Tracking coarse sediment in an Alpine subglacial channel using radio-tagged particles

Détails

Ressource 1Télécharger: tracking-coarse-sediment-in-an-alpine-subglacial-channel-using-radio-tagged-particles.pdf (5586.33 [Ko])
Etat: Public
Version: Final published version
Licence: CC BY-NC-ND 4.0
ID Serval
serval:BIB_9439BA7B0CCD
Type
Article: article d'un périodique ou d'un magazine.
Collection
Publications
Institution
Titre
Tracking coarse sediment in an Alpine subglacial channel using radio-tagged particles
Périodique
Journal of Glaciology
Auteur⸱e⸱s
Jenkin Matt, Hofmann Margaux, Hubbard Bryn, Mancini Davide, Miesen Floreana M., Herman Frédéric, Lane Stuart N.
ISSN
0022-1430
1727-5652
Statut éditorial
Publié
Date de publication
09/10/2023
Peer-reviewed
Oui
Pages
1-15
Langue
anglais
Résumé
We present a method for tracking radio-tagged pebbles and cobbles through subglacial meltwater channels under shallow temperate glaciers. Natural particles tagged with active radio transmitters were injected directly into a large subglacial channel 300 m up-glacier from the terminus of the Glacier d'Otemma, Switzerland. A roving antenna was developed to localise tagged particles planimetrically in subglacial and proglacial channel reaches (350 and 150 m long, respectively) using a probabilistic technique, delivering records of the change in particle location and transport distance over time with uncertainty. The roving antenna had a ±5−15 m planimetric precision, a 75% particle localisation rate and operated at a maximum ice depth of 47 m. Additionally, stationary supraglacial and proglacial antennas continuously monitored the passage of tagged particles through consecutive reaches of the channel, constraining the timing of particle transport events. The proglacial antenna system had a 98.1% detection rate and was operational to 0.89 m water depth during testing. Roving and stationary antenna records were combined to create a transport distance model for each particle, which may be used in conjunction with hydraulic data to investigate the kinematics of particle motion. When applied at scale in future studies, this method may be used to reveal the mechanisms and timescales of coarse sediment export from Alpine glaciers.
Mots-clé
glaciological instruments and methods, subglacial sediments, subglacial processes
Web of science
Open Access
Oui
Financement(s)
Fonds national suisse / 188734
Création de la notice
25/11/2024 13:08
Dernière modification de la notice
06/12/2024 7:15
Données d'usage