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. 2016 Nov 15;38(1):131–152. doi: 10.1007/s10712-016-9399-6

Table 1.

Global and regional estimates of groundwater depletion (GWD) contribution to sea level rise (SLR)

GWD (km3 year−1) SLR (mm year−1) Year Notes Sources
Global Sahagian et al. (1994) 86.7 0.24 Contemporary Limited regions (e.g., USA, India, China)

Literature

Country statistics

Postel (1999) 200 0.56 Contemporary Global

Literature

Country statistics

Gornitz (2001) 36–108 0.1–0.3 Contemporary Limited regions (e.g., USA, India, China)

Literature

Country statistics

Foster and Loucks (2006) 26.8 0.075 Contemporary Limited regions (e.g., Middle East, Northern Africa)

Literature

Country statistics

Wada et al. (2010)

126 (±32)

283 (±40)

0.35 (±0.09)

0.79 (±0.11)

1960

2000

Depletion equals abstraction in excess of recharge

IGRAC-GGIS

PCR-GLOBWB (0.5°)

Konikow (2011) 145 (±39) 0.4 (±0.11) 2000–2008 Extrapolated for other than USA, north India, North China Plain, Saudi Arabia, Nubian and Sahara In situ groundwater level measurements, GRACE satellite observation, calibrated groundwater model, extrapolation (15.4 %; depletion to abstraction ratio of USA)
Wada et al. (2012)

163 (±28)

204 (±30)

0.45 (±0.07)

0.57 (±0.08)

1990–2000

2000

Corrected against reported regional depletion estimates

IGRAC-GGIS

PCR-GLOBWB (0.5°)

Pokhrel et al. (2012) 455 (±42) 1.27 (±0.12) 2000 Depletion equals water demand in excess of water availability MATSIRO (1.0°)
Döll et al. (2014) 113 0.31 2000–2009 Application of deficit irrigation WaterGAP (0.5o), In situ groundwater level measurements, GRACE satellite observation
Van Dijk et al. (2014) 92 0.26 2003–2012 Without data assimilation, original depletion equals 168 km3 year−1 Data assimilation with GRACE satellite observation
Famiglietti (2014) 77.4 0.22 2003–2013

Time periods vary among studies considered

Limited regions

Various studies using GRACE-derived total terrestrial water storage changes
Pokhrel et al. (2015) 330 0.92 2000 570 km3 year−1 for the global groundwater abstraction for 2000 MATSIRO (1.0°)
Wada et al. (2016)

7.2 (±1.4)

97 (±14)

0.02 (±0.004)

0.27 (±0.04)

1900

2000

Coupled atmosphere-land–ocean model simulation NCAR CESM-CAM4-CLM4 (1.0°)

Regional

Northwest Sahara

Richey et al. (2015) 2.7 0.008 2003–2012 Algeria, Libya, Tunisia GRACE-derived total terrestrial water storage changes
Middle East and North Africa (MENA) Foster and Loucks (2006) 26.8 0.0075 Contemporary

Literature

Country statistics

Voss et al. (2013) 13.0 (±1.6) 0.036 (±0.005) 2003–2009 Cumulative 91.3 (± 10.9) km3 for 2003–2009 GRACE-derived total terrestrial water storage changes
Arabian Richey et al. (2015) 15.5 0.04 2003–2013 Iraq, Jordan, Oman, Qatar, Saudi Arabia, UAE, Yemen GRACE-derived total terrestrial water storage changes
Guarani Richey et al. (2015) 1.0 0.003 2003–2013 Argentina, Brazil, Paraguay, Uruguay GRACE-derived total terrestrial water storage changes
North China Plain (NCP) Cao et al. (2013)

4.0

2.5

4.0

2.0

7.0

4.0

0.01

0.007

0.01

0.006

0.02

0.01

1960–2008

1970s

1980s

1990–1996

1997–2001

2002–2008

Cumulatively 158 km3 for 1960–2008 (20% of pumpage of 807 km3) MODFLOW
Feng et al. (2013) 8.3 (±1.1) 0.02 (±0.03) 2003–2010 2.5 km3 year−1 for shallow aquifers reported by Groundwater Bulletin of China Northern Plains GRACE-derived total terrestrial water storage changes
Huang et al. (2015)

2.5 (±0.4)-PP

1.5 (±0.2)-ECP

0.007 (±0.001)

0.004 (±0.0005)

2003–2012

Piedmont Plain (PP)

East Central Plain (ECP)

GRACE-derived total terrestrial water storage changes
Indus Cheema et al. (2014) 31 0.09 2007 68 km3 of total groundwater abstraction Remote sensing combined with a hydrological model and spatial information on canal water supplies
Northern India Rodell et al. (2009) 17.7 (±4.5) 0.05 (±0.01) 2002–2008 Cumulative 109 km3 for 2002–2008 GRACE-derived total terrestrial water storage changes
Northern India and surrounding regions Tiwari et al. (2009) 54 (±9) 0.15 (±0.03) 2002–2008 GRACE-derived total terrestrial water storage changes
Jacob et al. (2012) 35 0.1 2003–2010 GRACE-derived total terrestrial water storage changes
Bangladesh Shamsudduha et al. (2012)

0.44(±1.24)–2.04(± 0.79)- wet seasons

0.52(± 0.5)–2.83(± 0.42)-annual

0.001(± 0.004)–0.006(± 0.002)

0.002(± 0.001)–0.008(± 0.001)

2003–2007 Depletion of 0.52 (± 0.30)–0.85 (± 0.17) km3 year−1 from borehole hydrographs GRACE-derived total terrestrial water storage changes
California’s Central Valley Famiglietti et al. (2011) 3.1 (± 0.6) 0.009 (± 0.002) 2003–2010 Cumulative 20.3 km3 for 2003–2010 GRACE-derived total terrestrial water storage changes
Scanlon et al. (2012a)

2.0

6–8

0.006

0.017–0.022

1962–2003

2006–2010

Cumulative 24.6 km3 for 1976–1977, 49.3 km3 for 1987–1992, 140 km3 since the 1860s, and 80 km3 since the 1960s MODFLOW
Scanlon et al. (2012b) 8.9 (± 0.9) 0.025 (± 0.0025) 2006–2010 Cumulative 31.0 (± 3.0) km3 for 2006–2010 GRACE-derived total terrestrial water storage changes
High Plains Aquifer Scanlon et al. (2012a)

5.7

7.0

12.5

0.016

0.02

0.035

1950–2007

1987–2007

2003–2013

Cumulative 330 km3 after pre-development in the 1950s MODFLOW
Canning Basin Richey et al. (2015) 3.6 0.01 2003–2013 Australia GRACE-derived total terrestrial water storage changes