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As a result, risks generally decreased with higher recycled water contributions (RWCs).
The calculated minimum pre-event water contributions differed up to 60%.
Event water contributions were important during large rainfall events, intense rainfall events and late in the snowmelt season, with maximum event water contributions up to 37% and 46%, depending on the method used for determining the pre-event water composition.
We therefore used two different approaches to quantify diffuse pore water contributions from peatlands to a creek within a small watershed in Southcentral Alaska.
Riparian water contributions were greater at the large catchment size (696 ha) while seep groundwater was important for the small headwater catchments.
Using data from only one rain sampler can result in significant errors in the estimated pre-event water contributions to streamflow.
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Base flow is the ground water contribution to stream flow.
The water contribution was provided by a device simulating short duration rain.
The model includes rainfall, runoff, actual evapotranspiration, water contribution from deeper layers and deep percolation.
Electrical conductivity (EC) was used to estimate water contribution from the two main sub-watersheds.
While the proportion of new or event water was over 50% in wetland dominated catchments, the event water contribution in forested catchments was between 10% and 30%.
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