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Seasonal InSAR Displacements Documenting the Active Layer Freeze and Thaw Progression in Central-Western Spitsbergen, Svalbard

In permafrost areas, the active layer undergoes seasonal frost heave and thaw subsidence caused by ice formation and melting. The amplitude and timing of the ground displacement cycles depend on the climatic and ground conditions. Here we used Sentinel-1 Synthetic Aperture Radar Interferometry (InSA...

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Gorde:
Xehetasun bibliografikoak
Egile Nagusiak: Line Rouyet, Lin Liu, Sarah Marie Strand, Hanne Hvidtfeldt Christiansen, Tom Rune Lauknes, Yngvar Larsen
Formatua: Artigo
Hizkuntza:Inglês
Argitaratua: MDPI AG 2021-07-01
Saila:Remote Sensing
Gaiak:
Sarrera elektronikoa:https://www.mdpi.com/2072-4292/13/15/2977
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