ◽  
pp. 2069-2081 ◽  
Author(s):  
T. A. Räsänen ◽  
C. Lehr ◽  
I. Mellin ◽  
P. J. Ward ◽  
M. Kummu

Abstract. Globally, there have been many extreme weather events in recent decades. A challenge has been to determine whether these extreme weather events have increased in number and intensity compared to the past. This challenge is made more difficult due to the lack of long-term instrumental data, particularly in terms of river discharge, in many regions including Southeast Asia. Thus our main aim in this paper is to develop a river basin scale approach for assessing interannual hydrometeorological and discharge variability on long, palaeological, time scales. For the development of the basin-wide approach, we used the Mekong River basin as a case study area, although the approach is also intended to be applicable to other basins. Firstly, we derived a basin-wide Palmer Drought Severity Index (PDSI) from the Monsoon Asia Drought Atlas (MADA). Secondly, we compared the basin-wide PDSI with measured discharge to validate our approach. Thirdly, we used basin-wide PDSI to analyse the hydrometeorology and discharge of the case study area over the study period of 1300–2005. For the discharge-MADA comparison and hydrometeorological analyses, we used methods such as linear correlations, smoothing, moving window variances, Levene type tests for variances, and wavelet analyses. We found that the developed basin-wide approach based on MADA can be used for assessing long-term average conditions and interannual variability for river basin hydrometeorology and discharge. It provides a tool for studying interannual discharge variability on a palaeological time scale, and therefore the approach contributes to a better understanding of discharge variability during the most recent decades. Our case study revealed that the Mekong has experienced exceptional levels of interannual variability during the post-1950 period, which could not be observed in any other part of the study period. The increased variability was found to be at least partly associated with increased El Niño Southern Oscillation (ENSO) activity.


2002 ◽  
Vol 2 (4) ◽  
pp. 35-57 ◽  
Author(s):  
Kathryn Hochstetler

This article focuses on one common transnational NGO strategy, the boomerang strategy. In this strategy, Southern NGOs seek international allies to help them pressure their states from outside. The article uses a case study of a transnational mobilization against a water superhighway or “Hidrovia” in the La Plata River basin in South America to develop arguments about the long term impacts of throws of the boomerang. I argue that what happens after the boomerang depends on two related factors: the extent to which the target state(s) have accepted the international norms at stake and the presence or absence of a specific set of domestic capacities in the target state(s). Because Brazil has higher levels of national environmental legal capacity and greater acceptance of international environmental norms than its neighbors, environmentalists were able to block the Hidrovia there after the successful collective pressure, while Argentine environmentalists were not.


Ecohydrology ◽  
2014 ◽  
Vol 8 (1) ◽  
pp. 46-57 ◽  
Author(s):  
Wenfei Liu ◽  
Xiaohua Wei ◽  
Shirong Liu ◽  
Yuanqiu Liu ◽  
Houbao Fan ◽  
...  
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