Expansion rate and geometry of floating vegetation mats on the margins of thermokarst lakes, northern Seward Peninsula, Alaska, USA

• Published in: Earth Surface Processes and Landforms
• Main Authors: Parsekian, Andrew D., Jones, Benjamin M., Jones, Miriam, Grosse, Guido, Walter Anthony, Katey M., Slater, Lee
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2011
• Subjects: permafrost; Seward Peninsula; Thermokarst; Alaska
• Online Access: http://dx.doi.org/10.1002/esp.2210; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fesp.2210; https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.2210; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/esp.2210

ABSTRACT Investigations on the northern Seward Peninsula in Alaska identified zones of recent (<50 years) permafrost collapse that led to the formation of floating vegetation mats along thermokarst lake margins. The occurrence of floating vegetation mat features indicates rapid degradation of near‐surface permafrost and lake expansion. This paper reports on the recent expansion of these collapse features and their geometry is determined using geophysical and remote sensing measurements. The vegetation mats were observed to have an average thickness of 0.57 m and petrophysical modeling indicated that gas content of 1.5–5% enabled floatation above the lake surface. Furthermore, geophysical investigation provides evidence that the mats form by thaw and subsidence of the underlying permafrost rather than terrestrialization. The temperature of the water below a vegetation mat was observed to remain above freezing late in the winter. Analysis of satellite and aerial imagery indicates that these features have expanded at maximum rates of 1–2 m yr ‐1 over a 56 year period. Including the spatial coverage of floating ‘thermokarst mats’ increases estimates of lake area by as much as 4% in some lakes. Copyright © 2011 John Wiley & Sons, Ltd.