Analysis of a Nepalese water resources system: stress, adaptive capacity and vulnerability

2009 ◽  
Vol 9 (2) ◽  
pp. 213-222 ◽  
Author(s):  
V. P. Pandey ◽  
M. S. Babel ◽  
F. Kazama

It is widely accepted that water resources are vulnerable to socioeconomic development and environment change including climate change/variability. So, analyzing the type and extent of stresses (that render water a vulnerable resource) and the capacity of the system to adapt is necessary for integrated water resources management. This paper departs from the common notion that links vulnerability to water crisis, and analyzes a water resources system in the Bagmati River Basin (BRB) in Nepal from the perspective of both stress and adaptive capacity. The analysis is based on evaluation of eleven indicators, eight parameters, two sub-indices and an index. The situation analysis in basin and sub-watershed scale suggests considerable variation in parameter values and vulnerability index in different geographical (basin and sub-watershed) and spatial (three sub-watersheds) scales within the BRB, revealing the need for differential policy interventions based on scale. The northern sub-watershed in the BRB which has favourable climate for human settlement and cultivation, is more vulnerable than the southern sub-watershed. Relatively higher vulnerability in northern sub-watershed is due to high stress (related mainly to water scarcity) and low adaptive capacity (related mainly to low natural capacity). The comprehensive and easily interpretable finding is expected to help decision makers to reach sound solutions to reduce vulnerability of water resources system in the dynamic environment.

2011 ◽  
Vol 11 (2) ◽  
pp. 480-488 ◽  
Author(s):  
Vishnu Prasad Pandey ◽  
Mukand S. Babel ◽  
Sangam Shrestha ◽  
Futaba Kazama

2021 ◽  
Vol 13 (14) ◽  
pp. 7589
Author(s):  
Yang Yang ◽  
Shiwei Liu ◽  
Cunde Xiao ◽  
Cuiyang Feng ◽  
Chenyu Li

In Tarim River Basin (TRB), the retreat of glacier and snow cover reduction due to climate warming threatens the regional economy of downstream basins that critically depends on meltwater. However, the quantitative evaluation of its impact on multiple sectors of the socioeconomic system is incomplete. Based on compiled regional input–output table of the year 2012, this study developed a method to analyze the relationships between economic activities and related meltwater withdrawal, as well as sectoral transfer. The results show that the direct meltwater withdrawal intensity (DMWI) of agriculture was much higher than other sectors, reaching 2348.02 m3/10,000 CNY. Except for A01 (agriculture) and A02 (mining and washing of coal), the embodied meltwater withdrawal (EMW) driven by the final demand of other sectors was greater than direct meltwater withdrawal, and all sectors required inflows of virtual water (72.45 × 108 m3, accounting for 29% of total supply from cryospheric water resources) for their production processes in 2012. For sectors with high DMWI, improving water-use efficiency is an effective way to reduce water withdrawal. To some extent, the unbalanced supply of cryospheric water resources due to geographical segregation can be regulated by virtual water flows from water-saving to water-intensive sectors. Such decisions can affect the balance between socioeconomic development and environment conservation for long-term sustainability.


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