The Use of the Value of Heat Cycle to Assess the Energy Stability of Permafrost Soils at the Change of Conditions on the Surface
The basis for assessing the stability of geosystems to changes in external heat cycle conditions is the calculation method. It is shown that permafrost soils are characterized by increased values of annual heat cycle QY ≥ 300 MJ/m2, i.e., half-sum of heat arrival and flow rate per year. This...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
MDPI AG
2019-03-01
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| Series: | Geosciences |
| Subjects: | |
| Online Access: | http://www.mdpi.com/2076-3263/9/3/112 |