Consequences of the Aral Sea restoration for its present physical state: temperature, mixing, and oxygen regime
The Aral Sea is both an example of large-scale environmental degradation caused by human activity and a message of hope through its partial restoration. The field observations and model scenarios show that the restored part of the Aral Sea appears to be healthy in terms of vertical mixing and oxygenation, but small changes of water level or transparency could alter the entire ecosystem.
Multigene phylogeny, morphology, and pathogenicity uncover two novel Globisporangium species (Oomycota) from freshwater habitats in northwestern Iran
The role of trade-off shapes for community adaptation and maintenance of ecosystem functions under environmental change
Revisiting Cyanobacteria-Temperature Dynamics: Intraspecific Competition and Trait Diversity as Keys to Predicting Harmful Algal Blooms under Climate Change
Urban Hydrological Connectivity and Response Patterns Across Timescales: An Integrated Time-Frequency Domain Analysis
The authors investigated the interconnections of rainfall, groundwater and stream flow in the Wuhle river in Berlin using autocorrelation, cross-correlation and time-frequency analyses of long-term data. Despite the strong influence of urban storm drainage, they showed a high degree of persistence of the groundwater signals.
Integral Modelling Approach for Hyporheic Exchange due to Porous Log Jams: Comparison With Experiments and Sensitivity Studies
Where, when, and how FAIR do data from aquatic mesocosm experiments get published?
Individual differences in speed–accuracy trade-off influence social decision-making in dyads
Hydrological Connectivity Dominates NO3-N Cycling in Complex Landscapes – Insights From Integration of Isotopes and Water Quality Modeling
The authors integrated isotope-aided with N modelling to quantify the (dis)connection of different flow paths and related biogeochemical transformations, which is important for land and water management. Hydrological connectivity controls N transformations by regulating soil moisture and available NO3-N for processing from upstream inflows.