Changes to the river bed
The build-up of gravel has changed the profile of the river bed, which means that water level is higher than pre-flood, however, the actual amount of flow or discharge is similar. With the river now having a wider, flatter profile in some places, the warm weather and hot summer ahead will create conditions for algae and cyanobacteria to proliferate. There was more gravel than would occur after a flood in a ‘natural system’, and FOM’s view is that recent pine harvesting would not have helped.
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