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Long-Term Active Layer and Ground Surface Temperature Trends: Results of Observations at Alaskan CALM Sites Nikolai Shiklomanov, University of Delaware.

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Presentation on theme: "Long-Term Active Layer and Ground Surface Temperature Trends: Results of Observations at Alaskan CALM Sites Nikolai Shiklomanov, University of Delaware."— Presentation transcript:

1 Long-Term Active Layer and Ground Surface Temperature Trends: Results of Observations at Alaskan CALM Sites Nikolai Shiklomanov, University of Delaware

2 CIRCUMPOLAR ACTIVE-LAYER MONITORING (CALM) NETWORK

3 Ground Surface Temperature Thaw depth Frost Heave / Thaw Subsidence CALM Observations

4 CALM Sampling Strategy

5 Active Layer Trends for Characteristic North Slope Landscapes

6 North SlopeInterior

7 Seasonal Progression of Thaw Depth

8 Trends of Air and Ground Temperatures within Bioclimatic Zones

9 The Length of Thawing Period at the Ground Surface within Bioclimatic Zones

10 Detection of Frost Heave and Thaw Settlement within Representative Landscapes. Use of high-precision Differential Global Positioning System (DGPS) technology. Three primary locations representative of main physiographic provinces. Spatially-oriented observations at various characteristic landscapes. 36 observational points in each landscape unit. Observations were initiated in 2001 and were conducted twice a year (June and August).

11 TRANSITION LAYER (TL) TL Transition Layer – boundary layer (0.1–2.0 m) between the active layer and permanently frozen part of permafrost. Shur Y.L., 1988

12 Thaw Settlement within Representative Landscapes.

13 R 2 =0.63 R 2 =0.91 ALT vs (ALT is as measured by metal probe) ALT vs (ALT is corrected for ground subsidence)

14

15 Thank you


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