California's current extreme drought must be a lesson for managing water in a warmer, more densely populated world, say Amir AghaKouchak and colleagues.

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The Decision Tree Framework described in this book provides resource-limited project planners and program managers with a cost-effective and effort-efficient, scientifically defensible, repeatable, and clear method for demonstrating the robustness of a project to climate change.

Order of the National Green Tribunal (Principal Bench, New Delhi) in the matter of Rahul Nagar Vs. Govt. of NCT of Delhi & Ors dated 24/08/2015 regarding illegal sand mining on the river bank of Yamuna and its surrounding areas without proper compliance, proper permissions and particular Environmental Clearance.

The law and policy frameworks for allocation or reallocation of water to different uses, or within a category of use, remain underdeveloped in India. This paper intends providing a starting point for a conversation on the law and policy dimensions of inter-sectoral water allocation. Focusing on a specific inter-sectoral water allocation conflict in Rajsamand District, Rajasthan, it illustrates gaps in the existing law and policy frameworks and highlights multiple issues that need to be addressed.

Projected future trends in water availability are associated with large uncertainties in many regions of the globe. In mountain areas with complex topography, climate models have often limited capabilities to adequately simulate the precipitation variability on small spatial scales. Also, their validation is hampered by typically very low station density. In the Central Andes of South America, a semi-arid high-mountain region with strong seasonality, zonal wind in the upper troposphere is a good proxy for interannual precipitation variability.

Order of the National Green Tribunal (Principal Bench, New Delhi) in the matter of Himalaya Environment & Employment Co-operative Society Ltd. Vs. State of Uttarakhand & Ors. dated 11/08/2015 regarding construction of roads in Uttarakhand which will cause destruction of greenery and trees as it is a soft soil and by construction of roads, hills are likely to slide.

Tropical mountain regions contain the main headwaters of important rivers in Central America. We selected 2 contrasting catchments located in a mountainous region to evaluate the precision of daily flow estimates based on the Hydrological Land Use Change (HYLUC) and Nedbør-Afstrømnings Model (NAM) hydrological models. A second objective was to simulate the impact of expected climate change for the year 2050 on stream flows and seasonal distribution of rainfall.

Climate change has the capacity to alter physical and biological ecosystem processes, jeopardizing the survival of associated species. This is a particular concern in cool, wet northern peatlands that could experience warmer, drier conditions. Here we show that climate, ecosystem processes and food chains combine to influence the population performance of species in British blanket bogs.

Order of the National Green Tribunal (Principal Bench, New Delhi) in the matter of Manoj Mishra Vs. Union of India & Ors. dated 28/07/2015 regarding Yamuna pollution.

Additional Chief Secretary, Irrigation and Additional Chief Secretary, Urban Local Bodies Haryana informed the Tribunal that ten cumecs water would be continued to be discharged at Hathnikund. However, they may have some difficulty in the lean season to maintain 10 cumecs flow in the River Yamuna from Hathnikund to Wazirabad.

The Thailand floods in 2011 caused unprecedented economic damage in the Chao Phraya River basin. To diagnose the flood hazard characteristics, this study analyses the hydrologic sensitivity of flood runoff and inundation to rainfall. The motivation is to address why the seemingly insignificant monsoon rainfall, or 1.2 times more rainfall than for past large floods, including the ones in 1995 and 2006, resulted in such devastating flooding. To quantify the hydrologic sensitivity, this study simulated long-term rainfall–runoff and inundation for the entire river basin (160 000 km2).

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