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Monitoring groundwater storage changes in the highly seasonal humid tropics: Validation of GRACE measurements in the Bengal Basin
Author(s) -
Shamsudduha M.,
Taylor R. G.,
Longuevergne L.
Publication year - 2012
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/2011wr010993
Subject(s) - environmental science , groundwater recharge , groundwater , hydrology (agriculture) , monsoon , structural basin , water storage , drainage basin , aquifer , climatology , geology , geography , paleontology , geotechnical engineering , cartography , geomorphology , inlet
Satellite monitoring of changes in terrestrial water storage provides invaluable information regarding the basin‐scale dynamics of hydrological systems where ground‐based records are limited. In the Bengal Basin of Bangladesh, we test the ability of satellite measurements under the Gravity Recovery and Climate Experiment (GRACE) to trace both the seasonality and trend in groundwater storage associated with intensive groundwater abstraction for dry‐season irrigation and wet‐season (monsoonal) recharge. We show that GRACE (CSR, GRGS) datasets of recent (2003 to 2007) groundwater storage changes (Δ GWS ) correlate well ( r = 0.77 to 0.93, p value < 0.0001) with in situ borehole records from a network of 236 monitoring stations and account for 44% of the total variation in terrestrial water storage (Δ TWS ); highest correlation ( r = 0.93, p value < 0.0001) and lowest root‐mean‐square error (<4 cm) are realized using a spherical harmonic product of CSR. Changes in surface water storage estimated from a network of 298 river gauging stations and soil‐moisture derived from Land Surface Models explain 22% and 33% of Δ TWS , respectively. Groundwater depletion estimated from borehole hydrographs (−0.52 ± 0.30 km 3 yr −1 ) is within the range of satellite‐derived estimates (−0.44 to −2.04 km 3 yr −1 ) that result from uncertainty associated with the simulation of soil moisture (CLM, NOAH, VIC) and GRACE signal‐processing techniques. Recent (2003 to 2007) estimates of groundwater depletion are substantially greater than long‐term (1985 to 2007) mean (−0.21 ± 0.03 km 3 yr −1 ) and are explained primarily by substantial increases in groundwater abstraction for the dry‐season irrigation and public water supplies over the last two decades.