Glacier Remote Sensing Using Sentinel-2. Part I: Radiometric and Geometric Performance, and Application to Ice Velocity

With its temporal resolution of 10 days (five days with two satellites, and significantly more at high latitudes), its swath width of 290 km, and its 10 m and 20 m spatial resolution bands from the visible to the shortwave infrared, the European Sentinel-2 satellites have significant potential for g...

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Published in:Remote Sensing
Main Authors: Andreas Kääb, Solveig Winsvold, Bas Altena, Christopher Nuth, Thomas Nagler, Jan Wuite
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2016
Subjects:
Online Access:https://doi.org/10.3390/rs8070598
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spelling ftmdpi:oai:mdpi.com:/2072-4292/8/7/598/ 2023-08-20T04:00:43+02:00 Glacier Remote Sensing Using Sentinel-2. Part I: Radiometric and Geometric Performance, and Application to Ice Velocity Andreas Kääb Solveig Winsvold Bas Altena Christopher Nuth Thomas Nagler Jan Wuite agris 2016-07-15 application/pdf https://doi.org/10.3390/rs8070598 EN eng Multidisciplinary Digital Publishing Institute Remote Sensing in Agriculture and Vegetation https://dx.doi.org/10.3390/rs8070598 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 8; Issue 7; Pages: 598 Sentinel-2 Landsat ortho-rectification geo-location ice velocity Aletsch Glacier Fox Glacier Jakobshavn Isbree Antarctic Peninsula Text 2016 ftmdpi https://doi.org/10.3390/rs8070598 2023-07-31T20:55:11Z With its temporal resolution of 10 days (five days with two satellites, and significantly more at high latitudes), its swath width of 290 km, and its 10 m and 20 m spatial resolution bands from the visible to the shortwave infrared, the European Sentinel-2 satellites have significant potential for glacier remote sensing, in particular mapping of glacier outlines and facies, and velocity measurements. Testing Level 1C commissioning and ramp-up phase data for initial sensor quality experiences, we find a high radiometric performance, but with slight striping effects under certain conditions. Through co-registration of repeat Sentinal-2 data we also find lateral offset patterns and noise on the order of a few metres. Neither of these issues will complicate most typical glaciological applications. Absolute geo-location of the data investigated was on the order of one pixel at the time of writing. The most severe geometric problem stems from vertical errors of the DEM used for ortho-rectifying Sentinel-2 data. These errors propagate into locally varying lateral offsets in the images, up to several pixels with respect to other georeferenced data, or between Sentinel-2 data from different orbits. Finally, we characterize the potential and limitations of tracking glacier flow from repeat Sentinel-2 data using a set of typical glaciers in different environments: Aletsch Glacier, Swiss Alps; Fox Glacier, New Zealand; Jakobshavn Isbree, Greenland; Antarctic Peninsula at the Larsen C ice shelf. Text Antarc* Antarctic Antarctic Peninsula glacier Greenland Ice Shelf Jakobshavn MDPI Open Access Publishing Antarctic Antarctic Peninsula Fox Glacier ENVELOPE(114.417,114.417,-66.233,-66.233) Greenland New Zealand Remote Sensing 8 7 598
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Sentinel-2
Landsat
ortho-rectification
geo-location
ice velocity
Aletsch Glacier
Fox Glacier
Jakobshavn Isbree
Antarctic Peninsula
spellingShingle Sentinel-2
Landsat
ortho-rectification
geo-location
ice velocity
Aletsch Glacier
Fox Glacier
Jakobshavn Isbree
Antarctic Peninsula
Andreas Kääb
Solveig Winsvold
Bas Altena
Christopher Nuth
Thomas Nagler
Jan Wuite
Glacier Remote Sensing Using Sentinel-2. Part I: Radiometric and Geometric Performance, and Application to Ice Velocity
topic_facet Sentinel-2
Landsat
ortho-rectification
geo-location
ice velocity
Aletsch Glacier
Fox Glacier
Jakobshavn Isbree
Antarctic Peninsula
description With its temporal resolution of 10 days (five days with two satellites, and significantly more at high latitudes), its swath width of 290 km, and its 10 m and 20 m spatial resolution bands from the visible to the shortwave infrared, the European Sentinel-2 satellites have significant potential for glacier remote sensing, in particular mapping of glacier outlines and facies, and velocity measurements. Testing Level 1C commissioning and ramp-up phase data for initial sensor quality experiences, we find a high radiometric performance, but with slight striping effects under certain conditions. Through co-registration of repeat Sentinal-2 data we also find lateral offset patterns and noise on the order of a few metres. Neither of these issues will complicate most typical glaciological applications. Absolute geo-location of the data investigated was on the order of one pixel at the time of writing. The most severe geometric problem stems from vertical errors of the DEM used for ortho-rectifying Sentinel-2 data. These errors propagate into locally varying lateral offsets in the images, up to several pixels with respect to other georeferenced data, or between Sentinel-2 data from different orbits. Finally, we characterize the potential and limitations of tracking glacier flow from repeat Sentinel-2 data using a set of typical glaciers in different environments: Aletsch Glacier, Swiss Alps; Fox Glacier, New Zealand; Jakobshavn Isbree, Greenland; Antarctic Peninsula at the Larsen C ice shelf.
format Text
author Andreas Kääb
Solveig Winsvold
Bas Altena
Christopher Nuth
Thomas Nagler
Jan Wuite
author_facet Andreas Kääb
Solveig Winsvold
Bas Altena
Christopher Nuth
Thomas Nagler
Jan Wuite
author_sort Andreas Kääb
title Glacier Remote Sensing Using Sentinel-2. Part I: Radiometric and Geometric Performance, and Application to Ice Velocity
title_short Glacier Remote Sensing Using Sentinel-2. Part I: Radiometric and Geometric Performance, and Application to Ice Velocity
title_full Glacier Remote Sensing Using Sentinel-2. Part I: Radiometric and Geometric Performance, and Application to Ice Velocity
title_fullStr Glacier Remote Sensing Using Sentinel-2. Part I: Radiometric and Geometric Performance, and Application to Ice Velocity
title_full_unstemmed Glacier Remote Sensing Using Sentinel-2. Part I: Radiometric and Geometric Performance, and Application to Ice Velocity
title_sort glacier remote sensing using sentinel-2. part i: radiometric and geometric performance, and application to ice velocity
publisher Multidisciplinary Digital Publishing Institute
publishDate 2016
url https://doi.org/10.3390/rs8070598
op_coverage agris
long_lat ENVELOPE(114.417,114.417,-66.233,-66.233)
geographic Antarctic
Antarctic Peninsula
Fox Glacier
Greenland
New Zealand
geographic_facet Antarctic
Antarctic Peninsula
Fox Glacier
Greenland
New Zealand
genre Antarc*
Antarctic
Antarctic Peninsula
glacier
Greenland
Ice Shelf
Jakobshavn
genre_facet Antarc*
Antarctic
Antarctic Peninsula
glacier
Greenland
Ice Shelf
Jakobshavn
op_source Remote Sensing; Volume 8; Issue 7; Pages: 598
op_relation Remote Sensing in Agriculture and Vegetation
https://dx.doi.org/10.3390/rs8070598
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs8070598
container_title Remote Sensing
container_volume 8
container_issue 7
container_start_page 598
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