87 research outputs found

    Multi-Site Daily Rainfall Prediction for Climate Change Scenarios Using the Non-Parametric K-Nearest Neighbours

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    Source: ICHE Conference Archive - https://mdi-de.baw.de/icheArchiv

    Selection of Spatial Extent of Predictor Variables in Statistical Downscaling

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    Source: ICHE Conference Archive - https://mdi-de.baw.de/icheArchiv

    Mahanadi streamflow: climate change impact assessment and adaptive strategies

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    Impacts of climate change on hydrology are assessed by downscaling large scale General Circulation Model (GCM) outputs of climate variables to local scale hydrologic variables. This modeling approach is characterized by uncertainties resulting from the use of different models, different scenarios, etc. Modeling uncertainty in climate change impact assessment includes assigning weights to GCMs and scenarios, based on their performances and providing weighted mean projection for the future. This projection is further used for water resources planning and adaptation to combat the adverse impacts of climate change. The present article summarizes the recent published work of the authors on uncertainty modeling and development of adaptation strategies to climate change for the Mahanadi river in India

    Is flood to drip irrigation a solution to groundwater depletion in the Indo-Gangetic plain?

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    Indian river basins are intensively managed with country-specific agricultural practices of cultivating submerged paddy and uncontrolled groundwater (GW) irrigation. Numerical experiments with the state-of-the-art land surface models, such as variable infiltration capacity (VIC), without incorporating region-specific practices, could be misleading. Here, we coupled VIC with 2D GW model AMBHAS, incorporating India-specific irrigation practices and crop practices, including submerged paddy fields. We performed numerical experiments to understand the causal factors of GW depletion in the northwest Indo-Gangetic plain (IGP). We identify widespread flood irrigation and cultivation of water-intensive paddy as critical drivers of the declining GW scenario. Our numerical experiments suggest that the introduction of drip irrigation reduces GW depletion in the northwest, but does not change the sign of GW level trends. The GW levels in the non-paddy fields of the middle IGP are less sensitive to irrigation practices due to the high return flow to GW for flood irrigation
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