Transboundary River Systems in the Context of Climate Change

2014 ◽  
pp. 310-349
2019 ◽  
Vol 69 ◽  
pp. 162-172 ◽  
Author(s):  
Shlomi Dinar ◽  
David Katz ◽  
Lucia De Stefano ◽  
Brian Blankespoor

2020 ◽  
Vol 15 (9) ◽  
pp. 094012
Author(s):  
Yifan Cheng ◽  
Nathalie Voisin ◽  
John R Yearsley ◽  
Bart Nijssen

2020 ◽  
Vol 34 (11) ◽  
pp. 3465-3478
Author(s):  
Vasileios Kitsikoudis ◽  
Bernhard P. J. Becker ◽  
Ymkje Huismans ◽  
Pierre Archambeau ◽  
Sébastien Erpicum ◽  
...  

2015 ◽  
Vol 17 (6) ◽  
pp. 1057-1069 ◽  
Author(s):  
P. G. Whitehead ◽  
E. Barbour ◽  
M. N. Futter ◽  
S. Sarkar ◽  
H. Rodda ◽  
...  

The potential impacts of climate change and socio-economic change on flow and water quality in rivers worldwide is a key area of interest.


Water ◽  
2021 ◽  
Vol 13 (20) ◽  
pp. 2800
Author(s):  
Karlygash Kaliyeva ◽  
Petras Punys ◽  
Yermekul Zhaparkulova

The impact of regional climate change on the runoff and the regime of glacier- and snow-fed rivers in the transboundary river Shu basin between Kazakhstan and Kyrgyzstan is investigated. This study covered three of the most representative rivers of the Shu basin. It was based on the weather and gauging stations’ observation data in the river Shu basin — the northern Tien Shan. Based on the trend analysis, an increase in the average annual temperature and river discharge was identified within the observation period as a whole, and for the separate compared periods. Furthermore, the mean annual flow projections were made based on the methodology of the retrospective analysis of runoff and the rate of river flow increase for the observation period, and further extrapolation of data for the forecast period. According to the analysis, the mean annual flow for the considered rivers will be decreased by 25 to 30% on average by 2050. These findings are necessary for elaborating adaptation measures in water allocation for freshwater supply, irrigation and hydropower within this transboundary river.


2020 ◽  
Vol 13 (4) ◽  
pp. 109-122
Author(s):  
Michael Klare

Ever since American security analysts began to consider the impact of global warming on international security, water has been viewed as an especially critical factor. In many parts of the developing world, water supplies are already insufficient to meet societal requirements, and, by shrinking these supplies further, climate change will cause widespread hardship, unrest, and conflict. But exactly what role water plays in this equation has been the subject of considerable reassessment over time. When analysts first examined warming’s impacts, they largely assumed that climate-related water scarcities would most likely provoke conflict within nations; only later did analysts look closely at the possibility of conflicts arising between states, typically in the context of shared river systems. This risk appears particularly acute in South Asia, where several highly-populated countries, including China, India, and Pakistan, rely on river systems which depend for part of their flow on meltwater from the Himalayan glaciers, which are contracting as a result of climate change. In the absence of greater efforts by these countries to address this peril in a collaborative, equitable manner, looming water shortages could combine with other antagonisms to trigger armed conflict, possibly entailing the use of nuclear weapons.


2021 ◽  
Vol 7 (6) ◽  
Author(s):  
Andrianirina Sedera Rajosoa ◽  
Chérifa Abdelbaki ◽  
Khaldoon A. Mourad

AbstractWater resources in the Middle East and North Africa (MENA region) face over-exploitation and over-pollution due to population growth, climate change and the lack of advanced water governance approaches. These challenges become more serious in transboundary river basins and may lead to conflict between riparian countries. The main objective of this paper is to assess water resources and needs at the Medjerda River Basin (MRB), shared by Tunisia and Algeria using the Water Evaluation and Planning (WEAP) system between 2020 and 2050. Four scenarios were built to assess the current and future status of the water supply and demands in both countries. The results show that water demands, and shortages are increasing, and some demand sites will face real water scarcity in the future due to climate change and development practices. Therefore, new allocation and management plans should be examined at the regional level based on real collaboration among all stakeholders.


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