Hysteresis and adaptation time scales of salt intrusion and the Turbidity Maximum Zone in a tidal estuary

• Salt intrusion and TMZ location are determined using 7 years of monitoring data. • The combined effects of discharge, tidal range and surge events are analyzed. • Spatial and temporal lags are quantified in response to changes in drivers. • There is a hysteresis between discharge and salt intrusion/TMZ location. • The estuary is in a constant state of adjustment. Salt intrusion and sediment dynamics affect the water quality of estuaries. Multiple factors, such as river discharge, tidal forcing and surge events influence salt intrusion and the location of the Turbidity Maximum Zone (TMZ). As these drivers vary frequently, estuarine systems are in a permanent state of adaptation. This study quantifies the spatio-temporal variability in response to the change in drivers for a typical tidal, funnel-shaped estuary. Using 7 years of monitoring data of discharge, tides, salinity and turbidity, we determined the dynamics of the along-channel displacement of the salt intrusion and TMZ location along the Weser estuary (North Sea, Germany). Both parameters exhibit large lags in their response to changes in discharge. Fast changes such as discharge peaks (Q > 450 m 3 /s), induce a substantial hysteresis in salt intrusion and TMZ location. The average temporal lag for the system to adapt to a discharge peak is 16 tidal cycles. The influence of tidal range depends on the season (high or low discharge) and the corresponding lag is comparatively small (on average, 3 tidal cycles). Moreover, surge events introduce substantial and random variations of the salt intrusion and TMZ location, without lag. The largest along-channel displacement (18.5 km) is due to discharge, which is 4 times higher than the displacement induced by surge. This study enhances our understanding of the response and adaptation times of estuaries to driver variability and provides insights into how discharge, spring-neap variability of the tidal range, and surge events collectively control salt intrusion and TMZ location.

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Publication Details

Journal
Journal of Hydrology
Published
2025-05-25
DOI
https://doi.org/10.1016/j.jhydrol.2025.133564
Citations
1
Primary Topic
Oceanographic and Atmospheric Processes
Type
article
Field-Weighted Citation Impact
1.79
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article

Hysteresis and adaptation time scales of salt intrusion and the Turbidity Maximum Zone in a tidal estuary

Marius Becker, Frank Kösters, Carolina Consuegra, C. L. Winter
1 citations
Journal of Hydrology
Oceanographic and Atmospheric Processes
1.79
article

Hysteresis and adaptation time scales of salt intrusion and the Turbidity Maximum Zone in a tidal estuary

Marius Becker, Frank Kösters, Carolina Consuegra, C. L. Winter
article en
1 citations

Abstract

• Salt intrusion and TMZ location are determined using 7 years of monitoring data. • The combined effects of discharge, tidal range and surge events are analyzed. • Spatial and temporal lags are quantified in response to changes in drivers. • There is a hysteresis between discharge and salt intrusion/TMZ location. • The estuary is in a constant state of adjustment. Salt intrusion and sediment dynamics affect the water quality of estuaries. Multiple factors, such as river discharge, tidal forcing and surge events influence salt intrusion and the location of the Turbidity Maximum Zone (TMZ). As these drivers vary frequently, estuarine systems are in a permanent state of adaptation. This study quantifies the spatio-temporal variability in response to the change in drivers for a typical tidal, funnel-shaped estuary. Using 7 years of monitoring data of discharge, tides, salinity and turbidity, we determined the dynamics of the along-channel displacement of the salt intrusion and TMZ location along the Weser estuary (North Sea, Germany). Both parameters exhibit large lags in their response to changes in discharge. Fast changes such as discharge peaks (Q > 450 m 3 /s), induce a substantial hysteresis in salt intrusion and TMZ location. The average temporal lag for the system to adapt to a discharge peak is 16 tidal cycles. The influence of tidal range depends on the season (high or low discharge) and the corresponding lag is comparatively small (on average, 3 tidal cycles). Moreover, surge events introduce substantial and random variations of the salt intrusion and TMZ location, without lag. The largest along-channel displacement (18.5 km) is due to discharge, which is 4 times higher than the displacement induced by surge. This study enhances our understanding of the response and adaptation times of estuaries to driver variability and provides insights into how discharge, spring-neap variability of the tidal range, and surge events collectively control salt intrusion and TMZ location.

Journal of HydrologyVol. 661
Christian-Albrechts-Universität zu Kiel (DE), Bundesanstalt für Wasserbau (DE)
Life below water
Openalex Percentile: Top 17%
Oceanographic and Atmospheric Processes
1.79
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