EGU25-864, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-864
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Tuesday, 29 Apr, 10:05–10:15 (CEST)
 
Room 0.16
GRACE satellites and in-situ well data reveals that specific yield declines with depleting groundwater levels
K Satish Kumar1, Maya Raghunath Suryawanshi1, Chethan Varadaganahalli Anandagowda1, Balaram Shaw1, Vandana Sukumaran1, Aayushi Kochar1, and Bramha Dutt Vishwakarma1,2
K Satish Kumar et al.
  • 1Interdisciplinary Centre for Water Research, Indian Institute of Science, Bangalore, India (ksatishkumar@iisc.ac.in)
  • 2Centre for Earth Sciences, Indian Institute of Science, Bengaluru, India

Specific yield (Sy) is defined as the ratio of the volume of water that saturated rock or soil yields by gravity to the total volume of the rock or soil. Sy is often taken as a constant that when multiplied to groundwater level change provides water volume change, hence it is crucial in validating Gravity Recovery And Climate Experiment (GRACE)-derived groundwater changes, providing estimates of available groundwater resources, and in modelling groundwater aquifers. In this study, we used GRACE data and available quality-controlled in-situ well data to estimate Sy instead. Our hope was that it would match the available Sy, however we observed a time-varying Sy. Upon further investigation we found a negative correlation between water level and Sy. Hence the time-evolution of Sy was due to changes in the water level. We processed available well data and GRACE(-FO) in India, the United States, Europe, and Australia, spanning from January 2004 to December 2022. We also developed a general law/empirical relationship between Sy and groundwater level. All regional-specific empirical relationships exhibit a decrease in Sy as the average groundwater level depth drops, but the decay rate of Sy is notably faster in India (0.17 ± 0.04 m-1) compared to the United States (0.03 ± 0.01 m-1), Australia (0.06 ± 0.02 m-1), and European countries (0.04 ± 0.03 m-1). This empirical expression allows for the estimation of Sy based on readily available groundwater level data, thus supporting large-scale groundwater assessments and modelling efforts. At the global scale, a 50% decrease in Sy results in a groundwater level depletion of ~17 meters. However, in India, due to a faster decay rate, the same 50% reduction in Sy causes a groundwater level depletion of ~4 meters. This relationship can be utilized by hydrologists, water resource managers, and policymakers to predict Sy and assess changes in groundwater levels over time, aiding in more effective and sustainable water resource management.

How to cite: Kumar, K. S., Suryawanshi, M. R., Varadaganahalli Anandagowda, C., Shaw, B., Sukumaran, V., Kochar, A., and Vishwakarma, B. D.: GRACE satellites and in-situ well data reveals that specific yield declines with depleting groundwater levels, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-864, https://doi.org/10.5194/egusphere-egu25-864, 2025.