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Land subsidence in Iran caused by widespread water reservoir overexploitation

Motagh, Mahdi ; Walter, Thomas R. ; Sharifi, Mohammad Ali ; Fielding, Eric ; Schenk, Andreas ; Anderssohn, Jan ; Zschau, Jochen

Geophysical research letters, 2008-08, Vol.35 (16), p.L16403-n/a [Periódico revisado por pares]

Washington, DC: American Geophysical Union

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  • Título:
    Land subsidence in Iran caused by widespread water reservoir overexploitation
  • Autor: Motagh, Mahdi ; Walter, Thomas R. ; Sharifi, Mohammad Ali ; Fielding, Eric ; Schenk, Andreas ; Anderssohn, Jan ; Zschau, Jochen
  • Assuntos: Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Freshwater ; Geodesy and Gravity ; groundwater ; Hydrology ; inSAR ; Non-tectonic deformation ; Remote sensing ; Reservoirs (surface) ; Space geodetic surveys ; subsidence
  • É parte de: Geophysical research letters, 2008-08, Vol.35 (16), p.L16403-n/a
  • Notas: istex:C1F439F119AB76E2F796CD44031434E647A9B239
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    ArticleID:2008GL033814
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  • Descrição: The increasing demands upon groundwater resources due to expanding metropolitan and agricultural areas are a serious challenge, particularly in semiarid and arid regions. In Iran, decades of unrestrained groundwater extraction for domestic, agricultural, and industrial use have resulted in a precipitous depletion of this valuable resource. Here we show that the decline in groundwater levels is associated with land‐surface deformation on local and regional scales. Combining water‐level data with satellite radar observations provides evidence for the prevalence of compacting aquifers in the country. Groundwater level decline is often associated with destruction of the aquifers, which appears to be a common problem in the groundwater basins of central and northeast Iran. Global warming and future climate change will affect arid and semiarid areas in the coming decades, further augmenting hazards associated with groundwater‐induced land subsidence.
  • Editor: Washington, DC: American Geophysical Union
  • Idioma: Inglês

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