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Parafluvial zones occur in emergent gravel bars and other river sediment structures where exchange with surface water is limited to horizontal inflow and outflow. Within parafluvial zones, interstitial water flows down longitudinal flowpaths in response to hydraulic‐head gradients. Changes in physical and biogeochemical conditions along these flowpaths lead to the formation of longitudinal gradients...
Flood‐related disturbances are predicted to be seriously altered by climate change effects, and this will have strong implications for stream communities. Predicting how and why community structure responds to changes in disturbance regimes will require measures of disturbance that are closely linked to community variability. A range of disturbance measures have been tested for their ability to explain...
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