Articles | Volume 14, issue 4
https://doi.org/10.5194/tc-14-1437-2020
https://doi.org/10.5194/tc-14-1437-2020
Research article
 | 
30 Apr 2020
Research article |  | 30 Apr 2020

Ground subsidence and heave over permafrost: hourly time series reveal interannual, seasonal and shorter-term movement caused by freezing, thawing and water movement

Stephan Gruber

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Cited articles

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Arenson, L. U., Kääb, A., and O'Sullivan, A.: Detection and analysis of ground deformation in permafrost environments, Permafrost Periglac., 27, 339–351, https://doi.org/10.1002/ppp.1932, 2016. a
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Government of Canada: Yellowknife A, daily data reports, available at: http://climate.weather.gc.ca/climate_data/daily_data_e.html?StationID=51058 (last access: 21 July 2019), 2019. a
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Short summary
A simple method to record heave and subsidence of the land surface at specific field locations is described. Hourly observations from three sites, over two winters and one summer, are analyzed and discussed. The data are rich in features that point to the influence of freezing and thawing and of wetting and drying of the soil. This type of observation may offer new insight into the processes of heat and mass transfer in soil and help to monitor climate change impacts.