Related Experiment Video
Updated: Nov 20, 2025

Watershed Planning within a Quantitative Scenario Analysis Framework
Published on: July 24, 2016
Effect of climate and socioeconomic changes on future surface water availability from mountainous water sources in
Muhammad Shafqat Mehboob1, Yeonjoo Kim1
1Department of Civil and Environmental Engineering, Yonsei University, Seoul 03722, South Korea.
Abstract:
Pakistan is highly dependent on water resources from the mountainous regions of the Upper Indus Basin (UIB), especially for irrigation. An evaluation framework was developed and applied in this study to understand the variability in surface water availability to agricultural and domestic sectors across various future climate and socioeconomic pathways in five catchments within the UIB (Astore, Gilgit, Hunza, Shigar, and Shyoke). A planning tool named Water Evaluation and Planning (WEAP) was used to understand the dynamics of past and future water demands for multiple future scenarios. We combined three different climate scenarios (representative concentration pathways) with socioeconomic scenarios (shared socioeconomic pathways) of economic development and population and local agricultural land development pathways. The results indicate that the external driving forces of climate change and socioeconomic growth will cause a discrepancy between the supply and demand of water resources in regions with higher socioeconomic growth, particularly those with agricultural development as the dominant external factor. Among the five catchments within the UIB, Astore and Gilgit face a water shortfall in all future scenarios, whereas Shyoke will encounter water deficiencies only in the case of agricultural land development. We also demonstrated that the impact of climate change is markedly different in Astore and Gilgit. Over Astore, the impact of precipitation will control the unmet water demands by increasing winter streamflow whereas over Gilgit non-climatic factors, such as population and agricultural growth, will control future unmet water demands.
More Related Videos
08:09Wastewater Irrigation Impacts on Soil Hydraulic Conductivity: Coupled Field Sampling and Laboratory Determination of Saturated Hydraulic Conductivity
Published on: August 19, 2018
13:27Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
Published on: June 8, 2015
Related Concept Videos
What is Climate?
Responses to Drought and Flooding
Global Climate Change
Design Example: Analyzing Capacity Contours for Flood Risk Assessment
The Water Cycle
Adaptations that Reduce Water Loss