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Bengaluru groundwater fluctuations reflected in crustal deformation


Affiliations
1 ACSIR-Academy of Scientific and Innovative Research, Ghaziabad 201 002, India
2 CSIR-National Geophysical Research Institute, Uppal Road, Hyderabad 500 007, India
 

The water crisis in Bengaluru is mainly due to a large deficit in rainfall during 2023. Less precipitation led to less recharge and subsurface storage. The recharge or subsurface loading causes elastic deformation of the crust, namely subsidence during monsoon and its recovery afterward. Such deformation can be measured using continuous GPS measurements. We see an excellent correspondence between the trends of Bengaluru rainfall over the past two decades and the vertical surface deformation derived from the continuous GPS measurements at the IISc site. Decreased precipitation in 2023 led to less annual subsidence than in the earlier four years when the rainfall increased in subsequent years from 2019 to 2022, increasing subsidence every year following the monsoon. The rainfall pattern in Hyderabad was similar to that in Bengaluru, but in terms of the magnitude of rainfall and corresponding crustal subsidence, which was estimated from the GPS measurements at the HYDE site, it was less pronounced. These two examples demonstrate the influence of the hydrological process on the crustal deformation process.

Keywords

Crustal deformation, GPS, groundwater, rainfall.
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  • Bengaluru groundwater fluctuations reflected in crustal deformation

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Authors

Joshi K. Catherine
ACSIR-Academy of Scientific and Innovative Research, Ghaziabad 201 002, India
Shubham Rajewar
CSIR-National Geophysical Research Institute, Uppal Road, Hyderabad 500 007, India
Akarsh Asoka
ACSIR-Academy of Scientific and Innovative Research, Ghaziabad 201 002, India
Kalpna Gahalaut
CSIR-National Geophysical Research Institute, Uppal Road, Hyderabad 500 007, India
Vineet Gahalaut
ACSIR-Academy of Scientific and Innovative Research, Ghaziabad 201 002, India

Abstract


The water crisis in Bengaluru is mainly due to a large deficit in rainfall during 2023. Less precipitation led to less recharge and subsurface storage. The recharge or subsurface loading causes elastic deformation of the crust, namely subsidence during monsoon and its recovery afterward. Such deformation can be measured using continuous GPS measurements. We see an excellent correspondence between the trends of Bengaluru rainfall over the past two decades and the vertical surface deformation derived from the continuous GPS measurements at the IISc site. Decreased precipitation in 2023 led to less annual subsidence than in the earlier four years when the rainfall increased in subsequent years from 2019 to 2022, increasing subsidence every year following the monsoon. The rainfall pattern in Hyderabad was similar to that in Bengaluru, but in terms of the magnitude of rainfall and corresponding crustal subsidence, which was estimated from the GPS measurements at the HYDE site, it was less pronounced. These two examples demonstrate the influence of the hydrological process on the crustal deformation process.

Keywords


Crustal deformation, GPS, groundwater, rainfall.



DOI: https://doi.org/10.18520/cs%2Fv127%2Fi2%2F238-239