A land process model [the coupled hydrological and biogeochemical model (CHANGE)] is used to quantitatively assess changes in the ice phenology, thickness, and volume of terrestrial Arctic rivers from 1979 to 2009. The CHANGE model was coupled with a river routing and discharge model enabling explicit representation of river ice and water temperature dynamics. Model-simulated river ice phenological dates and thickness were generally consistent with in situ river ice data and landscape freeze–thaw (FT) satellite observations. Climate data indicated an increasing trend in winter surface air temperature (SAT) over the pan-Arctic during the study period. Nevertheless, the river ice thickness simulations exhibited a thickening regional trend ind...
Paleolimnological evidence from some Arctic lakes suggests that longer ice-free seasons have been e...
With permafrost warming, the observed discharge of the Kolyma River in northeastern Siberia decrease...
The Arctic has warmed rapidly, increasing shrub cover and density, and thawing permafrost. Understan...
A land process model [the coupled hydrological and biogeochemical model (CHANGE)] is used to quantit...
Predicting the future changes in river ice development and impacts on seasonal sediment transport re...
Predicting the future changes in river ice development and impacts on seasonal sediment transport re...
The Arctic is considered to be particularly sensitive to global climate change. Global warming will ...
This paper looks at the response of river ice to recent warming in the Arctic at six major downstrea...
Since the 1980s, the Arctic has experienced an amplified warming of more than twice the rate of the ...
Arctic river icings are surface ice accumulations that can be >10 km2 in area and >10 m thick....
Over the recent decades, the warming in Arctic has affected changes in the terrestrial hydrologic pr...
Arctic rivers drain ~15% of the global land surface and significantly influence local communities an...
More than one-third of Earth’s landmass is drained by rivers that seasonally freeze over. Ice transf...
The dramatic decline in Arctic sea ice cover is anticipated to influence atmospheric temperatures an...
AbstractThe dramatic decline in Arctic sea ice cover is anticipated to influence atmospheric tempera...
Paleolimnological evidence from some Arctic lakes suggests that longer ice-free seasons have been e...
With permafrost warming, the observed discharge of the Kolyma River in northeastern Siberia decrease...
The Arctic has warmed rapidly, increasing shrub cover and density, and thawing permafrost. Understan...
A land process model [the coupled hydrological and biogeochemical model (CHANGE)] is used to quantit...
Predicting the future changes in river ice development and impacts on seasonal sediment transport re...
Predicting the future changes in river ice development and impacts on seasonal sediment transport re...
The Arctic is considered to be particularly sensitive to global climate change. Global warming will ...
This paper looks at the response of river ice to recent warming in the Arctic at six major downstrea...
Since the 1980s, the Arctic has experienced an amplified warming of more than twice the rate of the ...
Arctic river icings are surface ice accumulations that can be >10 km2 in area and >10 m thick....
Over the recent decades, the warming in Arctic has affected changes in the terrestrial hydrologic pr...
Arctic rivers drain ~15% of the global land surface and significantly influence local communities an...
More than one-third of Earth’s landmass is drained by rivers that seasonally freeze over. Ice transf...
The dramatic decline in Arctic sea ice cover is anticipated to influence atmospheric temperatures an...
AbstractThe dramatic decline in Arctic sea ice cover is anticipated to influence atmospheric tempera...
Paleolimnological evidence from some Arctic lakes suggests that longer ice-free seasons have been e...
With permafrost warming, the observed discharge of the Kolyma River in northeastern Siberia decrease...
The Arctic has warmed rapidly, increasing shrub cover and density, and thawing permafrost. Understan...