Thermokarst Lakes on the Arctic Coastal Plain of Alaska: Spatial and Temporal Variability in Summer Water Temperature

ABSTRACT In summer 2010, water temperature profile measurements were made in 12 thermokarst lakes along a 150‐km long north–south transect across the Arctic Coastal Plain of northern Alaska. In shallow lakes, gradual warming of the water column to 1–4°C begins at the lake bed during decay of the ice...

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Bibliographic Details
Published in:Permafrost and Periglacial Processes
Main Authors: Hinkel, Kenneth M., Lenters, John D., Sheng, Yongwei, Lyons, Evan A., Beck, Richard A., Eisner, Wendy R., Maurer, Eric F., Wang, Jida, Potter, Brittany L.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2012
Subjects:
Arctic
Impact Lake
Permafrost and Periglacial Processes
Thermokarst
Alaska
Online Access:http://dx.doi.org/10.1002/ppp.1743
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.1743
https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.1743
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Summary:ABSTRACT In summer 2010, water temperature profile measurements were made in 12 thermokarst lakes along a 150‐km long north–south transect across the Arctic Coastal Plain of northern Alaska. In shallow lakes, gradual warming of the water column to 1–4°C begins at the lake bed during decay of the ice cover in spring. Rapid warming follows ice‐off, with water temperature responding synchronously to synoptic weather variations across the area. Regionally, ice‐off occurs 2–4 weeks later on lakes near the coast. Inland lakes are warmer (13°C) in mid‐summer than those near the coast (7°C), reflecting the regional climate gradient and the maritime effect. All lakes are well mixed and largely isothermal, with some thermal stratification (< 2°C) occurring during calm, sunny periods in deeper lakes. In deep (6–9 m) lake‐bed depressions that are likely ice‐wedge troughs, water cools by conduction to the colder sediments below, while concurrent warming occurs in the upper water column. A spatially dense sample of near‐surface temperature measurements was collected from one lake over a short period and shows warmer (2–3°C) temperatures on the upwind, sheltered end of the lake. This study demonstrates that climatic gradients, meteorological conditions and basin characteristics impact lake temperature dynamics. Copyright © 2012 John Wiley & Sons, Ltd.

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