Fluctuation of Groundwater Levels and Recharge Patterns in Northern Ghana
Evaluating groundwater levels and recharge patterns is part of sustainably managing the water supply and predicting the possibility of water shortages, especially in light of climate change, extreme events (floods/droughts), increasing population and development. In the northern region of Ghana, gro...
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doaj-c977747f8b9b4ef1babde66f007e9b542020-11-24T22:39:33ZengMDPI AGClimate2225-11542014-12-013111510.3390/cli3010001cli3010001Fluctuation of Groundwater Levels and Recharge Patterns in Northern GhanaAlexandra Lutz0Solomon Minyila1Bansaga Saga2Samuel Diarra3Braimah Apambire4James Thomas5Division of Hydrologic Sciences, Desert Research Institute, 2215 Raggio Parkway, Reno, NV 89512, USAGhana Integrated Water, Sanitation, and Hygiene Project, World Vision Ghana, Savelugu, GhanaGhana Integrated Water, Sanitation, and Hygiene Project, World Vision Ghana, Savelugu, GhanaWater, Sanitation, and Hygiene Learning Center, West Africa Region, World Vision International, PO Box 12713, Niamey, NigerDivision of Hydrologic Sciences, Desert Research Institute, 2215 Raggio Parkway, Reno, NV 89512, USADivision of Hydrologic Sciences, Desert Research Institute, 2215 Raggio Parkway, Reno, NV 89512, USAEvaluating groundwater levels and recharge patterns is part of sustainably managing the water supply and predicting the possibility of water shortages, especially in light of climate change, extreme events (floods/droughts), increasing population and development. In the northern region of Ghana, groundwater is increasingly relied upon as a source of potable water for rural populations, but seasonal and inter-annual fluctuations of groundwater levels and recharge patterns are not always known. The fluctuation of groundwater levels on a seasonal basis shows that groundwater levels at all sites increase in response to seasonal precipitation. On an annual basis, all sites show an overall net decline of groundwater levels over the study period, which may be associated with below-average departures of precipitation during five of the seven study years. The variability of recharge patterns among five sites is attributed to the spatio-temporal variability of precipitation and hydrogeologic site uniqueness. The overarching potential benefit of this study is to facilitate closing knowledge gaps and contribute to a foundation for a more robust evaluation of groundwater resources in the area, especially as more data become available.http://www.mdpi.com/2225-1154/3/1/1precipitationwater resourcesclimate |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Alexandra Lutz Solomon Minyila Bansaga Saga Samuel Diarra Braimah Apambire James Thomas |
spellingShingle |
Alexandra Lutz Solomon Minyila Bansaga Saga Samuel Diarra Braimah Apambire James Thomas Fluctuation of Groundwater Levels and Recharge Patterns in Northern Ghana Climate precipitation water resources climate |
author_facet |
Alexandra Lutz Solomon Minyila Bansaga Saga Samuel Diarra Braimah Apambire James Thomas |
author_sort |
Alexandra Lutz |
title |
Fluctuation of Groundwater Levels and Recharge Patterns in Northern Ghana |
title_short |
Fluctuation of Groundwater Levels and Recharge Patterns in Northern Ghana |
title_full |
Fluctuation of Groundwater Levels and Recharge Patterns in Northern Ghana |
title_fullStr |
Fluctuation of Groundwater Levels and Recharge Patterns in Northern Ghana |
title_full_unstemmed |
Fluctuation of Groundwater Levels and Recharge Patterns in Northern Ghana |
title_sort |
fluctuation of groundwater levels and recharge patterns in northern ghana |
publisher |
MDPI AG |
series |
Climate |
issn |
2225-1154 |
publishDate |
2014-12-01 |
description |
Evaluating groundwater levels and recharge patterns is part of sustainably managing the water supply and predicting the possibility of water shortages, especially in light of climate change, extreme events (floods/droughts), increasing population and development. In the northern region of Ghana, groundwater is increasingly relied upon as a source of potable water for rural populations, but seasonal and inter-annual fluctuations of groundwater levels and recharge patterns are not always known. The fluctuation of groundwater levels on a seasonal basis shows that groundwater levels at all sites increase in response to seasonal precipitation. On an annual basis, all sites show an overall net decline of groundwater levels over the study period, which may be associated with below-average departures of precipitation during five of the seven study years. The variability of recharge patterns among five sites is attributed to the spatio-temporal variability of precipitation and hydrogeologic site uniqueness. The overarching potential benefit of this study is to facilitate closing knowledge gaps and contribute to a foundation for a more robust evaluation of groundwater resources in the area, especially as more data become available. |
topic |
precipitation water resources climate |
url |
http://www.mdpi.com/2225-1154/3/1/1 |
work_keys_str_mv |
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