Characterising englacial R-channels using artificial moulins

The englacial and subglacial drainage systems exert key controls on glacier dynamics. However, due to their inaccessibility, they are still only poorly understood and more detailed observations are important, particularly to validate and tune physical models describing their dynamics. By creating ar...

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Main Authors: Pohle, Annegret, id_orcid:0 000-0002-0986-5778, Werder, Mauro, id_orcid:0 000-0003-0137-9377, Gräff, Dominik, id_orcid:0 000-0003-1642-4783, Farinotti, Daniel, id_orcid:0 000-0003-3417-4570
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2022
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/537322
https://doi.org/10.3929/ethz-b-000537322
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author Pohle, Annegret
id_orcid:0 000-0002-0986-5778
Werder, Mauro
id_orcid:0 000-0003-0137-9377
Gräff, Dominik
id_orcid:0 000-0003-1642-4783
Farinotti, Daniel
id_orcid:0 000-0003-3417-4570
author_facet Pohle, Annegret
id_orcid:0 000-0002-0986-5778
Werder, Mauro
id_orcid:0 000-0003-0137-9377
Gräff, Dominik
id_orcid:0 000-0003-1642-4783
Farinotti, Daniel
id_orcid:0 000-0003-3417-4570
author_sort Pohle, Annegret
collection ETH Zürich Research Collection
description The englacial and subglacial drainage systems exert key controls on glacier dynamics. However, due to their inaccessibility, they are still only poorly understood and more detailed observations are important, particularly to validate and tune physical models describing their dynamics. By creating artificial glacier moulins – boreholes connected to the subglacial drainage system and supplied with water from surface streams – we present a novel method to monitor the evolution of an englacial hydrological system with high temporal resolution. Here, we use artificial moulins as representations for vertical, pressurised, englacial R-channels. From tracer and pressure measurements, we derive time series of the hydraulic gradient, discharge, flow speed and channel cross-sectional area. Using these, we compute the Darcy–Weisbach friction factor, obtaining values which increase from 0.1 to 13 within five days of channel evolution. Furthermore, we simulate the growth of the cross-sectional area using different temperature gradients. The comparison to our measurements largely supports the common assumption that the temperature follows the pressure melting point. The deviations from this behaviour are analysed using various heat transfer parameterisations to assess their applicability. Finally, we discuss how artificial moulins could be combined with glacier-wide tracer experiments to constrain parameters of subglacial drainage more precisely. ISSN:0022-1430 ISSN:1727-5652
format Article in Journal/Newspaper
genre Journal of Glaciology
genre_facet Journal of Glaciology
id ftethz:oai:www.research-collection.ethz.ch:20.500.11850/537322
institution Open Polar
language English
op_collection_id ftethz
op_doi https://doi.org/20.500.11850/53732210.3929/ethz-b-00053732210.1017/jog.2022.4
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1017/jog.2022.4
info:eu-repo/semantics/altIdentifier/wos/000768582400001
info:eu-repo/grantAgreement/ETHZ/ETH Grants/ETH-11 19-2
http://hdl.handle.net/20.500.11850/537322
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International
op_source Journal of Glaciology, 68 (271)
publishDate 2022
publisher Cambridge University Press
record_format openpolar
spelling ftethz:oai:www.research-collection.ethz.ch:20.500.11850/537322 2025-03-30T15:17:09+00:00 Characterising englacial R-channels using artificial moulins Pohle, Annegret id_orcid:0 000-0002-0986-5778 Werder, Mauro id_orcid:0 000-0003-0137-9377 Gräff, Dominik id_orcid:0 000-0003-1642-4783 Farinotti, Daniel id_orcid:0 000-0003-3417-4570 2022-10 application/application/pdf https://hdl.handle.net/20.500.11850/537322 https://doi.org/10.3929/ethz-b-000537322 en eng Cambridge University Press info:eu-repo/semantics/altIdentifier/doi/10.1017/jog.2022.4 info:eu-repo/semantics/altIdentifier/wos/000768582400001 info:eu-repo/grantAgreement/ETHZ/ETH Grants/ETH-11 19-2 http://hdl.handle.net/20.500.11850/537322 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International Journal of Glaciology, 68 (271) Glacier discharge Glacier hydrology Glaciological instruments and methods info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2022 ftethz https://doi.org/20.500.11850/53732210.3929/ethz-b-00053732210.1017/jog.2022.4 2025-03-05T22:09:18Z The englacial and subglacial drainage systems exert key controls on glacier dynamics. However, due to their inaccessibility, they are still only poorly understood and more detailed observations are important, particularly to validate and tune physical models describing their dynamics. By creating artificial glacier moulins – boreholes connected to the subglacial drainage system and supplied with water from surface streams – we present a novel method to monitor the evolution of an englacial hydrological system with high temporal resolution. Here, we use artificial moulins as representations for vertical, pressurised, englacial R-channels. From tracer and pressure measurements, we derive time series of the hydraulic gradient, discharge, flow speed and channel cross-sectional area. Using these, we compute the Darcy–Weisbach friction factor, obtaining values which increase from 0.1 to 13 within five days of channel evolution. Furthermore, we simulate the growth of the cross-sectional area using different temperature gradients. The comparison to our measurements largely supports the common assumption that the temperature follows the pressure melting point. The deviations from this behaviour are analysed using various heat transfer parameterisations to assess their applicability. Finally, we discuss how artificial moulins could be combined with glacier-wide tracer experiments to constrain parameters of subglacial drainage more precisely. ISSN:0022-1430 ISSN:1727-5652 Article in Journal/Newspaper Journal of Glaciology ETH Zürich Research Collection
spellingShingle Glacier discharge
Glacier hydrology
Glaciological instruments and methods
Pohle, Annegret
id_orcid:0 000-0002-0986-5778
Werder, Mauro
id_orcid:0 000-0003-0137-9377
Gräff, Dominik
id_orcid:0 000-0003-1642-4783
Farinotti, Daniel
id_orcid:0 000-0003-3417-4570
Characterising englacial R-channels using artificial moulins
title Characterising englacial R-channels using artificial moulins
title_full Characterising englacial R-channels using artificial moulins
title_fullStr Characterising englacial R-channels using artificial moulins
title_full_unstemmed Characterising englacial R-channels using artificial moulins
title_short Characterising englacial R-channels using artificial moulins
title_sort characterising englacial r-channels using artificial moulins
topic Glacier discharge
Glacier hydrology
Glaciological instruments and methods
topic_facet Glacier discharge
Glacier hydrology
Glaciological instruments and methods
url https://hdl.handle.net/20.500.11850/537322
https://doi.org/10.3929/ethz-b-000537322