Data scarce modelling the impact of present and future groundwater development on Jordan multiaquifer groundwater resources
Rapidly growing demands and climate change stresses water resources worldwide and leads to highly competitive situations between the environment and socio-economic development of a region, calling for a smart and modelling driven water resources management. However, data scarcity often prevents the...
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| Published in | The Science of the total environment Vol. 870; p. 161729 |
|---|---|
| Main Authors | , , , |
| Format | Journal Article |
| Language | English |
| Published |
Netherlands
Elsevier B.V
20.04.2023
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| Subjects | |
| Online Access | Get full text |
| ISSN | 0048-9697 1879-1026 1879-1026 |
| DOI | 10.1016/j.scitotenv.2023.161729 |
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| Abstract | Rapidly growing demands and climate change stresses water resources worldwide and leads to highly competitive situations between the environment and socio-economic development of a region, calling for a smart and modelling driven water resources management. However, data scarcity often prevents the realisation of a comprehensive, nation-wide resources model, which provides reliable and spatially discretized results of water resources development.
We present a workflow approach to set up a large-scale multi-aquifer model, overcoming data shortage by stepwise calibration and integrating hydrological and numerical groundwater flow modelling into a coupled system. The study aims to develop such a system to assess how groundwater resources react on anthropogenic impacts on the example of the Kingdom of Jordan, one of the water poorest countries on globe.
Simulated heads reliably resembled the monitored ones in >70 % of the observation wells. That makes us confident, the model represents all the states well from 1970, prior to the intense development of the country until 2015. The water balance shows an annual deficit of 1.16 million cubic meter (MCM) due to an overdraft. The discharge to the Dead Sea increased from 564 MCM/yr to 696 MCM/yr over the time period. Regional drawdowns of >250 m and groundwater depression with an extension of approx.100 km are observable in both large aquifer complexes. Most severe areas in the upper calcareous aquifer are located in the north of Amman and practically in all urban and agricultural agglomerations across the country. Groundwater tables in the deeper sandstone aquifer are particularly affected in the south as well as in the wider vicinity of the Dead Sea as consequence of its continuous dropping. Simulations of the future development of the groundwater tables indicate a severe deterioration of the situation with further declines in groundwater levels of up to 70 m.
[Display omitted]
•Overcoming data shortage for groundwater modelling by a nested calibration process.•75 % of Jordan's groundwater basins are subject to intense groundwater depletion.•Regional drawdowns exceed 250 m.•Jordanian aquifers release 519–676 × 106 m3/a of groundwater to the Dead Sea.•Dead Sea dropping affects water tables up to 100 km east in the interior of Jordan. |
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| AbstractList | Rapidly growing demands and climate change stresses water resources worldwide and leads to highly competitive situations between the environment and socio-economic development of a region, calling for a smart and modelling driven water resources management. However, data scarcity often prevents the realisation of a comprehensive, nation-wide resources model, which provides reliable and spatially discretized results of water resources development. We present a workflow approach to set up a large-scale multi-aquifer model, overcoming data shortage by stepwise calibration and integrating hydrological and numerical groundwater flow modelling into a coupled system. The study aims to develop such a system to assess how groundwater resources react on anthropogenic impacts on the example of the Kingdom of Jordan, one of the water poorest countries on globe. Simulated heads reliably resembled the monitored ones in >70 % of the observation wells. That makes us confident, the model represents all the states well from 1970, prior to the intense development of the country until 2015. The water balance shows an annual deficit of 1.16 million cubic meter (MCM) due to an overdraft. The discharge to the Dead Sea increased from 564 MCM/yr to 696 MCM/yr over the time period. Regional drawdowns of >250 m and groundwater depression with an extension of approx.100 km are observable in both large aquifer complexes. Most severe areas in the upper calcareous aquifer are located in the north of Amman and practically in all urban and agricultural agglomerations across the country. Groundwater tables in the deeper sandstone aquifer are particularly affected in the south as well as in the wider vicinity of the Dead Sea as consequence of its continuous dropping. Simulations of the future development of the groundwater tables indicate a severe deterioration of the situation with further declines in groundwater levels of up to 70 m.Rapidly growing demands and climate change stresses water resources worldwide and leads to highly competitive situations between the environment and socio-economic development of a region, calling for a smart and modelling driven water resources management. However, data scarcity often prevents the realisation of a comprehensive, nation-wide resources model, which provides reliable and spatially discretized results of water resources development. We present a workflow approach to set up a large-scale multi-aquifer model, overcoming data shortage by stepwise calibration and integrating hydrological and numerical groundwater flow modelling into a coupled system. The study aims to develop such a system to assess how groundwater resources react on anthropogenic impacts on the example of the Kingdom of Jordan, one of the water poorest countries on globe. Simulated heads reliably resembled the monitored ones in >70 % of the observation wells. That makes us confident, the model represents all the states well from 1970, prior to the intense development of the country until 2015. The water balance shows an annual deficit of 1.16 million cubic meter (MCM) due to an overdraft. The discharge to the Dead Sea increased from 564 MCM/yr to 696 MCM/yr over the time period. Regional drawdowns of >250 m and groundwater depression with an extension of approx.100 km are observable in both large aquifer complexes. Most severe areas in the upper calcareous aquifer are located in the north of Amman