Pakistani planners are increasingly prone to recognize the many links between water, food, and energy security. The construction of new large dams is seen by many as a concrete measure to achieve resource security for Pakistani for a future marked by climactic variability and unpredictability. This article explores the geopolitical and political geographic implications of Pakistan’s strategic vision of building dams as a way to prepare for climate change.

Hydropower development clearly has a significant role to play in the closer integration of different parts of the Himalayas and in facilitating downstream benefits throughout South Asia. However, the neo-liberal approach to infrastructure-led growth frequently overlooks the significant social, economic and political issues associated with this model of development in the region. Furthermore, the ongoing securitisation of water constrains the terms of debate under the guise of a unified national interest and enables large-scale dams to be constructed without due process.

With water concerns growing increasingly urgent, the global community will benefit from a treatment of the lessons learned and best practices in water dispute resolutions and approaches to water management. This report discusses the outcome of a working group of water experts from the Near East and South Asia (NESA) region,1 set up by the Strategic Studies Network, National Defense University, Washington DC.

Sir Creek, the 17th and last drainage branch of the river Indus, is a meandering riverine feature approximately 92 km (50 NM) long in the low-lying marshy region of Rann of Kutch. The Sir Creek boundary dispute between India and Pakistan is rooted in differing interpretations of the 1914 resolution passed by the Government of Bombay (GoB) or Bombay Residency.

Germany, located in Central Europe, has access to different national and international river basins and lakes, including the Rhine, Elbe, Danube and Lake Constance. Precipitation in Germany differs between comfortable amounts in the Alpine region (1500–2000 mm/a) to moderate amounts in the central and northern regions (600–800 mm/a). In brief, the geological conditions are in favour of successful groundwater storage.