Rapid groundwater decline and some cases of recovery in aquifers globally

Groundwater resources are vital to ecosystems and livelihoods. Excessive groundwater withdrawals can cause groundwater levels to decline 1 – 10 , resulting in seawater intrusion 11 , land subsidence 12 , 13 , streamflow depletion 14 – 16 and wells running dry 17 . However, the global pace and preval...

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Veröffentlicht in:	Nature (London) Jg. 625; H. 7996; S. 715 - 721
Hauptverfasser:	Jasechko, Scott, Seybold, Hansjörg, Perrone, Debra, Fan, Ying, Shamsudduha, Mohammad, Taylor, Richard G., Fallatah, Othman, Kirchner, James W.
Format:	Journal Article
Sprache:	Englisch
Veröffentlicht:	London Nature Publishing Group UK 25.01.2024 Nature Publishing Group
Schlagworte:	20th century 21st century 704/172 704/242 Acceleration Agricultural land Aquifer management Aquifer recharge Aquifer systems Aquifers Chemical analysis Ecosystem Groundwater Groundwater - analysis Groundwater depletion Groundwater levels Groundwater recharge Groundwater resources Humanities and Social Sciences multidisciplinary Precipitation Satellites Science Science (multidisciplinary) Seawater Stream discharge Stream flow Surface water Time series Trends Water analysis Water levels Water resources Water Supply - statistics & numerical data
ISSN:	0028-0836, 1476-4687, 1476-4687
Online-Zugang:	Volltext
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Abstract	Groundwater resources are vital to ecosystems and livelihoods. Excessive groundwater withdrawals can cause groundwater levels to decline 1 – 10 , resulting in seawater intrusion 11 , land subsidence 12 , 13 , streamflow depletion 14 – 16 and wells running dry 17 . However, the global pace and prevalence of local groundwater declines are poorly constrained, because in situ groundwater levels have not been synthesized at the global scale. Here we analyse in situ groundwater-level trends for 170,000 monitoring wells and 1,693 aquifer systems in countries that encompass approximately 75% of global groundwater withdrawals 18 . We show that rapid groundwater-level declines (>0.5 m year −1 ) are widespread in the twenty-first century, especially in dry regions with extensive croplands. Critically, we also show that groundwater-level declines have accelerated over the past four decades in 30% of the world’s regional aquifers. This widespread acceleration in groundwater-level deepening highlights an urgent need for more effective measures to address groundwater depletion. Our analysis also reveals specific cases in which depletion trends have reversed following policy changes, managed aquifer recharge and surface-water diversions, demonstrating the potential for depleted aquifer systems to recover. Analysis of about 170,000 monitoring wells and 1,693 aquifer systems worldwide shows that extensive and often accelerating groundwater declines are widespread in the twenty-first century, but that groundwater levels are recovering in some cases.
AbstractList	Groundwater resources are vital to ecosystems and livelihoods. Excessive groundwater withdrawals can cause groundwater levels to decline1–10, resulting in seawater intrusion11, land subsidence12,13, streamflow depletion14–16 and wells running dry17. However, the global pace and prevalence of local groundwater declines are poorly constrained, because in situ groundwater levels have not been synthesized at the global scale. Here we analyse in situ groundwater-level trends for 170,000 monitoring wells and 1,693 aquifer systems in countries that encompass approximately 75% of global groundwater withdrawals18. We show that rapid groundwater-level declines (>0.5 m year−1) are widespread in the twenty-first century, especially in dry regions with extensive croplands. Critically, we also show that groundwater-level declines have accelerated over the past four decades in 30% of the world’s regional aquifers. This widespread acceleration in groundwater-level deepening highlights an urgent need for more effective measures to address groundwater depletion. Our analysis also reveals specific cases in which depletion trends have reversed following policy changes, managed aquifer recharge and surface-water diversions, demonstrating the potential for depleted aquifer systems to recover. Analysis of about 170,000 monitoring wells and 1,693 aquifer systems worldwide shows that extensive and often accelerating groundwater declines are widespread in the twenty-first century, but that groundwater levels are recovering in some cases. Groundwater resources are vital to ecosystems and livelihoods. Excessive groundwater withdrawals can cause groundwater levels to decline1-10, resulting in seawater intrusion11, land subsidence12,13, streamflow depletion14-16 and wells running dry17. However, the global pace and prevalence of local groundwater declines are poorly constrained, because in situ groundwater levels have not been synthesized at the global scale. Here we analyse in situ groundwater-level trends for 170,000 monitoring wells and 1,693 aquifer systems in countries that encompass approximately 75% of global groundwater withdrawals18. We show that rapid groundwater-level declines (>0.5 m year-1) are widespread in the twenty-first century, especially in dry regions with extensive croplands. Critically, we also show that groundwater-level declines have accelerated over the past four decades in 30% of the world's regional aquifers. This widespread acceleration in groundwater-level deepening highlights an urgent need for more effective measures to address groundwater depletion. Our analysis also reveals specific cases in which depletion trends have reversed following policy changes, managed aquifer recharge and surface-water diversions, demonstrating the potential for depleted aquifer systems to recover.Groundwater resources are vital to ecosystems and livelihoods. Excessive groundwater withdrawals can cause groundwater levels to decline1-10, resulting in seawater intrusion11, land subsidence12,13, streamflow depletion14-16 and wells running dry17. However, the global pace and prevalence of local groundwater declines are poorly constrained, because in situ groundwater levels have not been synthesized at the global scale. Here