Applying artificial snowfall to reduce the melting of the Muz Taw Glacier, Sawir Mountains

The glaciers in the Sawir Mountains, Altai area, have been experiencing a continuing and accelerating ice loss since 1959, although the snowfall is abundant and evenly distributed over the year. As an attempt to reduce their melting, we carried out two artificial snowfall experiments on the Muz Taw...

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Published in:The Cryosphere
Main Authors: F. Wang, X. Yue, L. Wang, H. Li, Z. Du, J. Ming, Z. Li
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2020
Subjects:
Ela
Online Access:https://doi.org/10.5194/tc-14-2597-2020
https://doaj.org/article/6004691a280e4ef7b6fc4889df93c1c1
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spelling ftdoajarticles:oai:doaj.org/article:6004691a280e4ef7b6fc4889df93c1c1 2023-05-15T18:32:29+02:00 Applying artificial snowfall to reduce the melting of the Muz Taw Glacier, Sawir Mountains F. Wang X. Yue L. Wang H. Li Z. Du J. Ming Z. Li 2020-08-01T00:00:00Z https://doi.org/10.5194/tc-14-2597-2020 https://doaj.org/article/6004691a280e4ef7b6fc4889df93c1c1 EN eng Copernicus Publications https://tc.copernicus.org/articles/14/2597/2020/tc-14-2597-2020.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-14-2597-2020 1994-0416 1994-0424 https://doaj.org/article/6004691a280e4ef7b6fc4889df93c1c1 The Cryosphere, Vol 14, Pp 2597-2606 (2020) Environmental sciences GE1-350 Geology QE1-996.5 article 2020 ftdoajarticles https://doi.org/10.5194/tc-14-2597-2020 2022-12-31T08:30:49Z The glaciers in the Sawir Mountains, Altai area, have been experiencing a continuing and accelerating ice loss since 1959, although the snowfall is abundant and evenly distributed over the year. As an attempt to reduce their melting, we carried out two artificial snowfall experiments on the Muz Taw Glacier during 19–22 August 2018. We measured the albedo and mass balance at different sites along the glacier before and after the experiments. Two automatic weather stations (AWSs) were set up at the equilibrium line altitude (ELA) of the glacier as the target area and the forefield as the control area to record the precipitation, respectively. A comparison of the two precipitation records from the two AWSs suggests that natural precipitation could account for up to 21 % of the snowfall received by the glacier during the experiments. Because of the snowfalls, the glacier's surface albedo significantly increased in the middle to upper part; the average mass loss during 18–24 August (after the experiments) decreased by between 32 and 41 mm w.e (14 %–17 %) compared to during 12–18 August (before the experiments); and the mass resulting from the snowfall accounted for between 42 % and 54 % of the total melt during 18–24 August. We also propose a mechanism involving artificial snowfall, albedo, and mass balance, and the feedbacks describing the role of snowfall in reducing the melting of the glacier. The current status of the work is primitive as it is a preliminary trial, and the conclusions need more controlling experiments to validate it against larger spatio-temporal scales in future. Article in Journal/Newspaper The Cryosphere Directory of Open Access Journals: DOAJ Articles Ela ENVELOPE(9.642,9.642,63.170,63.170) The Cryosphere 14 8 2597 2606
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
F. Wang
X. Yue
L. Wang
H. Li
Z. Du
J. Ming
Z. Li
Applying artificial snowfall to reduce the melting of the Muz Taw Glacier, Sawir Mountains
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description The glaciers in the Sawir Mountains, Altai area, have been experiencing a continuing and accelerating ice loss since 1959, although the snowfall is abundant and evenly distributed over the year. As an attempt to reduce their melting, we carried out two artificial snowfall experiments on the Muz Taw Glacier during 19–22 August 2018. We measured the albedo and mass balance at different sites along the glacier before and after the experiments. Two automatic weather stations (AWSs) were set up at the equilibrium line altitude (ELA) of the glacier as the target area and the forefield as the control area to record the precipitation, respectively. A comparison of the two precipitation records from the two AWSs suggests that natural precipitation could account for up to 21 % of the snowfall received by the glacier during the experiments. Because of the snowfalls, the glacier's surface albedo significantly increased in the middle to upper part; the average mass loss during 18–24 August (after the experiments) decreased by between 32 and 41 mm w.e (14 %–17 %) compared to during 12–18 August (before the experiments); and the mass resulting from the snowfall accounted for between 42 % and 54 % of the total melt during 18–24 August. We also propose a mechanism involving artificial snowfall, albedo, and mass balance, and the feedbacks describing the role of snowfall in reducing the melting of the glacier. The current status of the work is primitive as it is a preliminary trial, and the conclusions need more controlling experiments to validate it against larger spatio-temporal scales in future.
format Article in Journal/Newspaper
author F. Wang
X. Yue
L. Wang
H. Li
Z. Du
J. Ming
Z. Li
author_facet F. Wang
X. Yue
L. Wang
H. Li
Z. Du
J. Ming
Z. Li
author_sort F. Wang
title Applying artificial snowfall to reduce the melting of the Muz Taw Glacier, Sawir Mountains
title_short Applying artificial snowfall to reduce the melting of the Muz Taw Glacier, Sawir Mountains
title_full Applying artificial snowfall to reduce the melting of the Muz Taw Glacier, Sawir Mountains
title_fullStr Applying artificial snowfall to reduce the melting of the Muz Taw Glacier, Sawir Mountains
title_full_unstemmed Applying artificial snowfall to reduce the melting of the Muz Taw Glacier, Sawir Mountains
title_sort applying artificial snowfall to reduce the melting of the muz taw glacier, sawir mountains
publisher Copernicus Publications
publishDate 2020
url https://doi.org/10.5194/tc-14-2597-2020
https://doaj.org/article/6004691a280e4ef7b6fc4889df93c1c1
long_lat ENVELOPE(9.642,9.642,63.170,63.170)
geographic Ela
geographic_facet Ela
genre The Cryosphere
genre_facet The Cryosphere
op_source The Cryosphere, Vol 14, Pp 2597-2606 (2020)
op_relation https://tc.copernicus.org/articles/14/2597/2020/tc-14-2597-2020.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-14-2597-2020
1994-0416
1994-0424
https://doaj.org/article/6004691a280e4ef7b6fc4889df93c1c1
op_doi https://doi.org/10.5194/tc-14-2597-2020
container_title The Cryosphere
container_volume 14
container_issue 8
container_start_page 2597
op_container_end_page 2606
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