Abstract
The comment by Davies and Simmons et al. (2023) argues that aquifer-eustasy works in-phase with glacio-eustasy and its magnitudes are on scale of decimeters. However, the in-phase relationship and limited magnitudes are inferred by climate models which based solely on volume changes in shallow groundwater and fail to take into account the capacity of deeper-seated aquifers. If deep groundwater is properly considered as well, both the in-phase relationship and magnitudes of aquifer-eustasy need to be reevaluated. More through investigations are required to understand the processes of charge and discharge in continental aquifers at different depths.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
