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Mohamed Hamdi and Kalifa Goïta
The Saskatchewan River Basin (SRB) of central Canada plays a crucial role in the Canadian Prairies. Yet, climate change and human action constitute a real threat to its hydrological processes. This study aims to evaluate and analyze groundwater spatial a...
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Ritambhara K. Upadhyay, Gaurav Tripathi, Bojan Ðurin, Sanja ?amanovic, Vlado Cetl, Naval Kishore, Mukta Sharma, Suraj Kumar Singh, Shruti Kanga, Md Wasim, Praveen Kumar Rai and Vinay Bhardwaj
The immense dependence of the growing population on groundwater has resulted in depletion at a fast pace can be seen nowadays. Identifying a groundwater potential zone can be proved as an aid to provide insight to the decision-makers and local authoritie...
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Ibrahim Al Khoury, Laurie Boithias and David Labat
Karst water resources represent a primary source of freshwater supply, accounting for nearly 25% of the global population water needs. Karst aquifers have complex recharge characteristics, storage patterns, and flow dynamics. They also face a looming str...
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Li-Li Zhao, Lu-Sheng Li, Huan-Jie Cai, Xiao-Hu Shi and Chao Zhang
Organic amendments improve general soil conditions and stabilize crop production, but their effects on the soil hydrothermal regime, root distribution, and their contributions to water productivity (WP) of maize have not been fully studied. A two-year fi...
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Sujay S. Kaushal, Arthur J. Gold and Paul M. Mayer
Land use and climate change can accelerate the depletion of freshwater resources that support humans and ecosystem services on a global scale. Here, we briefly review studies from around the world, and highlight those in this special issue. We identify s...
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Rocio Gonzalez, Taha B. M. J. Ouarda, Prashanth R. Marpu, Mariam M. Allam, Elfatih A. B. Eltahir and Simon Pearson
Population growth and economic development have impacted the capacity of water resources to meet demands in a number of arid countries. This study focuses on the United Arab Emirates (UAE) where low rainfall, high rate of growth and agricultural developm...
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