Chris Soulsby

TL;DR: This approach is powerful for assessing whether the dynamic response exhibited here is ubiquitous in other fluvial systems at the terrestrial-aquatic interface or in larger catchments, as demonstrated here for the hydrological year 2003-2004.

TL;DR: In this article, long-term experimental watersheds are used as a crucial evidence base for understanding and managing the provision of clean water supplies, predicting and mitigating the effects of floods, and protecting ecosystem services provided by rivers and wetlands.

TL;DR: In this article, the authors analyzed contributions to run-off using hourly stream water samples from seven individual melt-induced runoff events (plus one rainfall event) during 2011, 2012 and 2013 in two nested glacierized catchments in the Eastern Italian Alps.

TL;DR: In this article, a two-component end-member mixing analysis (EMMA) was used to estimate the contribution of groundwater to annual runoff in upland Scotland, and the results indicated that the contribution varied from 30% to 60% in the smallest (ca 1 km2) peat-dominated headwater catchment with limited groundwater storage, to > 60% with greater coverage of more freely draining soils and more extensive aquifers in alluvium and other drift.

TL;DR: In this paper, a coupled hydrological-biogeochemical model for a northern watershed with organic-rich soils, to simulate daily DOC concentrations was developed, and the relative importance of DOC fluxes from the major landscape units (e.g. hillslopes, groundwater and riparian saturation area) to be determined.