Evidences of Permafrost Signatures in the Planform Shape of Arctic Meandering Streams

Abstract We investigate whether geomorphic signatures of permafrost are embedded in planforms of river meanders, and we inquire as to how physical factors unique to permafrost environments are able to affect their dynamics. By exploiting satellite imagery, a data set of 19 freely‐meandering Arctic r...

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Published in:Geophysical Research Letters
Main Authors: Niccolò Ragno, Riccardo Bonanomi, Marta Crivellaro, Marco Tubino
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2024
Subjects:
Online Access:https://doi.org/10.1029/2024GL109410
https://doaj.org/article/a7fdafdf14724ae6b62df13e7a517ceb
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spelling ftdoajarticles:oai:doaj.org/article:a7fdafdf14724ae6b62df13e7a517ceb 2024-09-30T14:30:19+00:00 Evidences of Permafrost Signatures in the Planform Shape of Arctic Meandering Streams Niccolò Ragno Riccardo Bonanomi Marta Crivellaro Marco Tubino 2024-09-01T00:00:00Z https://doi.org/10.1029/2024GL109410 https://doaj.org/article/a7fdafdf14724ae6b62df13e7a517ceb EN eng Wiley https://doi.org/10.1029/2024GL109410 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2024GL109410 https://doaj.org/article/a7fdafdf14724ae6b62df13e7a517ceb Geophysical Research Letters, Vol 51, Iss 17, Pp n/a-n/a (2024) morphodynamics meandering permafrost remote sensing Geophysics. Cosmic physics QC801-809 article 2024 ftdoajarticles https://doi.org/10.1029/2024GL109410 2024-09-17T16:00:46Z Abstract We investigate whether geomorphic signatures of permafrost are embedded in planforms of river meanders, and we inquire as to how physical factors unique to permafrost environments are able to affect their dynamics. By exploiting satellite imagery, a data set of 19 freely‐meandering Arctic rivers is compared against an independent data set of 23 freely‐meandering streams flowing through temperate and tropical regions. Suitable dimensionless metrics are defined to characterize morphometric properties of meanders in terms of the spatio‐temporal distribution of curvature and channel width. Results show the absence of marked contrasts in the amplitude of bend‐curvature between the two data set. Differently, we find a permafrost signature in the channel width response, which manifests itself through larger values of the average bend‐width and by peaks of width fluctuations. Field data suggest that permafrost meanders tend to widen for increasing bend sinuosity, likely promoting a shift of their morphodynamic regime as final cutoff is approached. Article in Journal/Newspaper Arctic permafrost Directory of Open Access Journals: DOAJ Articles Arctic Geophysical Research Letters 51 17
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic morphodynamics
meandering
permafrost
remote sensing
Geophysics. Cosmic physics
QC801-809
spellingShingle morphodynamics
meandering
permafrost
remote sensing
Geophysics. Cosmic physics
QC801-809
Niccolò Ragno
Riccardo Bonanomi
Marta Crivellaro
Marco Tubino
Evidences of Permafrost Signatures in the Planform Shape of Arctic Meandering Streams
topic_facet morphodynamics
meandering
permafrost
remote sensing
Geophysics. Cosmic physics
QC801-809
description Abstract We investigate whether geomorphic signatures of permafrost are embedded in planforms of river meanders, and we inquire as to how physical factors unique to permafrost environments are able to affect their dynamics. By exploiting satellite imagery, a data set of 19 freely‐meandering Arctic rivers is compared against an independent data set of 23 freely‐meandering streams flowing through temperate and tropical regions. Suitable dimensionless metrics are defined to characterize morphometric properties of meanders in terms of the spatio‐temporal distribution of curvature and channel width. Results show the absence of marked contrasts in the amplitude of bend‐curvature between the two data set. Differently, we find a permafrost signature in the channel width response, which manifests itself through larger values of the average bend‐width and by peaks of width fluctuations. Field data suggest that permafrost meanders tend to widen for increasing bend sinuosity, likely promoting a shift of their morphodynamic regime as final cutoff is approached.
format Article in Journal/Newspaper
author Niccolò Ragno
Riccardo Bonanomi
Marta Crivellaro
Marco Tubino
author_facet Niccolò Ragno
Riccardo Bonanomi
Marta Crivellaro
Marco Tubino
author_sort Niccolò Ragno
title Evidences of Permafrost Signatures in the Planform Shape of Arctic Meandering Streams
title_short Evidences of Permafrost Signatures in the Planform Shape of Arctic Meandering Streams
title_full Evidences of Permafrost Signatures in the Planform Shape of Arctic Meandering Streams
title_fullStr Evidences of Permafrost Signatures in the Planform Shape of Arctic Meandering Streams
title_full_unstemmed Evidences of Permafrost Signatures in the Planform Shape of Arctic Meandering Streams
title_sort evidences of permafrost signatures in the planform shape of arctic meandering streams
publisher Wiley
publishDate 2024
url https://doi.org/10.1029/2024GL109410
https://doaj.org/article/a7fdafdf14724ae6b62df13e7a517ceb
geographic Arctic
geographic_facet Arctic
genre Arctic
permafrost
genre_facet Arctic
permafrost
op_source Geophysical Research Letters, Vol 51, Iss 17, Pp n/a-n/a (2024)
op_relation https://doi.org/10.1029/2024GL109410
https://doaj.org/toc/0094-8276
https://doaj.org/toc/1944-8007
1944-8007
0094-8276
doi:10.1029/2024GL109410
https://doaj.org/article/a7fdafdf14724ae6b62df13e7a517ceb
op_doi https://doi.org/10.1029/2024GL109410
container_title Geophysical Research Letters
container_volume 51
container_issue 17
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