Flood of August 1935 in the Muskingum River Basin, Ohio, with Meteorologic and hydrologic conditions, and Meteorology of the storm

1941 ◽  
2016 ◽  
Vol 36 (11) ◽  
pp. 3807-3818 ◽  
Author(s):  
Jessica Ayers ◽  
Darren L. Ficklin ◽  
Iris T. Stewart ◽  
Meredith Strunk

2020 ◽  
Author(s):  
Meseret Teweldebrihan ◽  
Saket Pande ◽  
Michael McClain

<p>Extensive migration, settlement, and relocation of people for water resources development practice along a river basin often changes its hydrologic conditions and leads to conflicts for available water resources. In view of this, this study compiled the dynamics of population migration, settlement, and water resource developments in the Dhidhessa River Basin (DRB). The trend in migration time series for 1984-2017 based on census data indicates that the migrated rural population were ‘pulled’ by the government initiative. On the other hand, survey revealed that the farmer have dire reasons to migrate from their origin due to the scarcity of land and water. However, given the distance to a dam location, such potential migrants are financially incapable of relocating on their own. The study, therefore, calls for an analysis that takes into account the wellbeing of the displaced agrarian society at large of the migrant population in particular in the dam-affected area.</p>


Author(s):  
Timothy W. Hawkins ◽  
Christopher J. Woltemade

Abstract A gridded hydrologic model was developed to assess the impact of projected climate change on future Delaware River Basin (DRB) hydrology. The DRB serves as a water supply resource to over 15 million people. Model evaluation statistics for both water year and monthly runoff projections indicate that the model is able to capture well the hydrologic conditions of the DRB. Basinwide, annual temperature is projected to increase from 2.0 to 5.5 °C by 2080–2099. Correspondingly, potential and actual evapotranspiration, precipitation, rainfall, and runoff are all projected to increase, while snowfall, snow water storage, snowmelt, and subsurface moisture are all projected to decrease. By 2080–2099, basinwide summer subsurface moisture is projected to decrease 7–18% due to increased evapotranspiration, while winter runoff is projected to increase 15–43% due to increased precipitation and snowmelt and a conversion of snowfall to rainfall. Significant spatial variability in future changes to hydrologic parameters exists across the DRB. Changes in the timing and amount of future runoff and other hydrologic conditions need to be considered for future water resource management.


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