2021
DOI: 10.1111/avsc.12561
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Using floristic gradient mapping to assess seasonal thaw depth in interior Alaska

Abstract: It is a critical part of the global climate system, as it stores nearly twice as much carbon as the atmosphere (Vaughan et al., 2013). Permafrost stability is, however, highly affected by climatic change because its conditions and extent are coupled to surface energy and gas fluxes in the form of surface-atmosphere interactions (Vaughan et al., 2013).

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Cited by 5 publications
(6 citation statements)
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“…The seven papers of this special issue provided themes and examples of patterns in vegetation status and change at very different spatial scales, from extremely detailed to regional spatial scales relying on both unmanned aerial systems (Conti et al, 2021; Malavasi et al, 2021) and ultimately available satellite sensors like Sentinel‐2 (Döpper et al, 2021; Ponce‐Fontenla et al, 2021; Torresani et al, 2021).…”
Section: Figurementioning
confidence: 99%
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“…The seven papers of this special issue provided themes and examples of patterns in vegetation status and change at very different spatial scales, from extremely detailed to regional spatial scales relying on both unmanned aerial systems (Conti et al, 2021; Malavasi et al, 2021) and ultimately available satellite sensors like Sentinel‐2 (Döpper et al, 2021; Ponce‐Fontenla et al, 2021; Torresani et al, 2021).…”
Section: Figurementioning
confidence: 99%
“…The contributions in this special issue encompass studies from different vegetation types, such as grasslands (Conti et al, 2021; Fassnacht et al, 2022), boreal vegetation (Döpper et al, 2021), mixed alpine conifer forests (Torresani et al, 2021), ultramafic rock outcrops (Ponce‐Fontenla et al, 2021) and coastal dune systems (Malavasi et al, 2021), illustrating the usefulness of remote sensing applied to different ecosystems.…”
Section: Figurementioning
confidence: 99%
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“…An important subsurface property, the annual maximum thaw depth to permafrost observed at the end of the summer, is referred to as the active layer thickness (ALT) and is known as a major indication of permafrost degradation (Chen et al 2019). In discontinuous permafrost regions, forest characteristics can be used as indicators of the presence or absence of nearsurface permafrost and its characteristics such as ALT (Viereck 1992, Döpper et al 2021.…”
Section: Introductionmentioning
confidence: 99%