Articles | Volume 15, issue 4
https://doi.org/10.5194/essd-15-1779-2023
https://doi.org/10.5194/essd-15-1779-2023
Data description paper
 | 
24 Apr 2023
Data description paper |  | 24 Apr 2023

Shallow-groundwater-level time series and a groundwater chemistry survey from a boreal headwater catchment, Krycklan, Sweden

Jana Erdbrügger, Ilja van Meerveld, Jan Seibert, and Kevin Bishop

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Cited articles

Bachmair, S., Weiler, M., and Troch, P. A.: Intercomparing hillslope hydrological dynamics: Spatio-temporal variability and vegetation cover effects, Water Resour. Res., 48, 1–18, https://doi.org/10.1029/2011WR011196, 2012. 
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Bishop, K., Seibert, J., Nyberg, L., and Rodhe, A.: Water storage in a till catchment. II: Implications of transmissivity feedback for flow paths and turnover times, Hydrol. Process., 25, 3950–3959, https://doi.org/10.1002/hyp.8355, 2011. 
Bishop, K. H., Grip, H., and O'Neill, A.: The origins of acid runoff in a hillslope during storm events, J. Hydrol., 116, 35–61, Available from: https://doi.org/10.1016/0022-1694(90)90114-D, 1990. 
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Groundwater can respond quickly to precipitation and is the main source of streamflow in most catchments in humid, temperate climates. To better understand shallow groundwater dynamics, we installed a network of groundwater wells in two boreal headwater catchments in Sweden. We recorded groundwater levels in 75 wells for 2 years and sampled the water and analyzed its chemical composition in one summer. This paper describes these datasets.
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