Evaluation of ICEYE Microsatellites Sensor for Surface Motion Detection—Jakobshavn Glacier Case Study

The marine-terminating glaciers are one of the biggest contributors to global sea-level rise. Research on this aspect of the effects of global climate change is developing nowadays in several directions. One of them is monitoring of glaciers movements, especially with satellite data. In addition to...

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Main Authors: Magdalena A. Łukosz, Ryszard Hejmanowski, Wojciech T. Witkowski
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:https://www.mdpi.com/1996-1073/14/12/3424/pdf
https://www.mdpi.com/1996-1073/14/12/3424/
id ftrepec:oai:RePEc:gam:jeners:v:14:y:2021:i:12:p:3424-:d:572303
record_format openpolar
spelling ftrepec:oai:RePEc:gam:jeners:v:14:y:2021:i:12:p:3424-:d:572303 2024-04-14T08:14:06+00:00 Evaluation of ICEYE Microsatellites Sensor for Surface Motion Detection—Jakobshavn Glacier Case Study Magdalena A. Łukosz Ryszard Hejmanowski Wojciech T. Witkowski https://www.mdpi.com/1996-1073/14/12/3424/pdf https://www.mdpi.com/1996-1073/14/12/3424/ unknown https://www.mdpi.com/1996-1073/14/12/3424/pdf https://www.mdpi.com/1996-1073/14/12/3424/ article ftrepec 2024-03-19T10:41:27Z The marine-terminating glaciers are one of the biggest contributors to global sea-level rise. Research on this aspect of the effects of global climate change is developing nowadays in several directions. One of them is monitoring of glaciers movements, especially with satellite data. In addition to well-known analyzes based on radar data from available satellites, the possibility of studying glacier displacements from new sensors, the so-called microsatellites need to be studied. The main purpose of research was evaluation of the possibility of applying new high-resolution ICEYE radar data to observe glacier motion. Stripmap High mode were used to obtain velocities for the Jakobshavn glacier with an Offset-Tracking method. Obtained results were compared with displacements obtained from the Sentinel-1 data. The comparative analysis was performed on displacements in range and azimuth directions and for maximum velocity values. Moreover, correlation plots showed that in different parts of glaciers, a comparison of obtained velocities delivers different correlation coefficients (R 2 ) in a range from 0.52 to 0.97. The analysis showed that the scale of movements is similar from both sensors. However, Sentinel-1 data present underestimation of velocities comparing to ICEYE data. The biggest deviations between results were observed around the maximum velocities, near the Kangia Ice Fjord Bay. In the analysis the amplitude information was used as well. This research presents that data from the ICEYE microsatellites can be successfully used for monitoring glacial areas and it allows for more precise observations of displacement velocity field. marine-terminating glacier; Jakobshavn glacier; Offset-Tracking; ICEYE microsatellites; glacier surface velocity Article in Journal/Newspaper Jakobshavn Kangia RePEc (Research Papers in Economics) The Sentinel ENVELOPE(73.317,73.317,-52.983,-52.983) Ice Fjord ENVELOPE(-37.694,-37.694,-54.060,-54.060)
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description The marine-terminating glaciers are one of the biggest contributors to global sea-level rise. Research on this aspect of the effects of global climate change is developing nowadays in several directions. One of them is monitoring of glaciers movements, especially with satellite data. In addition to well-known analyzes based on radar data from available satellites, the possibility of studying glacier displacements from new sensors, the so-called microsatellites need to be studied. The main purpose of research was evaluation of the possibility of applying new high-resolution ICEYE radar data to observe glacier motion. Stripmap High mode were used to obtain velocities for the Jakobshavn glacier with an Offset-Tracking method. Obtained results were compared with displacements obtained from the Sentinel-1 data. The comparative analysis was performed on displacements in range and azimuth directions and for maximum velocity values. Moreover, correlation plots showed that in different parts of glaciers, a comparison of obtained velocities delivers different correlation coefficients (R 2 ) in a range from 0.52 to 0.97. The analysis showed that the scale of movements is similar from both sensors. However, Sentinel-1 data present underestimation of velocities comparing to ICEYE data. The biggest deviations between results were observed around the maximum velocities, near the Kangia Ice Fjord Bay. In the analysis the amplitude information was used as well. This research presents that data from the ICEYE microsatellites can be successfully used for monitoring glacial areas and it allows for more precise observations of displacement velocity field. marine-terminating glacier; Jakobshavn glacier; Offset-Tracking; ICEYE microsatellites; glacier surface velocity
format Article in Journal/Newspaper
author Magdalena A. Łukosz
Ryszard Hejmanowski
Wojciech T. Witkowski
spellingShingle Magdalena A. Łukosz
Ryszard Hejmanowski
Wojciech T. Witkowski
Evaluation of ICEYE Microsatellites Sensor for Surface Motion Detection—Jakobshavn Glacier Case Study
author_facet Magdalena A. Łukosz
Ryszard Hejmanowski
Wojciech T. Witkowski
author_sort Magdalena A. Łukosz
title Evaluation of ICEYE Microsatellites Sensor for Surface Motion Detection—Jakobshavn Glacier Case Study
title_short Evaluation of ICEYE Microsatellites Sensor for Surface Motion Detection—Jakobshavn Glacier Case Study
title_full Evaluation of ICEYE Microsatellites Sensor for Surface Motion Detection—Jakobshavn Glacier Case Study
title_fullStr Evaluation of ICEYE Microsatellites Sensor for Surface Motion Detection—Jakobshavn Glacier Case Study
title_full_unstemmed Evaluation of ICEYE Microsatellites Sensor for Surface Motion Detection—Jakobshavn Glacier Case Study
title_sort evaluation of iceye microsatellites sensor for surface motion detection—jakobshavn glacier case study
url https://www.mdpi.com/1996-1073/14/12/3424/pdf
https://www.mdpi.com/1996-1073/14/12/3424/
long_lat ENVELOPE(73.317,73.317,-52.983,-52.983)
ENVELOPE(-37.694,-37.694,-54.060,-54.060)
geographic The Sentinel
Ice Fjord
geographic_facet The Sentinel
Ice Fjord
genre Jakobshavn
Kangia
genre_facet Jakobshavn
Kangia
op_relation https://www.mdpi.com/1996-1073/14/12/3424/pdf
https://www.mdpi.com/1996-1073/14/12/3424/
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