The studies of the Svalbard glacial surfaces albedo by an unmanned aerial vehicle.

Abstract Experiments related to the use of unmanned aerial vehicle (UAV) for assessing the albedo of Svalbard glaciers is described. Study area - Esmark Glacier (Isfjord Bay) and Aldegonda Glacier (Greenfjord Bay). The main purpose of the experiments is to estimate the surface albedo in the zone of...

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Published in:IOP Conference Series: Earth and Environmental Science
Main Authors: Ivanov, B V, Zhuravskiy, D M, Prokhorova, U V, Bezgreshnov, A M, Terekhov, A V, Kurapov, M V, Paramzin, A S, Kashkova, V S
Format: Article in Journal/Newspaper
Language:unknown
Published: IOP Publishing 2022
Subjects:
Online Access:http://dx.doi.org/10.1088/1755-1315/1040/1/012002
https://iopscience.iop.org/article/10.1088/1755-1315/1040/1/012002
https://iopscience.iop.org/article/10.1088/1755-1315/1040/1/012002/pdf
id crioppubl:10.1088/1755-1315/1040/1/012002
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spelling crioppubl:10.1088/1755-1315/1040/1/012002 2024-06-02T08:06:12+00:00 The studies of the Svalbard glacial surfaces albedo by an unmanned aerial vehicle. Ivanov, B V Zhuravskiy, D M Prokhorova, U V Bezgreshnov, A M Terekhov, A V Kurapov, M V Paramzin, A S Kashkova, V S 2022 http://dx.doi.org/10.1088/1755-1315/1040/1/012002 https://iopscience.iop.org/article/10.1088/1755-1315/1040/1/012002 https://iopscience.iop.org/article/10.1088/1755-1315/1040/1/012002/pdf unknown IOP Publishing http://creativecommons.org/licenses/by/3.0/ https://iopscience.iop.org/info/page/text-and-data-mining IOP Conference Series: Earth and Environmental Science volume 1040, issue 1, page 012002 ISSN 1755-1307 1755-1315 journal-article 2022 crioppubl https://doi.org/10.1088/1755-1315/1040/1/012002 2024-05-07T13:59:48Z Abstract Experiments related to the use of unmanned aerial vehicle (UAV) for assessing the albedo of Svalbard glaciers is described. Study area - Esmark Glacier (Isfjord Bay) and Aldegonda Glacier (Greenfjord Bay). The main purpose of the experiments is to estimate the surface albedo in the zone of the edge cracks of the outlet glacier (Esmark), where standard ground-based observations are impossible due to safety conditions, as well as to obtain spatial albedo estimates (Aldegonda) when satellite data cannot be used (overcast). The UAV (DJI Phantom 4 Pro) was retrofitted with a sensor that measures reflected solar radiation. The data on the incoming solar radiation at the surface level, measured by a similar sensor, were used to calculate the albedo. The albedo measurements were carried out along several profiles across the Aldegonda Glacier and along one profile above the Esmark Glacier, which was laid from a flat plateau (ice dome) through a zone of cracks to the open water surface of the fiord. For the first time, estimates of the surface albedo of the outlet glacier in the zone of edge cracks were obtained. Ground-based verification observations carried out on the Aldegonda glacier confirmed the results obtained by the UAV. Article in Journal/Newspaper Esmark Glacier glacier Isfjord* Svalbard IOP Publishing Esmark Glacier ENVELOPE(-37.241,-37.241,-54.236,-54.236) Isfjord ENVELOPE(-26.917,-26.917,73.333,73.333) Svalbard IOP Conference Series: Earth and Environmental Science 1040 1 012002
institution Open Polar
collection IOP Publishing
op_collection_id crioppubl
language unknown
description Abstract Experiments related to the use of unmanned aerial vehicle (UAV) for assessing the albedo of Svalbard glaciers is described. Study area - Esmark Glacier (Isfjord Bay) and Aldegonda Glacier (Greenfjord Bay). The main purpose of the experiments is to estimate the surface albedo in the zone of the edge cracks of the outlet glacier (Esmark), where standard ground-based observations are impossible due to safety conditions, as well as to obtain spatial albedo estimates (Aldegonda) when satellite data cannot be used (overcast). The UAV (DJI Phantom 4 Pro) was retrofitted with a sensor that measures reflected solar radiation. The data on the incoming solar radiation at the surface level, measured by a similar sensor, were used to calculate the albedo. The albedo measurements were carried out along several profiles across the Aldegonda Glacier and along one profile above the Esmark Glacier, which was laid from a flat plateau (ice dome) through a zone of cracks to the open water surface of the fiord. For the first time, estimates of the surface albedo of the outlet glacier in the zone of edge cracks were obtained. Ground-based verification observations carried out on the Aldegonda glacier confirmed the results obtained by the UAV.
format Article in Journal/Newspaper
author Ivanov, B V
Zhuravskiy, D M
Prokhorova, U V
Bezgreshnov, A M
Terekhov, A V
Kurapov, M V
Paramzin, A S
Kashkova, V S
spellingShingle Ivanov, B V
Zhuravskiy, D M
Prokhorova, U V
Bezgreshnov, A M
Terekhov, A V
Kurapov, M V
Paramzin, A S
Kashkova, V S
The studies of the Svalbard glacial surfaces albedo by an unmanned aerial vehicle.
author_facet Ivanov, B V
Zhuravskiy, D M
Prokhorova, U V
Bezgreshnov, A M
Terekhov, A V
Kurapov, M V
Paramzin, A S
Kashkova, V S
author_sort Ivanov, B V
title The studies of the Svalbard glacial surfaces albedo by an unmanned aerial vehicle.
title_short The studies of the Svalbard glacial surfaces albedo by an unmanned aerial vehicle.
title_full The studies of the Svalbard glacial surfaces albedo by an unmanned aerial vehicle.
title_fullStr The studies of the Svalbard glacial surfaces albedo by an unmanned aerial vehicle.
title_full_unstemmed The studies of the Svalbard glacial surfaces albedo by an unmanned aerial vehicle.
title_sort studies of the svalbard glacial surfaces albedo by an unmanned aerial vehicle.
publisher IOP Publishing
publishDate 2022
url http://dx.doi.org/10.1088/1755-1315/1040/1/012002
https://iopscience.iop.org/article/10.1088/1755-1315/1040/1/012002
https://iopscience.iop.org/article/10.1088/1755-1315/1040/1/012002/pdf
long_lat ENVELOPE(-37.241,-37.241,-54.236,-54.236)
ENVELOPE(-26.917,-26.917,73.333,73.333)
geographic Esmark Glacier
Isfjord
Svalbard
geographic_facet Esmark Glacier
Isfjord
Svalbard
genre Esmark Glacier
glacier
Isfjord*
Svalbard
genre_facet Esmark Glacier
glacier
Isfjord*
Svalbard
op_source IOP Conference Series: Earth and Environmental Science
volume 1040, issue 1, page 012002
ISSN 1755-1307 1755-1315
op_rights http://creativecommons.org/licenses/by/3.0/
https://iopscience.iop.org/info/page/text-and-data-mining
op_doi https://doi.org/10.1088/1755-1315/1040/1/012002
container_title IOP Conference Series: Earth and Environmental Science
container_volume 1040
container_issue 1
container_start_page 012002
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