South-American Transboundary Waters: The Management of the Guarani Aquifer System and the La Plata Basin Towards the Future

Author(s):  
Isabela Battistello Espindola ◽  
Maria Luisa Telarolli Almeida de Leite ◽  
Wagner Costa Ribeiro
2021 ◽  
pp. 251-285
Author(s):  
Isabela Battistello Espindola ◽  
Maria Luisa Telarolli Almeida de Leite ◽  
Wagner Costa Ribeiro

2019 ◽  
Vol 149 ◽  
pp. 103986 ◽  
Author(s):  
E. Avigliano ◽  
C. Clavijo ◽  
P. Scarabotti ◽  
S. Sánchez ◽  
S. Llamazares Vegh ◽  
...  

Water Policy ◽  
2016 ◽  
Vol 18 (5) ◽  
pp. 1120-1138 ◽  
Author(s):  
Isabella Alcañiz ◽  
Ramiro Berardo

When do countries cooperate in transboundary waters? One of the largest in the world, the La Plata Basin covers part of Argentina, Bolivia, Brazil, Paraguay, and Uruguay. These five countries co-manage the basin through a network of legal agreements, domestic and international organizations, and cooperative projects. In this paper, we examine the network structure of cross-national water projects within this intergovernmental framework. We use exponential random graph models to analyze the processes that lead to the formation of particular network structures when organizations participate in projects designed to improve the management of natural resources in the basin. Empirical results provide evidence that: (1) the network is characterized by a considerable level of bridging capital, rather than bonding capital, with a small group of organizations capturing most of the present links in the network; and (2) organizations that are active in two or more countries – especially basin governmental organizations – are the main collaborators in projects. These findings point to the extent to which coordinated state actors dominate the La Plata Basin. Study results carry significant implications for how networks facilitate the resolution of coordination problems and the administration of common resources in transboundary waters.


Author(s):  
Paulo Rodrigo Zanin ◽  
Prakki Satyamurty

AbstractThe inter-seasonal and inter-basins hydrological couplings between the Amazon and the La Plata basins are obtained with the help of ERA-5 atmospheric reanalysis, MERGE/CPTEC precipitation, GLEAM evapotranspiration and the GLDAS/Noah soil moisture datasets. The hypotheses formulated by Zanin and Satyamurty (2020a) about the hydrological processes interconnecting the Amazon Basin and the La Plata Basin are tested. A new method for finding the source-sink relationships among the boxes (regions) is presented. The precipitation recycling, frequency of source-sink behaviors, the soil moisture memory and the continental moisture transport between remote regions are evaluated. The main result of this study is that the amount of water precipitated over the Southeastern region of the Amazon Basin at the end of the South American Monsoon during autumn season, influences the amount of precipitation during winter season over the Central-western region of the La Plata Basin.


2009 ◽  
Vol 27 (2) ◽  
pp. 645-657 ◽  
Author(s):  
G. A. M. Silva ◽  
T. Ambrizzi ◽  
J. A. Marengo

Abstract. The differences on the phase and wavelength of the quasi-stationary waves over the South America generated by El Niño (EN) and La Niña (LN) events seem to affect the daily evolution of the South American Low Level Jet east of the Andes (SALLJ). For the austral summer period of 1977–2004 the SALLJ episodes detected according to Bonner criterion 1 show normal to above-normal frequency in EN years, and in LN years the episodes show normal to below-normal frequency. During EN and LN years the SALLJ episodes were associated with positive rainfall anomalies over the La Plata Basin, but more intense during LN years. During EN years the increase in the SALLJ cases were associated to intensification of the Subtropical Jet (SJ) around 30° S and positive Sea Level Pressure (SLP) anomalies over the western equatorial Atlantic and tropical South America, particularly over central Brazil. This favored the intensification of the northeasterly trade winds over the northern continent and it channeled by the Andes mountain to the La Plata Basin region where negative SLP are found. The SALLJ cases identified during the LN events were weaker and less frequent when compared to those for EN years. In this case the SJ was weaker than in EN years and the negative SLP anomalies over the tropical continent contributed to the inversion of the northeasterly trade winds. Also a southerly flow anomaly was generated by the geostrophic balance due to the anomalous blocking over southeast Pacific and the intense cyclonic transient over the southern tip of South America. As result the warm tropical air brought by the SALLJ encounters the cold extratropical air from the southerly winds over the La Plata basin. This configuration can increase the conditional instability over the La Plata basin and may explain the more intense positive rainfall anomalies in SALLJ cases during LN years than in EN years.


2014 ◽  
Vol 14 (23) ◽  
pp. 13337-13359 ◽  
Author(s):  
D. C. Zemp ◽  
C.-F. Schleussner ◽  
H. M. J. Barbosa ◽  
R. J. van der Ent ◽  
J. F. Donges ◽  
...  

Abstract. Continental moisture recycling is a crucial process of the South American climate system. In particular, evapotranspiration from the Amazon basin contributes substantially to precipitation regionally as well as over other remote regions such as the La Plata basin. Here we present an in-depth analysis of South American moisture recycling mechanisms. In particular, we quantify the importance of cascading moisture recycling (CMR), which describes moisture transport between two locations on the continent that involves re-evaporation cycles along the way. Using an Eulerian atmospheric moisture tracking model forced by a combination of several historical climate data sets, we were able to construct a complex network of moisture recycling for South America. Our results show that CMR contributes about 9–10% to the total precipitation over South America and 17–18% over the La Plata basin. CMR increases the fraction of total precipitation over the La Plata basin that originates from the Amazon basin from 18–23 to 24–29% during the wet season. We also show that the south-western part of the Amazon basin is not only a direct source of rainfall over the La Plata basin, but also a key intermediary region that distributes moisture originating from the entire Amazon basin towards the La Plata basin during the wet season. Our results suggest that land use change in this region might have a stronger impact on downwind rainfall than previously thought. Using complex network analysis techniques, we find the eastern side of the sub-tropical Andes to be a key region where CMR pathways are channeled. This study offers a better understanding of the interactions between the vegetation and the atmosphere on the water cycle, which is needed in a context of land use and climate change in South America.


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