Besides climate change impacts on water availability and hydrological risks, the
consequences on water quality is just beginning to be studied. This review aims at …

The retention of peatland carbon (C) and the ability to continue to draw down and store C
from the atmosphere is not only important for the UK terrestrial carbon inventory, but also for …

Concentrations of dissolved organic carbon have increased in many, but not all, surface
waters across acid impacted areas of Europe and North America over the last two decades …

Dissolved organic carbon (DOC) exports from many catchments in Europe and North-
America are steadily increasing. Several studies have sought to explain this observation. As …

Peatland water table depth is an important control on runoff production, plant growth and
carbon cycling. Many peatlands have been drained but are now subject to activities that …

Surface-water quality can change in response to climate perturbations, such as changes in
the frequency of heavy precipitation or droughts, through direct effects, such as dilution and …

Boreal peatlands are major sources of nitrogen (N), phosphorus (P) and dissolved organic
carbon (DOC) to downstream aquatic ecosystems, and forest harvesting generally further …

Extreme precipitation and flooding frequency associated with global climate change are
expected to increase worldwide, with major consequences in floodplains and areas …

At the global scale, inland waters are a significant source of atmospheric carbon (C),
particularly in the tropics. The active pipe concept predicts that C emissions from streams …

Large rivers transport a significant amount of terrestrially derived dissolved organic matter
(DOM) to coastal oceans, consisting of a critical component of the global biogeochemical …