GroMoPo Metadata for Rib catchment model
Authors: | |
---|---|
Owners: | gromopo_admin |
Type: | Resource |
Storage: | The size of this resource is 1.7 KB |
Created: | Feb 08, 2023 at 1:37 p.m. |
Last updated: | Feb 08, 2023 at 1:38 p.m. |
Citation: | See how to cite this resource |
Sharing Status: | Public |
---|---|
Views: | 981 |
Downloads: | 218 |
+1 Votes: | Be the first one to this. |
Comments: | No comments (yet) |
Abstract
Study region: Rib catchment in the Lake Tana sub-basin, Upper Blue Nile River, Ethiopia. Study focus: This paper aimed to assess the impacts of future increase in abstraction and recharge reduction on the groundwater, groundwater availability, and groundwater-surface waters interaction based on a three-dimensional groundwater flow modeling. Calibration was made under the steady state condition. Scenario analysis performed for 1) increase in abstraction, 2) decrease in recharge, 3) the worst-case scenario that combined the aforementioned two scenarios and with additional extraction for irrigation, and 4) for the optimal-case scenario, which considers 5% recharge increase for the worst-case scenario model. New hydrological insights for the region: It is found that the groundwater flows from uplands toward the Tana Lake. The total inflow to and outflow from the system in the calibrated model are 1733480 m(3)/d and 1840451 m(3)/d, respectively. Groundwater level drop, reduction in base flows to surface waters, and in evapotranspiration flux compared to the calibrated values encountered for all scenarios, which are significant (mean 38.4 m, 28.5-100 %, and 97.8 %, respectively) for the worst-case scenario. On the other hand, an increase in groundwater level (mean 9.8 m), base flows (0-14.4 %), and evapotranspiration flux (29.5 %) observed for the optimal scenario when compared to the worst-case scenario results. Results suggest that groundwater management measures should be implemented to mitigate the impacts.
Subject Keywords
Coverage
Spatial

Content
Additional Metadata
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
Comments
There are currently no comments
New Comment