Terrestrial water load and groundwater fluctuation in the Bengal Basin
Groundwater-level fluctuations represent hydraulic responses to changes in groundwater storage due to aquifer recharge and drainage as well as to changes in stress that include water mass loading and unloading above the aquifer surface. The latter 'poroelastic' response of confined aquifer...
| Main Authors: | , , , , , , , |
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| Format: | Journal Article |
| Published: |
Nature Publishing Group
2017
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| Online Access: | http://hdl.handle.net/20.500.11937/67360 |