Terrestrial hydrology is central to the Arctic system and its freshwater circulation. Water
transport and water constituents vary, however, across a very diverse geography. In this …

Numerous international scientific assessments and related articles have, during the last
decade, described the observed and potential impacts of climate change as well as other …

Many observations in and model simulations for northern basins have confirmed an
increased streamflow from degrading permafrost, while the streamflow has declined in the …

Large Arctic river basins experience substantial variability in climatic, landscape, and
permafrost conditions. However, the processes behind the observed changes at the scale of …

Climatic changes can profoundly alter hydrological conditions in river basins. Lake Baikal is
the deepest and largest freshwater reservoir on Earth, and has a unique ecosystem with …

Numerous components of the Arctic freshwater system (atmosphere, ocean, cryosphere, and
terrestrial hydrology) have experienced large changes over the past few decades, and these …

The long-term relationship between temperature and hydroclimate has remained uncertain
due to the short length of instrumental measurements and inconsistent results from climate …

The Arctic freshwater cycle is changing rapidly, which will require adequate monitoring of
river flows to detect, observe, and understand changes and provide adaptation information …

As environmental change in the Arctic accelerates, there is a growing need to accurately
quantify the response of Arctic ecosystems throughout the year. To assess the temporal …

The Arctic faces many environmental challenges, including the continued exploitation of its
mineral resources such as nickel (Ni). The responsible development of Ni mining in the …