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Data Publisher for Earth & Environmental Science

Sannel, A Britta K; Kuhry, Peter (2011): (Table 3) Changes in thermokarst lake extent, infilling with fen vegetation and lateral erosion at study sites in Canada, Russia and Sweden [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.834902, In supplement to: Sannel, ABK; Kuhry, P (2011): Warming-induced destabilization of peat plateau/thermokarst lake complexes. Journal of Geophysical Research, 116(G3), G03035, https://doi.org/10.1029/2010JG001635

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Coverage:
Median Latitude: 64.538900 * Median Longitude: -3.711133 * South-bound Latitude: 57.883300 * West-bound Longitude: -94.166700 * North-bound Latitude: 68.466700 * East-bound Longitude: 62.133300
Minimum Elevation: 77.0 m * Maximum Elevation: 550.0 m
Event(s):
HudsonBay_lowl * Latitude: 57.883300 * Longitude: -94.166700 * Elevation: 80.0 m * Location: Manitoba, Canada * Method/Device: Monitoring (MON)
Rogovaya * Latitude: 67.266700 * Longitude: 62.133300 * Elevation: 77.0 m * Location: Usa River basin, Northeast European Russia * Method/Device: Monitoring (MON)
Tavvavuoma * Latitude: 68.466700 * Longitude: 20.900000 * Elevation: 550.0 m * Location: Sweden * Method/Device: Monitoring (MON)
Comment:
Thermokarst lakes = surrounded by peat plateau along >75% of the shoreline. For all study sites the changes in lake area were statistically significant (p < 0.001), except for in the 2 km × 2 km area in Rogovaya (p = 0.63). Here, it could not be calculated as fen vegetation was difficult to identify in the aerial photographs.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Area/localityAreaSannel, A Britta KAerial photography and satellite imagery
2Latitude of eventLatitude
3Longitude of eventLongitude
4ResolutionResolutionSannel, A Britta KAerial photography and satellite imagery
5Time coverageCoverageSannel, A Britta KAerial photography and satellite imagery
6ChangeChangem2Sannel, A Britta KAerial photography and satellite imageryin thermokarst lake area
7Confidence intervalCISannel, A Britta KAerial photography and satellite imagerylower, 95%, area change in m**2
8Confidence intervalCISannel, A Britta KAerial photography and satellite imageryupper, 95%, area change in m**2
9ChangeChange%Sannel, A Britta KAerial photography and satellite imageryper decade in thermokarst lake area
10ChangeChangem2Sannel, A Britta KAerial photography and satellite imageryof infilling with fen vegetation
11Confidence intervalCISannel, A Britta KAerial photography and satellite imagerylower, 100%, fen vegetation change in m**2
12Confidence intervalCISannel, A Britta KAerial photography and satellite imageryupper, 100%, fen vegetation change in m**2
13ChangeChange%Sannel, A Britta KAerial photography and satellite imageryper decade in fen vegetation infilling
14--Sannel, A Britta KAerial photography and satellite imageryMax infilling rate in m/decade
15CommentCommentSannel, A Britta KAerial photography and satellite imagerymax infilling rate
16AreaAream2Sannel, A Britta KAerial photography and satellite imageryof lateral erosion (excluding newly formed lakes)
17Confidence intervalCISannel, A Britta KAerial photography and satellite imagerylower, 100%, lateral erosion in m**2
18Confidence intervalCISannel, A Britta KAerial photography and satellite imageryupper, 100%, lateral erosion in m**2
19ChangeChange%Sannel, A Britta KAerial photography and satellite imageryper decade in lateral erosion
20--Sannel, A Britta KAerial photography and satellite imageryMax erosion rate in m/decade; # = For a new pond that formed between 1975 and 2003
21CommentCommentSannel, A Britta KAerial photography and satellite imagerygeneral
Size:
180 data points

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