The fate of lake ice in the North American Arctic

Abstract

Abstract. Lakes comprise a large portion of the surface cover in northern North America, forming an important part of the cryosphere. The timing of lake ice phenological events (e.g. break-up/freeze-up) is a useful indicator of climate variability and change, which is of particular relevance in environmentally sensitive areas such as the North American Arctic. Further alterations to the present day ice regime could result in major ecosystem changes, such as species shifts and the disappearance of perennial ice cover. The Canadian Lake Ice Model (CLIMo) was used to simulate lake ice phenology across the North American Arctic from 1961-2100 using two climate scenarios produced by the Canadian Regional Climate Model (CRCM). Results from the 1961-1990 time period were validated using 15 locations across the Canadian Arctic, with both in situ ice cover observations from the Canadian Ice Database as well as additional ice cover simulations using nearby weather station data. Projected changes to the ice cover using the 30-year mean data between 1961-1990 and 2041-2070 suggest a shift in break-up and freeze-up dates for most areas ranging from 10-25 days earlier (break-up) and 0-15 days later (freeze-up). The resulting ice cover durations show mainly a 10-25 day reduction for the shallower lakes (3 and 10 m) and 10-30 day reduction for the deeper lakes (30 m). More extreme reductions of up to 60 days (excluding the loss of perennial ice cover) were shown in the coastal regions compared to the interior continental areas. The mean maximum ice thickness was shown to decrease by 10-60 cm with no snow cover and 5-50 cm with snow cover on the ice. Snow ice was also shown to increase through most of the study area with the exception of the Alaskan coastal areas.

Oxygen depletion in subarctic peatland thaw lakes

“…For example, ice and snow thickness control the availability of light to phytoplankton and thereby affect autotrophic biomass and oxygen production (Vincent et al 2013). The melting of snow and ice represents a positive feedback loop for warming, with modelling predictions generally showing earlier ice break-up dates and later freezeup dates for lakes in the North American Arctic (Graversen et al 2008;Brown and Duguay 2011). Analysis of multiple data sets has revealed a continuous and substantial reduction in spring snow cover extent over a 30 year period throughout the Arctic (Brown et al 2010), and the predicted shift towards a rainfall-dominated precipitation regime later this century will accelerate ice-melt and landscape erosion .…”

Variability and change in the Canadian cryosphere

“…Callaghan et al 2011;Francis et al 2009;Furgal and Prowse 2008;Lemke et al 2007;Rawlins et al 2010;Walsh et al 2005). These include declines in Arctic sea ice extent (Tivy et al 2011a;Stroeve et al 2011), mass loss from glaciers and ice caps (Gardner et al 2011;Rignot et al 2008), decreases in spring snow cover extent and duration , later freeze-up and earlier break-up of rivers and lakes Brown and Duguay 2011), and warming of permafrost (Romanovsky et al 2010).…”

Some Aspects of Ice-Hydropower Interaction in a Changing Climate

“…There is especially sparse literature on river studies. Large scale studies conducted on lakes project a general decrease in the ice cover duration and ice thickness due to changes in climate [22][23][24][25]. Few studies using detailed numerical modeling conducted on rivers also depicted reduction in the duration and extent of ice cover [26,27].…”