Details zur Publikation |
| Kategorie | Textpublikation |
| Referenztyp | Zeitschriften |
| DOI | 10.5194/hess-30-4611-2026 |
Lizenz ![]() |
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| Titel (primär) | Four decades of full-depth profiles reveal layer-resolved drivers of reservoir thermal regimes and episodic hypolimnetic warming |
| Autor | Mi, C.; Kong, X.; Jiang, Y.; Chan, C.N.; Rinke, K. |
| Quelle | Hydrology and Earth System Sciences |
| Erscheinungsjahr | 2026 |
| Department | SEEFO |
| Band/Volume | 30 |
| Heft | 14 |
| Sprache | englisch |
| Topic | T5 Future Landscapes |
| Supplements | Supplement 1 |
| Abstract | Thermal structure shapes ecological dynamics in lakes and reservoirs. Yet full-profile temperature records over multi-decades remain scarce, constraining mechanistic understanding of depth-resolved thermal changes and subseasonal extremes (e.g., surface heat waves and late-season hypolimnetic warming). In this study, we focused on Rappbode Reservoir, Germany's largest drinking-water reservoir, and compiled four decades of high-resolution, full-depth temperature profiles with concurrent hydro-meteorological records that are rarely available for stratified systems. Building on these data, we developed a novel two-step analytical framework that integrates long-term monitoring and process-based modelling to yield a high-resolution, internally consistent dataset of spatiotemporal temperature dynamics. We then applied interpretable machine learning to quantify depth-specific statistical attributions of hydro-meteorological and operational drivers, using process-based interpretation to assess mechanisms associated with late-stratification hypolimnetic warming. Our results suggested that driver contributions varied markedly with depth and stratification phase: stratification-strength metrics tied to atmospheric heat exchange (i.e., surface temperature, vertical temperature difference, Schmidt stability) showed the largest SHAP contributions from the 30 d antecedent moving average of shortwave radiation and air temperature. For hypolimnetic temperature, outflow discharge accounted for the largest contribution during late stratification. Additional process-based analyses supported a link between episodic hypolimnetic warming by up to 10 °C in four specific years and intensified deep withdrawals, which weakened the density gradient and promoted downward transport of warm upper-layer water into the hypolimnion. The dual-perspective framework developed here, which integrates process-based and machine-learning approaches, is broadly transferable for analyzing ecological processes and supporting evidence-based management in stratified waters. |
| Mi, C., Kong, X., Jiang, Y., Chan, C.N., Rinke, K. (2026): Four decades of full-depth profiles reveal layer-resolved drivers of reservoir thermal regimes and episodic hypolimnetic warming Hydrol. Earth Syst. Sci. 30 (14) 10.5194/hess-30-4611-2026 |
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