While the researchers try to address this by focusing on trends that are robust, the short 22-year period of observation using GRACE/GRACE-FO data limits the certainty about long-term changes and the ability to fully distinguish them from natural climate fluctuations. Longer-term monitoring is needed to confidently establish persistent trends.
Reliance on models with inherent uncertainties
The study relies on models to separate the various components of total water storage (groundwater, surface water, soil moisture, snow water equivalent). Model outputs inherently have uncertainties due to simplifications and limitations in representing complex hydrological processes.
Attribution of observed changes
The study notes that there is a shift in the location and timing of drying/wetting trends, but it doesn't definitively attribute this shift to a specific cause like long-term climate oscillations like the Pacific Decadal Oscillation (PDO). Further research is needed to disentangle the various driving forces.
Small changes in TWS in some areas
While the study finds significant increases in drying regions, the absolute values of TWS changes in some of these areas are small compared to the annual renewable freshwater supply. This might be misinterpreted.
Limited consideration of other climate patterns
The study doesn't fully explore the influence of other climate phenomena besides El Niño and La Niña on terrestrial water storage. Other climate patterns could potentially influence regional water storage, but their role is not extensively examined.