Simulated heat storage in a perennially ice-covered high Arctic lake: Sensitivity to climate change

• Published in: Journal of Geophysical Research
• Main Authors: Vincent, A.C., Mueller, D.R., Vincent, W.F.
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: 2008
• Subjects: Arctic; Ellesmere Island; Arctic Lake; Climate change
• Online Access: https://curve.carleton.ca/67baf1cd-1855-4274-b035-2253e8e11184; https://doi.org/10.1029/2007JC004360; http://onlinelibrary.wiley.com/doi/10.1029/2007JC004360/abstract?systemMessage=Wiley%20Online%20Library%20will%20be%20unavailable%20for%20up%20to%203%20hours%20on%20Saturday%2019th%20March%202016%20from%20%2011%3A00-14%3A00%20GMT%20/%2007%3A00-10%3A00%20EDT%20/%2019%3A00-22%3A00%20SGT%20for%20essential%20maintenance.%20%20Apologies%20for%20the%20inconvenience.

[1] Perennially ice-covered, meromictic lakes occur along the northern coast of Ellesmere Island in the Canadian high Arctic and have distinctive conductivity and temperature profiles. They are salinity stratified and have deep thermal maxima that persist throughout the year at temperatures up to 60°C above the winter minimum in the overlying atmosphere. Heat transfer in one of these lakes (Lake A, latitude 83.0°N, longitude 75.4°W) was simulated using a high spatial resolution model based on a one-dimensional heat diffusion and radiative transfer equation, which was solved through numerical integration. Boundary conditions were forced using climate data from an automated weather station installed next to the lake. There was a good fit between simulated and observed water column temperatures, including the midwater temperature maximum of 8.5°C, after 63 years of heating (RMSE = 0.10°C). This suggests that Lake A became ice-free in the 1940s, a known period of intense warming of the circumpolar Arctic. The model was sensitive to forcing by photosynthetically active radiation (PAR, 400–700 nm), in addition to optically related parameters such as surface reflectance, snow and ice cover, and the PAR diffuse attenuation coefficient. The unusual thermal structure is affected by stratified layers of pigmented microbial communities, which enhance the absorption of solar radiation. Simulation of ice-free summers revealed that the lake's thermal profile would lose its characteristic shape over several decades and that ongoing climate change could reduce the thermal maximum from 8.5° to 4°C within 50 years.