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Bangladesh
Understanding the Deformation Structures and Tectonics of the Active Orogenic Fold-Thrust Belt: Insights from the Outer Indo-Burman Ranges
Influence of hydrostratigraphy on the distribution of groundwater arsenic in the transboundary Ganges River delta aquifer system, India and Bangladesh
Miocene seismic stratigraphy and geomorphology of Bibiyana gas field, Surma Basin, Bangladesh
Linking rivers to the rock record: Channel patterns and paleocurrent circular variance
Sedimentology of the modern seasonal lower Ganges River with low inter-annual peak discharge variance, Bangladesh
Late Paleozoic detrital history of eastern Gondwanaland: petrofacies and detrital geochronology of Permo-Carboniferous intracratonic sequences of the northwest Bengal Basin
Indo-Burma passive amalgamation along the Kaladan Fault: Insights from zircon provenance in the Chittagong-Tripura Fold Belt (Bangladesh)
Mixing and Reactive Fronts in the Subsurface
Crustal architecture and Moho topography beneath the eastern Indian and Bangladesh margins – new insights on rift evolution and the continent–ocean boundary
Criticality in the planform behavior of the Ganges River meanders
Hydrophilanthropy gone wrong—How well-meaning scientists, engineers, and the general public can make the worldwide water and sanitation situation worse
Efforts to improve water quality and quantity, and sanitation in the world are impeded by a variety of technical and socioeconomic issues often unfamiliar to well-motivated individuals. Sustainable technological improvement can be thwarted by the lack of consideration of regional norms, customs, mores, and traditions, and by the absence of feasibility assessment and coordination with the community both before and during instatement of local improvements. Specifically, the absence of coordination means not fully allowing users to define their needs, resources, issues, and maintainable solutions, and not understanding local and regional power dynamics and the ability of the community to provide long-term project stewardship. Other mistakes can include: a lack of long-term planning; inadequate scientific and engineering design and construction; lack of anticipation of contingencies and complicating issues and lack of adaptive management to deal with these unforeseen events; use of inappropriate technology; absence of educational efforts (both for the community to understand and provide stewardship for the project, and for the education of those installing the facilities in the community); lack of follow-up; and lack of technical expertise and leadership. There is no single approach to water and sanitation development that fits all situations. However, avoiding common pitfalls can bring these important resources to villages worldwide, and in the process empower communities, reduce sickness and mortality, and improve the human condition.
The valuable role that science has to play in disaster preparedness and risk reduction is widely recognized and was highlighted during the development of the successor to the Hyogo Framework for Action for disaster risk reduction that was adopted in March 2015. However, there are many factors that limit how effectively science can inform both disaster risk reduction policy and practice. Understanding these factors and taking steps to overcome them require a broad view, and a comparative approach can be instructive. We focus on two projects that were independently completed by the authors: earthquake risk management in Bangladesh and flooding and wildfires management in the United States. We use each case to reflect on the implications of recent recommendations made by the Science and Technology Advisory Group (STAG) of the United Nations Office for Disaster Risk Reduction that attempt to increase the integration of science in disaster risk reduction policy making. We then use the STAG recommendations as a framework for integrating our independent case study findings. Despite the differences in the geographic contexts and hazards being considered, these examples broadly support the STAG recommendations. However, the fine details of the way in which science is used in decision making need to be given careful consideration if science is to fully support disaster risk reduction. Although our collective observations suggest that science is an important part of the disaster risk reduction (DRR) process, suggesting that it is “key to post-2015 DRR efforts” as the STAG recommendations do, may perhaps overstate the role that science is able to play.