Threshold sensitivity of shallow Arctic lakes and sublake permafrost to changing winter climate. Issue 12 (24th June 2016)

• Record Type: Journal Article
• Authors: Arp, Christopher D.; Jones, Benjamin M.; Grosse, Guido; Bondurant, Allen C.; Romanovsky, Vladimir E.; Hinkel, Kenneth M.; Parsekian, Andrew D.
• Is Part Of: Geophysical research letters. Volume 43:Issue 12(2016)
• Page Start: 6358
• Page End: 6365
• Publication Date: 2016-06-24
• Subjects: thermokarst lakes -- permafrost -- lake ice -- taliks -- climate change; Geophysics -- Periodicals; Planets -- Periodicals; Lunar geology -- Periodicals; 550
• DOI: 10.1002/2016GL068506
• Languages: English
• ISSNs: 0094-8276

Abstract

Abstract: Interactions and feedbacks between abundant surface waters and permafrost fundamentally shape lowland Arctic landscapes. Sublake permafrost is maintained when the maximum ice thickness (MIT) exceeds lake depth and mean annual bed temperatures (MABTs) remain below freezing. However, declining MIT since the 1970s is likely causing talik development below shallow lakes. Here we show high‐temperature sensitivity to winter ice growth at the water‐sediment interface of shallow lakes based on year‐round lake sensor data. Empirical model experiments suggest that shallow (1 m depth) lakes have warmed substantially over the last 30 years (2.4°C), with MABT above freezing 5 of the last 7 years. This is in comparison to slower rates of warming in deeper (3 m) lakes (0.9°C), with already well‐developed taliks. Our findings indicate that permafrost below shallow lakes has already begun crossing a critical thawing threshold approximately 70 years prior to predicted terrestrial permafrost thaw in northern Alaska. Key Points: Thermal controls on lake beds vary between ice‐ and open‐water periods Maximum ice thickness relative to lake depth is the major control on bed temperature Permafrost below shallow lakes is sensitive to thaw because of winter climate change