Geodetic Insights into Water-driven Aquifer and Ice Sheet Dynamics

Geodetic Insights into Water-driven Aquifer and Ice Sheet Dynamics

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Tracking supraglacial lake drainages with GNSS

16 of 18

16 of 18

Tracking supraglacial lake drainages with GNSS

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Geodetic Insights into Water-driven Aquifer and Ice Sheet Dynamics

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

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