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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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Citations
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Journal ArticleDOI

The global groundwater crisis

TL;DR: In this article, the authors argue that groundwater depletion the world over poses a far greater threat to global water security than is currently acknowledged, and propose a solution to this problem.
Journal ArticleDOI

Emerging trends in global freshwater availability.

TL;DR: Analysis of 2002–2016 GRACE satellite observations of terrestrial water storage reveals substantial changes in freshwater resources globally, which are driven by natural and anthropogenic climate variability and human activities.
Journal ArticleDOI

Quantifying renewable groundwater stress with GRACE

TL;DR: In this paper, renewable groundwater stress is quantified in the world's largest aquifersCharacteristic stress regimes are defined to determine the severity of stress overstressed aquifer are mainly in rangeland biomes with some croplands.
Journal ArticleDOI

Global-scale assessment of groundwater depletion and related groundwater abstractions: Combining hydrological modeling with information from well observations and GRACE satellites

TL;DR: In this article, a new version of the global hydrological model WaterGAP was applied to derive groundwater depletion at the grid cell, country, and global levels, which simulates not only net groundwater abstractions and groundwater recharge from soils, but also surface water recharge from surface water bodies in dry regions.
References
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Journal ArticleDOI

Detectability of variations in continental water storage from satellite observations of the time dependent gravity field

TL;DR: In this article, the authors characterize water storage changes in 20 drainage basins ranging in size from 130,000 to 5,782,000 km2 and use estimates of uncertainty in the GRACE technique to determine in which basins water storage change may be detectable by GRACE and how this detectability may vary in space and time.
Journal ArticleDOI

The potential for satellite-based monitoring of groundwater storage changes using GRACE: the High Plains aquifer, Central US

TL;DR: In the High Plains aquifer, the magnitude of annual groundwater storage changes averaged 19.8 mm between 1987 and 1998 and total uncertainty is predicted to be about 8.7 mm as mentioned in this paper.
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Evaluation of new GRACE time‐variable gravity data over the ocean

TL;DR: In this article, the mean uncertainty of GRACE maps determined from an average of data from all three processing centers is estimated to be less than 1.8 cm RMS at 750 km and 2.4 cm at 500 km smoothing.
Journal ArticleDOI

Impact of climate change on the water resources of the eastern Mediterranean and Middle East region: Modeled 21st century changes and implications

TL;DR: In this article, the authors investigated the likely effects of climate change on the water resources of the eastern Mediterranean and Middle East region using a high-resolution regional climate model (PRECIS) by comparing precipitation simulations of 2040-2069 and 2070-2099 with 1961-1990.
Journal ArticleDOI

A comparison of terrestrial water storage variations from GRACE with in situ measurements from Illinois

TL;DR: In this article, the first direct comparison of terrestrial water storage estimates from the Gravity Recovery and Climate Experiment (GRACE) satellite mission to in situ hydrological observations is presented.
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