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  4. Evidence of glacier-permafrost interactions associated with hydro-geomorphological processes and landforms at Snøhetta, Dovrefjell, Norway
 
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Titre

Evidence of glacier-permafrost interactions associated with hydro-geomorphological processes and landforms at Snøhetta, Dovrefjell, Norway

Type
article
Institution
UNIL/CHUV/Unisanté + institutions partenaires
Périodique
Geografiska Annaler: Series A, Physical Geography  
Auteur(s)
Miesen, Floreana
Auteure/Auteur
Dahl, Svein Olaf
Auteure/Auteur
Schrott, Lothar
Auteure/Auteur
Liens vers les personnes
Miesen, Floreana Marie  
Liens vers les unités
Inst. dynamiques surface terre  
ISSN
0435-3676
Statut éditorial
Publié
Date de publication
2021-07-03
Volume
103
Numéro
3
Première page
273
Dernière page/numéro d’article
302
Peer-reviewed
Oui
Langue
anglais
Résumé
Glacier-permafrost interactions are investigated to understand glacial-hydrological influence along a partly glacierised valley on the NE flank of the Snøhetta massif, Dovrefjell, southern Norway. Of particular interest is how processes are controlled by a hydrological connection between landforms. Field mapping identified an ice-marginal landsystem comprising a polythermal glacier, a proglacial lake, an ice-cored moraine complex and a river-lake with perennial frost mounds. A clear interaction between glacial and periglacial processes was observed in transitional landforms, most prominently in the ice-cored moraine which constitutes a permafrost environment that is directly reworked by glaciofluvial processes. The role of this interaction in controlling seasonal, partial drainage of the proglacial lake was assessed using remote sensing-based observations of lake surface size evolution and seasonal surface subsidence. Results suggest a two-fold threshold for lake drainage: Depending on the dynamics of glacial discharge and active layer depth, the ice-cored moraine may either act as a barrier or a pathway to meltwater exiting the glacier. This demonstrates the importance of meltwater dynamics in controlling landform evolution in a glacial-periglacial landscape. To further assess the importance of surface and subsurface hydrology in linking glacial and periglacial domains, water stable oxygen isotope ratios across the study area were studied to map the flow of meltwater from glacier to permafrost. Results include a model of the surface and subsurface hydrology in the catchment and promote a conceptual understanding of water as a thermal, hydraulic and mechanical agent of transient glacier-permafrost interaction operating at heterogeneous timescales.
Sujets

Proglacial hydrology

ice-cored moraines

glacier-permafrost in...

PID Serval
serval:BIB_39A3EC7B9975
DOI
10.1080/04353676.2021.1955539
WOS
000679579000001
Permalien
https://iris.unil.ch/handle/iris/115799
Open Access
Oui
Date de création
2021-08-02T13:59:10.057Z
Date de création dans IRIS
2025-05-20T19:45:57Z
Fichier(s)
En cours de chargement...
Vignette d'image
Nom

Flo_GA_A.pdf

Version du manuscrit

published

Licence

https://creativecommons.org/licenses/by-nc-nd/4.0

Taille

3.23 MB

Format

Adobe PDF

PID Serval

serval:BIB_39A3EC7B9975.P001

URN

urn:nbn:ch:serval-BIB_39A3EC7B99758

Somme de contrôle

(MD5):48fc3039c112adc55ed480560768a9cb

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