Articles | Volume 30, issue 15
https://doi.org/10.5194/hess-30-4889-2026
https://doi.org/10.5194/hess-30-4889-2026
Research article
 | 
04 Aug 2026
Research article |  | 04 Aug 2026

Hysteresis between groundwater and surface water levels indicates the states of hydrological turnover affecting solute transport and redox processes

Lars Bäthke and Tobias Schuetz

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Latest update: 04 Aug 2026
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Short summary

We investigated the interplay between stream stage and near-stream groundwater levels using hysteresis patterns to characterize hydrological turnover (HT) and exchange dynamics. Based on two years of high-resolution data, hysteresis direction and magnitude track seasonal system states. The hysteresis index (h-index) is related to HT and serves as a diagnostic indicator of connectivity, storage, and hyporheic exchange, with implications for biogeochemical processes under drought.

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