and practically in all urban and agricultural agglomerations across the country. Groundwater tables in the deeper sandstone aquifer are particularly affected in the south as well as in the wider vicinity of the Dead Sea as consequence of its continuous dropping. Simulations of the future development of the groundwater tables indicate a severe deterioration of the situation with further declines in groundwater levels of up to 70 m. Rapidly growing demands and climate change stresses water resources worldwide and leads to highly competitive situations between the environment and socio-economic development of a region, calling for a smart and modelling driven water resources management. However, data scarcity often prevents the realisation of a comprehensive, nation-wide resources model, which provides reliable and spatially discretized results of water resources development. We present a workflow approach to set up a large-scale multi-aquifer model, overcoming data shortage by stepwise calibration and integrating hydrological and numerical groundwater flow modelling into a coupled system. The study aims to develop such a system to assess how groundwater resources react on anthropogenic impacts on the example of the Kingdom of Jordan, one of the water poorest countries on globe. Simulated heads reliably resembled the monitored ones in >70 % of the observation wells. That makes us confident, the model represents all the states well from 1970, prior to the intense development of the country until 2015. The water balance shows an annual deficit of 1.16 million cubic meter (MCM) due to an overdraft. The discharge to the Dead Sea increased from 564 MCM/yr to 696 MCM/yr over the time period. Regional drawdowns of >250 m and groundwater depression with an extension of approx.100 km are observable in both large aquifer complexes. Most severe areas in the upper calcareous aquifer are located in the north of Amman and practically in all urban and agricultural agglomerations across the country. Groundwater tables in the deeper sandstone aquifer are particularly affected in the south as well as in the wider vicinity of the Dead Sea as consequence of its continuous dropping. Simulations of the future development of the groundwater tables indicate a severe deterioration of the situation with further declines in groundwater levels of up to 70 m. Rapidly growing demands and climate change stresses water resources worldwide and leads to highly competitive situations between the environment and socio-economic development of a region, calling for a smart and modelling driven water resources management. However, data scarcity often prevents the realisation of a comprehensive, nation-wide resources model, which provides reliable and spatially discretized results of water resources development. We present a workflow approach to set up a large-scale multi-aquifer model, overcoming data shortage by stepwise calibration and integrating hydrological and numerical groundwater flow modelling into a coupled system. The study aims to develop such a system to assess how groundwater resources react on anthropogenic impacts on the example of the Kingdom of Jordan, one of the water poorest countries on globe. Simulated heads reliably resembled the monitored ones in >70 % of the observation wells. That makes us confident, the model represents all the states well from 1970, prior to the intense development of the country until 2015. The water balance shows an annual deficit of 1.16 million cubic meter (MCM) due to an overdraft. The discharge to the Dead Sea increased from 564 MCM/yr to 696 MCM/yr over the time period. Regional drawdowns of >250 m and groundwater depression with an extension of approx.100 km are observable in both large aquifer complexes. Most severe areas in the upper calcareous aquifer are located in the north of Amman and practically in all urban and agricultural agglomerations across the country. Groundwater tables in the deeper sandstone aquifer are particularly affected in the south as well as in the wider vicinity of the Dead Sea as consequence of its continuous dropping. Simulations of the future development of the groundwater tables indicate a severe deterioration of the situation with further declines in groundwater levels of up to 70 m. [Display omitted] •Overcoming data shortage for groundwater modelling by a nested calibration process.•75 % of Jordan's groundwater basins are subject to intense groundwater depletion.•Regional drawdowns exceed 250 m.•Jordanian aquifers release 519–676 × 106 m3/a of groundwater to the Dead Sea.•Dead Sea dropping affects water tables up to 100 km east in the interior of Jordan. |
| ArticleNumber | 161729 |
| Author | Geyer, S. Rödiger, T. Odeh, T. Siebert, C. |
| Author_xml | – sequence: 1 givenname: T. surname: Rödiger fullname: Rödiger, T. email: tino.roediger@ufz.de organization: Helmholtz-Centre for Environmental Research UFZ, Dept. Catchment Hydrology, Theodor-Lieser-Str. 4, 06120 Halle, Germany – sequence: 2 givenname: S. surname: Geyer fullname: Geyer, S. organization: Helmholtz-Centre for Environmental Research UFZ, Dept. Catchment Hydrology, Theodor-Lieser-Str. 4, 06120 Halle, Germany – sequence: 3 givenname: T. surname: Odeh fullname: Odeh, T. organization: The Hashemite University, Prince Al Hassan bin Talal College for Natural Resources and Environment, Dept. of Water Management and Environment, Zarqa, Jordan – sequence: 4 givenname: C. surname: Siebert fullname: Siebert, C. organization: Helmholtz-Centre for Environmental Research UFZ, Dept. Catchment Hydrology, Theodor-Lieser-Str. 4, 06120 Halle, Germany |
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| Cites_doi | 10.1016/S0143-6228(99)00012-0 10.1016/j.scitotenv.2015.12.003 10.1007/BF02702043 10.4319/lo.1985.30.3.0451 10.1007/s10040-017-1601-5 10.1007/s12665-010-0898-3 10.1007/s12665-013-2371-6 10.1002/2014WR015595 10.1080/02508060801927663 10.1007/s002549900105 10.1016/j.scitotenv.2014.04.010 10.1007/s10040-017-1535-y 10.3390/w12020325 10.1145/321607.321609 10.1016/S0022-1694(00)00293-6 10.1175/JCLI-D-11-00296.1 10.1144/GSL.QJEG.1982.015.02.01 10.1007/s00254-008-1322-0 10.1007/s10040-022-02523-3 10.5194/se-10-1451-2019 10.1007/s12665-012-2135-8 10.1002/2016WR020261 10.3390/resources4040819 10.1080/10106049.2020.1797185 |
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| Keywords | Overdraft Data scarcity Large scale groundwater modelling Groundwater recharge/water budget Pilot point calibration |
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| Title | Data scarce modelling the impact of present and future groundwater development on Jordan multiaquifer groundwater resources |
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