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Late summer thaw (cm) |
|
Map |
Site |
Location |
Method |
'90 |
'91 |
'92 |
'93 |
'94 |
'95 |
'96 |
'97 |
'98 |
'99 | 2000 | '01 |
United States (Alaska) |
|
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Ivotuk (Sphag) |
68 29' N |
100 |
- |
- |
- |
- |
- |
- |
- |
- |
57 |
50 |
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Ivotuk (MAT) |
68 29' N |
100 |
- |
- |
- |
- |
- |
- |
- |
- |
61 |
49 |
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U26C | Ivotuk |
68 29' N
155 44' W |
1000 |
- | - | - | - | - | - | - | - | - | - | 55 |
LEGEND
Methods: 2-4 digit numbers refer to size of grid in meters (10,100,1000); Some sites have a combination of methods; P = single point probe or multiple points along transect; TT = thaw tube; T = interpolated thaw depth based on temperature profile, generally obtained by data logger, accuracy = +/- 10 cm; B = nearest borehole, number is depth in m. tba = data being processed; I = Inactive.
Data: dash (-) = site not yet established; * = no data collected from site that year; # = Russian 1000-m grids in 1997 only; all other data from 100-m grids. [ ] = Canadian sites with 100-m grids; For sites with boreholes >2m, interpolated thaw reported in 0.1 m
Data compiled by Jerry Brown and Ken Hinkel