we analyse in situ groundwater-level trends for 170,000 monitoring wells and 1,693 aquifer systems in countries that encompass approximately 75% of global groundwater withdrawals18. We show that rapid groundwater-level declines (>0.5 m year-1) are widespread in the twenty-first century, especially in dry regions with extensive croplands. Critically, we also show that groundwater-level declines have accelerated over the past four decades in 30% of the world's regional aquifers. This widespread acceleration in groundwater-level deepening highlights an urgent need for more effective measures to address groundwater depletion. Our analysis also reveals specific cases in which depletion trends have reversed following policy changes, managed aquifer recharge and surface-water diversions, demonstrating the potential for depleted aquifer systems to recover. Groundwater resources are vital to ecosystems and livelihoods. Excessive groundwater withdrawals can cause groundwater levels to decline , resulting in seawater intrusion , land subsidence , streamflow depletion and wells running dry . However, the global pace and prevalence of local groundwater declines are poorly constrained, because in situ groundwater levels have not been synthesized at the global scale. Here we analyse in situ groundwater-level trends for 170,000 monitoring wells and 1,693 aquifer systems in countries that encompass approximately 75% of global groundwater withdrawals . We show that rapid groundwater-level declines (>0.5 m year ) are widespread in the twenty-first century, especially in dry regions with extensive croplands. Critically, we also show that groundwater-level declines have accelerated over the past four decades in 30% of the world's regional aquifers. This widespread acceleration in groundwater-level deepening highlights an urgent need for more effective measures to address groundwater depletion. Our analysis also reveals specific cases in which depletion trends have reversed following policy changes, managed aquifer recharge and surface-water diversions, demonstrating the potential for depleted aquifer systems to recover. Groundwater resources are vital to ecosystems and livelihoods. Excessive groundwater withdrawals can cause groundwater levels to decline 1 – 10 , resulting in seawater intrusion 11 , land subsidence 12 , 13 , streamflow depletion 14 – 16 and wells running dry 17 . However, the global pace and prevalence of local groundwater declines are poorly constrained, because in situ groundwater levels have not been synthesized at the global scale. Here we analyse in situ groundwater-level trends for 170,000 monitoring wells and 1,693 aquifer systems in countries that encompass approximately 75% of global groundwater withdrawals 18 . We show that rapid groundwater-level declines (>0.5 m year −1 ) are widespread in the twenty-first century, especially in dry regions with extensive croplands. Critically, we also show that groundwater-level declines have accelerated over the past four decades in 30% of the world’s regional aquifers. This widespread acceleration in groundwater-level deepening highlights an urgent need for more effective measures to address groundwater depletion. Our analysis also reveals specific cases in which depletion trends have reversed following policy changes, managed aquifer recharge and surface-water diversions, demonstrating the potential for depleted aquifer systems to recover. Analysis of about 170,000 monitoring wells and 1,693 aquifer systems worldwide shows that extensive and often accelerating groundwater declines are widespread in the twenty-first century, but that groundwater levels are recovering in some cases. Groundwater resources are vital to ecosystems and livelihoods. Excessive ground water withdrawals can cause ground water levels to decline1-10, resulting in seawater intrusion11, land subsidence12,13, streamflow depletion14-16 and wells running dry17. However, the global pace and prevalence of local groundwater declines are poorly constrained, because in situ ground water levels have not been synthesized at the global scale. Here we analyse in situ groundwater-level trends for 170,000 monitoring wells and 1,693 aquifer systems in countries that encompass approximately 75% of global groundwater withdrawals18. We show that rapid groundwater-level declines (>0.5 m year-1) are widespread in the twenty-first century, especially in dry regions with extensive croplands. Critically, we also show that groundwater-level declines have accelerated over the past four decades in 30% of the world's regional aquifers. This widespread acceleration in groundwater-level deepening highlights an urgent need for more effective measures to address groundwater depletion. Our analysis also reveals specific cases in which depletion trends have reversed following policy changes, managed aquifer recharge and surface-water diversions, demonstrating the potential for depleted aquifer systems to recover. Groundwater resources are vital to ecosystems and livelihoods. Excessive groundwater withdrawals can cause groundwater levels to decline 1–10 , resulting in seawater intrusion 11 , land subsidence 12,13 , streamflow depletion 14–16 and wells running dry 17 . However, the global pace and prevalence of local groundwater declines are poorly constrained, because in situ groundwater levels have not been synthesized at the global scale. Here we analyse in situ groundwater-level trends for 170,000 monitoring wells and 1,693 aquifer systems in countries that encompass approximately 75% of global groundwater withdrawals 18 . We show that rapid groundwater-level declines (>0.5 m year −1 ) are widespread in the twenty-first century, especially in dry regions with extensive croplands. Critically, we also show that groundwater-level declines have accelerated over the past four decades in 30% of the world’s regional aquifers. This widespread acceleration in groundwater-level deepening highlights an urgent need for more effective measures to address groundwater depletion. Our analysis also reveals specific cases in which depletion trends have reversed following policy changes, managed aquifer recharge and surface-water diversions, demonstrating the potential for depleted aquifer systems to recover.
