Thermal states, responsiveness and degradation of marginal permafrost in Mongolia
Ground thermal conditions in marginal permafrost in Mongolia were assessed using ground temperatures measured year‐round at 69 borehole sites. Permafrost is continuous in northern Mongolia and exists as sporadic/isolated patches in the south. Ground temperatures are strongly controlled by local envi...
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Veröffentlicht in: | Permafrost and periglacial processes 2018-10, Vol.29 (4), p.271-282 |
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Format: | Artikel |
Sprache: | eng |
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