Fully Automated Detection of Supraglacial Lake Area for Northeast Greenland Using Sentinel-2 Time-Series

The usability of multispectral satellite data for detecting and monitoring supraglacial meltwater ponds has been demonstrated for western Greenland. For a multitemporal analysis of large regions or entire Greenland, largely automated processing routines are required. Here, we present a sequence of a...

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Published in:Remote Sensing
Main Authors: Philipp Hochreuther, Niklas Neckel, Nathalie Reimann, Angelika Humbert, Matthias Braun
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/rs13020205
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spelling ftmdpi:oai:mdpi.com:/2072-4292/13/2/205/ 2023-08-20T04:06:41+02:00 Fully Automated Detection of Supraglacial Lake Area for Northeast Greenland Using Sentinel-2 Time-Series Philipp Hochreuther Niklas Neckel Nathalie Reimann Angelika Humbert Matthias Braun agris 2021-01-08 application/pdf https://doi.org/10.3390/rs13020205 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs13020205 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 13; Issue 2; Pages: 205 supraglacial lakes 79 °N Sentinel-2 lake area automated detection Greenland Text 2021 ftmdpi https://doi.org/10.3390/rs13020205 2023-08-01T00:49:51Z The usability of multispectral satellite data for detecting and monitoring supraglacial meltwater ponds has been demonstrated for western Greenland. For a multitemporal analysis of large regions or entire Greenland, largely automated processing routines are required. Here, we present a sequence of algorithms that allow for an automated Sentinel-2 data search, download, processing, and generation of a consistent and dense melt pond area time-series based on open-source software. We test our approach for a ~82,000 km2 area at the 79 °N Glacier (Nioghalvfjerdsbrae) in northeast Greenland, covering the years 2016, 2017, 2018 and 2019. Our lake detection is based on the ratio of the blue and red visible bands using a minimum threshold. To remove false classification caused by the similar spectra of shadow and water on ice, we implement a shadow model to mask out topographically induced artifacts. We identified 880 individual lakes, traceable over 479 time-steps throughout 2016–2019, with an average size of 64,212 m2. Of the four years, 2019 had the most extensive lake area coverage with a maximum of 333 km2 and a maximum individual lake size of 30 km2. With 1.5 days average observation interval, our time-series allows for a comparison with climate data of daily resolution, enabling a better understanding of short-term climate-glacier feedbacks. Text glacier Greenland MDPI Open Access Publishing Greenland Remote Sensing 13 2 205
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic supraglacial lakes
79 °N
Sentinel-2
lake area
automated detection
Greenland
spellingShingle supraglacial lakes
79 °N
Sentinel-2
lake area
automated detection
Greenland
Philipp Hochreuther
Niklas Neckel
Nathalie Reimann
Angelika Humbert
Matthias Braun
Fully Automated Detection of Supraglacial Lake Area for Northeast Greenland Using Sentinel-2 Time-Series
topic_facet supraglacial lakes
79 °N
Sentinel-2
lake area
automated detection
Greenland
description The usability of multispectral satellite data for detecting and monitoring supraglacial meltwater ponds has been demonstrated for western Greenland. For a multitemporal analysis of large regions or entire Greenland, largely automated processing routines are required. Here, we present a sequence of algorithms that allow for an automated Sentinel-2 data search, download, processing, and generation of a consistent and dense melt pond area time-series based on open-source software. We test our approach for a ~82,000 km2 area at the 79 °N Glacier (Nioghalvfjerdsbrae) in northeast Greenland, covering the years 2016, 2017, 2018 and 2019. Our lake detection is based on the ratio of the blue and red visible bands using a minimum threshold. To remove false classification caused by the similar spectra of shadow and water on ice, we implement a shadow model to mask out topographically induced artifacts. We identified 880 individual lakes, traceable over 479 time-steps throughout 2016–2019, with an average size of 64,212 m2. Of the four years, 2019 had the most extensive lake area coverage with a maximum of 333 km2 and a maximum individual lake size of 30 km2. With 1.5 days average observation interval, our time-series allows for a comparison with climate data of daily resolution, enabling a better understanding of short-term climate-glacier feedbacks.
format Text
author Philipp Hochreuther
Niklas Neckel
Nathalie Reimann
Angelika Humbert
Matthias Braun
author_facet Philipp Hochreuther
Niklas Neckel
Nathalie Reimann
Angelika Humbert
Matthias Braun
author_sort Philipp Hochreuther
title Fully Automated Detection of Supraglacial Lake Area for Northeast Greenland Using Sentinel-2 Time-Series
title_short Fully Automated Detection of Supraglacial Lake Area for Northeast Greenland Using Sentinel-2 Time-Series
title_full Fully Automated Detection of Supraglacial Lake Area for Northeast Greenland Using Sentinel-2 Time-Series
title_fullStr Fully Automated Detection of Supraglacial Lake Area for Northeast Greenland Using Sentinel-2 Time-Series
title_full_unstemmed Fully Automated Detection of Supraglacial Lake Area for Northeast Greenland Using Sentinel-2 Time-Series
title_sort fully automated detection of supraglacial lake area for northeast greenland using sentinel-2 time-series
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/rs13020205
op_coverage agris
geographic Greenland
geographic_facet Greenland
genre glacier
Greenland
genre_facet glacier
Greenland
op_source Remote Sensing; Volume 13; Issue 2; Pages: 205
op_relation https://dx.doi.org/10.3390/rs13020205
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs13020205
container_title Remote Sensing
container_volume 13
container_issue 2
container_start_page 205
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