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...
Published in: | Journal of Glaciology |
---|---|
Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press
2022
|
Subjects: | |
Online Access: | https://doi.org/10.1017/jog.2022.4 https://doaj.org/article/42d87a9115b24b80b43b4f3cbba27ddc |
id |
ftdoajarticles:oai:doaj.org/article:42d87a9115b24b80b43b4f3cbba27ddc |
---|---|
record_format |
openpolar |
spelling |
ftdoajarticles:oai:doaj.org/article:42d87a9115b24b80b43b4f3cbba27ddc 2023-05-15T16:57:32+02:00 Characterising englacial R-channels using artificial moulins Annegret Pohle Mauro A. Werder Dominik Gräff Daniel Farinotti 2022-10-01T00:00:00Z https://doi.org/10.1017/jog.2022.4 https://doaj.org/article/42d87a9115b24b80b43b4f3cbba27ddc EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143022000041/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.4 0022-1430 1727-5652 https://doaj.org/article/42d87a9115b24b80b43b4f3cbba27ddc Journal of Glaciology, Vol 68, Pp 879-890 (2022) Glacier discharge glacier hydrology glaciological instruments and methods Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2022 ftdoajarticles https://doi.org/10.1017/jog.2022.4 2023-03-12T01:30:54Z 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. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 1 12 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Glacier discharge glacier hydrology glaciological instruments and methods Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
Glacier discharge glacier hydrology glaciological instruments and methods Environmental sciences GE1-350 Meteorology. Climatology QC851-999 Annegret Pohle Mauro A. Werder Dominik Gräff Daniel Farinotti Characterising englacial R-channels using artificial moulins |
topic_facet |
Glacier discharge glacier hydrology glaciological instruments and methods Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
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. |
format |
Article in Journal/Newspaper |
author |
Annegret Pohle Mauro A. Werder Dominik Gräff Daniel Farinotti |
author_facet |
Annegret Pohle Mauro A. Werder Dominik Gräff Daniel Farinotti |
author_sort |
Annegret Pohle |
title |
Characterising englacial R-channels using artificial moulins |
title_short |
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_sort |
characterising englacial r-channels using artificial moulins |
publisher |
Cambridge University Press |
publishDate |
2022 |
url |
https://doi.org/10.1017/jog.2022.4 https://doaj.org/article/42d87a9115b24b80b43b4f3cbba27ddc |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology, Vol 68, Pp 879-890 (2022) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143022000041/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.4 0022-1430 1727-5652 https://doaj.org/article/42d87a9115b24b80b43b4f3cbba27ddc |
op_doi |
https://doi.org/10.1017/jog.2022.4 |
container_title |
Journal of Glaciology |
container_start_page |
1 |
op_container_end_page |
12 |
_version_ |
1766049100339347456 |