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Mapping the spatially-variable elastic storage properties of the aquifer
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Classroom Contents
Geodetic Insights into Water-driven Aquifer and Ice Sheet Dynamics
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- 1 Intro
- 2 Poroelastic vs inelastic aquifer response to groundwater fluctuations
- 3 Understanding the mechanics of aquifer systems is central to the sustainable exploitation of groundwater resources
- 4 Monitoring the health of aquifer systems with geodesy
- 5 A multi-technique approach for aquifer monitoring
- 6 Long history of inelastic subsidence in the San Joaquin Valley
- 7 Characterizing groundwater fluctuations at the seasonal and drought timescales
- 8 Mapping the spatially-variable elastic storage properties of the aquifer
- 9 Poroelastic deformation due to long-term groundwater decline
- 10 Initiation and acceleration of inelastic subsidence starting in 2021
- 11 Surface deformation does not recover despite groundwater recharge
- 12 Meltwater is ubiquitous on Greenland and Antarctic ice sheets
- 13 Supraglacial lakes in Greenland are expanding inland with warming climate
- 14 2022-2023 GNSS campaign in Western Greenland
- 15 Tracking ice dynamics with on-ice GNSS
- 16 Tracking supraglacial lake drainages with GNSS
- 17 Understanding displacement signals from supraglacial lake drainage event
- 18 Estimating (large-scale) elastic loading deformation with GRACE
