Applying artificial snowfall to reduce the melting of the Muz Taw Glacier, Sawir Mountains
<p>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...
Main Authors: | , , , , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2020-08-01
|
Series: | The Cryosphere |
Online Access: | https://tc.copernicus.org/articles/14/2597/2020/tc-14-2597-2020.pdf |
Summary: | <p>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.</p> |
---|---|
ISSN: | 1994-0416 1994-0424 |