Author	Jasechko, Scott Seybold, Hansjörg Fan, Ying Kirchner, James W. Taylor, Richard G. Shamsudduha, Mohammad Fallatah, Othman Perrone, Debra
Author_xml	– sequence: 1 givenname: Scott orcidid: 0000-0001-6470-7708 surname: Jasechko fullname: Jasechko, Scott email: jasechko@ucsb.edu organization: Bren School of Environmental Science & Management, University of California, Santa Barbara – sequence: 2 givenname: Hansjörg surname: Seybold fullname: Seybold, Hansjörg organization: Department of Environmental Systems Sciences, ETH Zürich – sequence: 3 givenname: Debra orcidid: 0000-0002-4268-8478 surname: Perrone fullname: Perrone, Debra organization: Environmental Studies Program, University of California, Santa Barbara – sequence: 4 givenname: Ying orcidid: 0000-0002-0024-7965 surname: Fan fullname: Fan, Ying organization: Department of Earth and Planetary Sciences, Rutgers University – sequence: 5 givenname: Mohammad orcidid: 0000-0002-9708-7223 surname: Shamsudduha fullname: Shamsudduha, Mohammad organization: Institute for Risk and Disaster Reduction, University College London – sequence: 6 givenname: Richard G. orcidid: 0000-0002-9867-8033 surname: Taylor fullname: Taylor, Richard G. organization: Department of Geography, University College London – sequence: 7 givenname: Othman orcidid: 0000-0001-6189-9767 surname: Fallatah fullname: Fallatah, Othman organization: Department of Nuclear Engineering, Faculty of Engineering, King Abdulaziz University, Center for Training and Radiation Protection, Faculty of Engineering, King Abdulaziz University – sequence: 8 givenname: James W. surname: Kirchner fullname: Kirchner, James W. organization: Department of Environmental Systems Sciences, ETH Zürich, Swiss Federal Research Institute WSL, Department of Earth and Planetary Science, University of California, Berkeley
BackLink	https://www.ncbi.nlm.nih.gov/pubmed/38267682$$D View this record in MEDLINE/PubMed
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Snippet	Groundwater resources are vital to ecosystems and livelihoods. Excessive groundwater withdrawals can cause groundwater levels to decline 1 – 10 , resulting in... Groundwater resources are vital to ecosystems and livelihoods. Excessive groundwater withdrawals can cause groundwater levels to decline 1–10 , resulting in... Groundwater resources are vital to ecosystems and livelihoods. Excessive groundwater withdrawals can cause groundwater levels to decline , resulting in... Groundwater resources are vital to ecosystems and livelihoods. Excessive ground water withdrawals can cause ground water levels to decline1-10, resulting in... Groundwater resources are vital to ecosystems and livelihoods. Excessive groundwater withdrawals can cause groundwater levels to decline1-10, resulting in... Groundwater resources are vital to ecosystems and livelihoods. Excessive groundwater withdrawals can cause groundwater levels to decline1–10, resulting in...
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SubjectTerms	20th century 21st century 704/172 704/242 Acceleration Agricultural land Aquifer management Aquifer recharge Aquifer systems Aquifers Chemical analysis Ecosystem Groundwater Groundwater - analysis Groundwater depletion Groundwater levels Groundwater recharge Groundwater resources Humanities and Social Sciences multidisciplinary Precipitation Satellites Science Science (multidisciplinary) Seawater Stream discharge Stream flow Surface water Time series Trends Water analysis Water levels Water resources Water Supply - statistics & numerical data
Title	Rapid groundwater decline and some cases of recovery in aquifers globally
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