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Open AccessJournal ArticleDOI

Groundwater depletion in the Middle East from GRACE with implications for transboundary water management in the Tigris-Euphrates-Western Iran region

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TLDR
Observations from the GRACE satellite mission are used to evaluate freshwater storage trends in the north-central Middle East, including portions of the Tigris and Euphrates River Basins and western Iran, from January 2003 to December 2009 to indicate that groundwater losses are the major source of this trend.
Abstract
In this study, we use observations from the Gravity Recovery and Climate Experiment (GRACE) satellite mission to evaluate freshwater storage trends in the north-central Middle East, including portions of the Tigris and Euphrates River Basins and western Iran, from January 2003 to December 2009. GRACE data show an alarming rate of decrease in total water storage of approximately -27.2 plus or minus 0.6 millimeters per year equivalent water height, equal to a volume of 143.6 cubic kimometers during the course of the study period. Additional remote-sensing information and output from land surface models were used to identify that groundwater losses are the major source of this trend. The approach used in this study provides an example of ''best current capabilities'' in regions like the Middle East, where data access can be severely limited. Results indicate that the region lost 17.3 plus or minus 2.1 millimeters per year equivalent water height of groundwater during the study period, or 91.3 plus or minus 10.9 cubic kilometers in volume. Furthermore, results raise important issues regarding water use in transboundary river basins and aquifers, including the necessity of international water use treaties and resolving discrepancies in international water law, while amplifying the need for increased monitoring for core components of the water budget.

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Journal ArticleDOI

Aquifer Depletion in the Arlit Mining Area (Tim Mersoï Basin, North Niger)

TL;DR: In this paper, the authors evaluated the groundwater storage changes of the Tim Mersoi Basin and analyzed the spatio-temporal evolution of the Tarat aquifer under the effect of mining activities in the Arlit region.
Book ChapterDOI

Integration of GRACE Data for Improvement of Hydrological Models

TL;DR: In this paper, the integration methodologies highlighting the different aspects of model improvement such as the hydrologic parameter of interest, complexity of the model framework, and representation of hydrological processes are discussed.
Journal ArticleDOI

How Droughts Influence Earthquakes

Ren Diandong, +1 more
Abstract: Earthquakes result from strain build-up from without and weakening from within faults. A generic co-seismic condition is presented that includes just three angles representing, respectively, fault geometry, fault strength, and the ratio of fault coupling to lithostatic loading. Correspondingly, gravity fluctuations, bridging effects, and granular material production/distribution form an earthquake triad. As a dynamic constituent of the gravity field, groundwater fluctuation is the nexus between the triad components. It is pivotal in regulating major seismic irregularity, by reducing natural (dry, or purely tectonic, stationary seismicity) inter-seismic periods and by lowering magnitudes. Specifically, to exert stress on the fault, groundwater does not need to reside deep in proximity to the locked fault interface, as it can work remotely. It can act mechanically-direct (MD), by a differential de-loading and superimposing a seismogenetic lateral stress field, thereby aiding plate-coupling, from without, or mechanically-indirect (MI) by enhancing fault fatigue, and hence weakening the fault, from within. To verify this hypothesis, gravity measurements, and a numerical model, are used. The remote action hypothesis is globally applicable. Detailed results are presented for the Himalayan and New Zealand regions. The gravity recovery and Climate experiment (GRACE measurements) reveals that major earthquakes (Mw 5 and above) always occur in the dry stage, indicating drought and associated groundwater extraction is an important trigger for major earthquakes. By exploring 73 historical records successfully reproduced by the model, it is found that for collisional (e.g., the peri-Tibetan Plateau) and strike-slip (e.g., the San Andreas Fault) systems, the MD mechanism dominates, because the orographically induced spatially highly variable precipitation is channeled into greater depth by through-cut faults. Droughts elsewhere also are seismogenetic, but likely through MI effects. In a warming future climate, mechanisms identified here play a greater role in increasing the recurrence frequency of major earthquakes, but also in slightly reducing their severity.
Journal ArticleDOI

A Review of Managed Aquifer Recharge Potential in the Middle East and North Africa Region with Examples from the Kingdom of Saudi Arabia and the United Arab Emirates

TL;DR: In this paper , the authors present an analysis of groundwater renewability and the effectiveness of recharge dams on groundwater recharge, as well as the potential of MAR technology in the MENA region.
References
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Journal ArticleDOI

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TL;DR: In this article, the authors constructed a 2.5° latitude-longitude grid for the 17-yr period from 1979 to 1995 by merging several kinds of information sources with different characteristics, including gauge observations, estimates inferred from a variety of satellite observations, and the NCEP-NCAR reanalysis.
Journal ArticleDOI

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Journal ArticleDOI

A simple hydrologically based model of land surface water and energy fluxes for general circulation models

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Journal ArticleDOI

Satellite-based estimates of groundwater depletion in India

TL;DR: The available evidence suggests that unsustainable consumption of groundwater for irrigation and other anthropogenic uses is likely to be the cause of groundwater depletion in northwest India and the consequences for the 114,000,000 residents of the region may include a reduction of agricultural output and shortages of potable water, leading to extensive socioeconomic stresses.
Journal ArticleDOI

GRACE measurements of mass variability in the Earth system.

TL;DR: Geoid variations observed over South America that can be largely attributed to surface water and groundwater changes show a clear separation between the large Amazon watershed and the smaller watersheds to the north.
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