Climatic changes to freshwater ice in the Arctic are projected to produce a variety of effects on hydrologic, ecological, and socio-economic systems. Key hydrologic impacts include changes to low flows, lake evaporation regimes and water levels, and river-ice break-up severity and timing. The latter are of particular concern because of their effect on river geomorphology, vegetation, sediment and nutrient fluxes, and sustainment of riparian aquatic habitats. Changes in ice phenology will affect a wide range of related biological aspects of seasonality. Some changes are likely to be gradual, but others could be more abrupt as systems cross critical ecological thresholds. Trans...
Vast mosaics of lakes, wetlands, and rivers on the Arctic Coastal Plain give the impression of water...
at 68"N have been studied since 1975 to predict physical, chemical and biological impacts of fu...
Lakes and streams in the foothills near Tookik Lake, Alaska, at 68°N have been studied since 1975 to...
Climatic changes to freshwater ice in the Arctic are projected to produce a variety of effects on h...
Freshwater ice dominates the Arctic terrestrial environment and significantly impacts bio-physical ...
In general, the arctic freshwater-terrestrial system will warm more rapidly than the global average,...
Paleolimnological evidence from some Arctic lakes suggests that longer ice-free seasons have been e...
Vast mosaics of lakes, wetlands, and rivers on the Arctic Coastal Plain give the impression of water...
Dramatic changes have been observed in the Arctic over the last century. Many of these involve the s...
Arctic river icings are surface ice accumulations that can be >10 km2 in area and >10 m thick....
Terrestrial hydrology is central to the Arctic system and its freshwater circulation. Water transpor...
Large variations exist in the size, abundance and biota of the two principal categories of freshwate...
The Arctic is considered to be particularly sensitive to global climate change. Global warming will ...
SummaryThis paper investigates patterns of lake-area and hydro-climatic change in Arctic river basin...
Most freshwater aquatic ecosystems have focused on open-water conditions, during spring, summer, and...
Vast mosaics of lakes, wetlands, and rivers on the Arctic Coastal Plain give the impression of water...
at 68"N have been studied since 1975 to predict physical, chemical and biological impacts of fu...
Lakes and streams in the foothills near Tookik Lake, Alaska, at 68°N have been studied since 1975 to...
Climatic changes to freshwater ice in the Arctic are projected to produce a variety of effects on h...
Freshwater ice dominates the Arctic terrestrial environment and significantly impacts bio-physical ...
In general, the arctic freshwater-terrestrial system will warm more rapidly than the global average,...
Paleolimnological evidence from some Arctic lakes suggests that longer ice-free seasons have been e...
Vast mosaics of lakes, wetlands, and rivers on the Arctic Coastal Plain give the impression of water...
Dramatic changes have been observed in the Arctic over the last century. Many of these involve the s...
Arctic river icings are surface ice accumulations that can be >10 km2 in area and >10 m thick....
Terrestrial hydrology is central to the Arctic system and its freshwater circulation. Water transpor...
Large variations exist in the size, abundance and biota of the two principal categories of freshwate...
The Arctic is considered to be particularly sensitive to global climate change. Global warming will ...
SummaryThis paper investigates patterns of lake-area and hydro-climatic change in Arctic river basin...
Most freshwater aquatic ecosystems have focused on open-water conditions, during spring, summer, and...
Vast mosaics of lakes, wetlands, and rivers on the Arctic Coastal Plain give the impression of water...
at 68"N have been studied since 1975 to predict physical, chemical and biological impacts of fu...
Lakes and streams in the foothills near Tookik Lake, Alaska, at 68°N have been studied since 1975 to...