Difference between revisions of "Category:03. Flow dynamics improvement"
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==General description== | ==General description== | ||
| − | Several pressures affect discharge and its timing, i.e. the flow regime, such as changes in land cover, soil structure and compacting, loss of floodplains and wetlands, | + | Several pressures affect discharge and its timing, i.e. the flow regime, such as changes in land cover, soil structure and compacting, loss of floodplains and wetlands, stormwater runoff from urban areas, and hydropeaking. The loss of water retention combined with accelerated runoff typically increases the frequency and magnitude of flood peaks but also reduces the availability of water to streams during the prevailing low flow (base flow) periods. |
In addition to the measures listed in this category, [http://wiki.reformrivers.eu/index.php/Category:01._Water_flow_quantity_improvement#General_description/ Category 01: Water flow quantity improvement] covers similar aspects. | In addition to the measures listed in this category, [http://wiki.reformrivers.eu/index.php/Category:01._Water_flow_quantity_improvement#General_description/ Category 01: Water flow quantity improvement] covers similar aspects. | ||
Revision as of 13:25, 22 December 2015
Flow dynamics improvement
General description
Several pressures affect discharge and its timing, i.e. the flow regime, such as changes in land cover, soil structure and compacting, loss of floodplains and wetlands, stormwater runoff from urban areas, and hydropeaking. The loss of water retention combined with accelerated runoff typically increases the frequency and magnitude of flood peaks but also reduces the availability of water to streams during the prevailing low flow (base flow) periods.
In addition to the measures listed in this category, Category 01: Water flow quantity improvement covers similar aspects.
Pages in category "03. Flow dynamics improvement"
The following 9 pages are in this category, out of 9 total.
EF |
ILM |
M cont.RS |
