Past and future contribution of global groundwater depletion to sea-level rise

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题名:	Past and future contribution of global groundwater depletion to sea-level rise
作者:	趙丰;Wada, Yoshihide;van Beek, Ludovicus P. H.;Sperna Weiland, Frederiek C.;Chao, Benjamin F.;Wu, Yun-Hao;Bierkens, Marc F. P.
贡献者:	地球科學學院地球科學學系
关键词:	Assessments;Climate;Climate change;Dams;Depletion;Earth;Earth sciences;Earth, ocean, space;Estimates;Exact sciences and technology;global hydrology;Groundwater;Groundwater depletion;Hydrology;Projection;reservoir impoundment;Reservoirs;Sea level;sea level rise;Tapering;Terrestrial environments;terrestrial water sources;Water demand
日期:	2012-05-01
上传时间:	2026-04-23 11:39:57 (UTC+8)
出版者:	Wiley-Blackwell;Washington, DC: Blackwell Publishing Ltd
摘要:	摘要： Recent studies suggest the increasing contribution of groundwater depletion to global sea‐level rise. Groundwater depletion has more than doubled during the last decades, primarily due to increase in water demand, while the increase in water impoundments behind dams has been tapering off since the 1990s. As a result, the contribution of groundwater depletion to sea‐level rise is likely to dominate over those of other terrestrial water sources in the coming decades. Yet, no projections into the 21st century are available. Here we present a reconstruction of past groundwater depletion and its contribution to global sea‐level variation, as well as 21st century projections based on three combined socio‐economic and climate scenarios (SRES) with transient climate forcing from three General Circulation Models (GCMs). We validate and correct estimated groundwater depletion with independent local and regional assessments, and place our results in context of other terrestrial water contributions to sea‐level variation. Our results show that the contribution of groundwater depletion to sea‐level increased from 0.035 (±0.009) mm yr−1 in 1900 to 0.57 (±0.09) mm yr−1 in 2000, and is projected to increase to 0.82 (±0.13) mm yr−1 by the year 2050. We estimate the net contribution of terrestrial sources to be negative of order −0.15 (±0.09) mm yr−1 over 1970–1990 as a result of dam impoundment. However, we estimate this to become positive of order +0.25 (±0.09) mm yr−1 over 1990–2000 due to increased groundwater depletion and decreased dam building. We project the net terrestrial contribution to increase to +0.87 (±0.14) mm yr−1 by 2050. As a result, the cumulative contribution will become positive by 2015, offsetting dam impoundment (maximum −31 ± 3.1 mm in 2010), and resulting in a total rise of +31 (±11) mm by 2050. 其他題名： Geophys. Res. Lett 出版者： Washington, DC: Blackwell Publishing Ltd 出版日期： 2012-05 出處： Geophysical Research Letters, 2012-05, Vol.39 (9), p.L09402--n/a 資源來源： Wiley Online Library All Journals 版權： Copyright 2012 by the American Geophysical Union 版權： 2015 INIST-CNRS 識別號： ISSN: 0094-8276 識別號： ISSN: 1944-8007 識別號： EISSN: 1944-8007 識別號： DOI: 10.1029/2012GL051230 識別號： CODEN: GPRLAJ
显示于类别:	[地球科學學系] 期刊論文

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