The separation of storm hydrographs using stable isotope tracers dates back to the late
1960s. These studies ushered in a paradigm shift in how hydrologists conceptualized runoff …

In spite of trying to understand processes in the same spatial domain, the catchment
hydrology and water quality scientific communities are relatively disconnected and so are …

Water fluxes in catchments are controlled by physical processes and material properties that
are complex, heterogeneous, and poorly characterized by direct measurement. As a result …

We bring together three decades of research from a boreal catchment to facilitate an
improved mechanistic understanding of surface water dissolved organic carbon (DOC) …

The shallow and deep hypothesis suggests that stream concentration‐discharge (CQ)
relationships are shaped by distinct source waters from different depths. Under this …

The Pacific Northwest encompasses a range of hydrologic regimes that can be broadly
characterized as either coastal (where rain and rain on snow are dominant) or interior …

We examine how tracer studies have enhanced our understanding of flow paths, residence
times and sources of stream flow in northern catchments. We define northern catchments as …

The riparian zone, the last few metres of soil through which water flows before entering a
gaining stream, has been identified as a first order control on key aspects of stream water …

The regulation of the spatial and seasonal variation in terrestrial dissolved organic carbon
(DOC) exports was studied in a 68 km2 boreal stream system in northern Sweden. A total of …

The effect of catchment scale and the influence of landscape characteristics on runoff
generation were investigated during snow melt in 15 nested boreal streams within the …