Dual-satellite (Sentinel-2 and Landsat 8) remote sensing of supraglacial lakes in Greenland

© 2018 All rights reserved. Remote sensing is commonly used to monitor supraglacial lakes on the Greenland Ice Sheet (GrIS); however, most satellite records must trade off higher spatial resolution for higher temporal resolution (e.g. MODIS) or vice versa (e.g. Landsat). Here, we overcome this issue...

Full description

Bibliographic Details
Main Authors: Williamson, AG, Banwell, AF, Willis, IC, Arnold, NS
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2018
Subjects:
Online Access:https://www.repository.cam.ac.uk/handle/1810/285168
https://doi.org/10.17863/CAM.32538
id ftunivcam:oai:www.repository.cam.ac.uk:1810/285168
record_format openpolar
spelling ftunivcam:oai:www.repository.cam.ac.uk:1810/285168 2024-01-14T10:07:16+01:00 Dual-satellite (Sentinel-2 and Landsat 8) remote sensing of supraglacial lakes in Greenland Williamson, AG Banwell, AF Willis, IC Arnold, NS 2018-09-26 application/pdf https://www.repository.cam.ac.uk/handle/1810/285168 https://doi.org/10.17863/CAM.32538 eng eng Copernicus Publications http://dx.doi.org/10.5194/tc-2018-56 Cryosphere https://doi.org/10.17863/CAM.25769 https://www.repository.cam.ac.uk/handle/1810/285168 doi:10.17863/CAM.32538 Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ 37 Earth Sciences 3709 Physical Geography and Environmental Geoscience Bioengineering 13 Climate Action Article 2018 ftunivcam https://doi.org/10.17863/CAM.3253810.17863/CAM.25769 2023-12-21T23:29:00Z © 2018 All rights reserved. Remote sensing is commonly used to monitor supraglacial lakes on the Greenland Ice Sheet (GrIS); however, most satellite records must trade off higher spatial resolution for higher temporal resolution (e.g. MODIS) or vice versa (e.g. Landsat). Here, we overcome this issue by developing and applying a dual-sensor method that can monitor changes to lake areas and volumes at high spatial resolution (10-30 m) with a frequent revisit time ( ~ 3 days). We achieve this by mosaicking imagery from the Landsat 8 Operational Land Imager (OLI) with imagery from the recently launched Sentinel-2 Multispectral Instrument (MSI) for a ~ 12 000 km2area of West Greenland in the 2016 melt season. First, we validate a physically based method for calculating lake depths with Sentinel-2 by comparing measurements against those derived from the available contemporaneous Landsat 8 imagery; we find close correspondence between the two sets of values (R2Combining double low line 0.841; RMSE Combining double low line 0.555 m). This provides us with the methodological basis for automatically calculating lake areas, depths, and volumes from all available Landsat 8 and Sentinel-2 images. These automatic methods are incorporated into an algorithm for Fully Automated Supraglacial lake Tracking at Enhanced Resolution (FASTER). The FASTER algorithm produces time series showing lake evolution during the 2016 melt season, including automated rapid ( ≤ 4 day) lake-drainage identification. With the dual Sentinel-2-Landsat 8 record, we identify 184 rapidly draining lakes, many more than identified with either imagery collection alone (93 with Sentinel-2; 66 with Landsat 8), due to their inferior temporal resolution, or would be possible with MODIS, due to its omission of small lakes < 0.125 km2. Finally, we estimate the water volumes drained into the GrIS during rapid-lake-drainage events and, by analysing downscaled regional climate-model (RACMO2.3p2) run-off data, the water quantity that enters the GrIS via the moulins ... Article in Journal/Newspaper Greenland Ice Sheet Apollo - University of Cambridge Repository Greenland Rapid Lake ENVELOPE(177.619,177.619,52.064,52.064)
institution Open Polar
collection Apollo - University of Cambridge Repository
op_collection_id ftunivcam
language English
topic 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
Bioengineering
13 Climate Action
spellingShingle 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
Bioengineering
13 Climate Action
Williamson, AG
Banwell, AF
Willis, IC
Arnold, NS
Dual-satellite (Sentinel-2 and Landsat 8) remote sensing of supraglacial lakes in Greenland
topic_facet 37 Earth Sciences
3709 Physical Geography and Environmental Geoscience
Bioengineering
13 Climate Action
description © 2018 All rights reserved. Remote sensing is commonly used to monitor supraglacial lakes on the Greenland Ice Sheet (GrIS); however, most satellite records must trade off higher spatial resolution for higher temporal resolution (e.g. MODIS) or vice versa (e.g. Landsat). Here, we overcome this issue by developing and applying a dual-sensor method that can monitor changes to lake areas and volumes at high spatial resolution (10-30 m) with a frequent revisit time ( ~ 3 days). We achieve this by mosaicking imagery from the Landsat 8 Operational Land Imager (OLI) with imagery from the recently launched Sentinel-2 Multispectral Instrument (MSI) for a ~ 12 000 km2area of West Greenland in the 2016 melt season. First, we validate a physically based method for calculating lake depths with Sentinel-2 by comparing measurements against those derived from the available contemporaneous Landsat 8 imagery; we find close correspondence between the two sets of values (R2Combining double low line 0.841; RMSE Combining double low line 0.555 m). This provides us with the methodological basis for automatically calculating lake areas, depths, and volumes from all available Landsat 8 and Sentinel-2 images. These automatic methods are incorporated into an algorithm for Fully Automated Supraglacial lake Tracking at Enhanced Resolution (FASTER). The FASTER algorithm produces time series showing lake evolution during the 2016 melt season, including automated rapid ( ≤ 4 day) lake-drainage identification. With the dual Sentinel-2-Landsat 8 record, we identify 184 rapidly draining lakes, many more than identified with either imagery collection alone (93 with Sentinel-2; 66 with Landsat 8), due to their inferior temporal resolution, or would be possible with MODIS, due to its omission of small lakes < 0.125 km2. Finally, we estimate the water volumes drained into the GrIS during rapid-lake-drainage events and, by analysing downscaled regional climate-model (RACMO2.3p2) run-off data, the water quantity that enters the GrIS via the moulins ...
format Article in Journal/Newspaper
author Williamson, AG
Banwell, AF
Willis, IC
Arnold, NS
author_facet Williamson, AG
Banwell, AF
Willis, IC
Arnold, NS
author_sort Williamson, AG
title Dual-satellite (Sentinel-2 and Landsat 8) remote sensing of supraglacial lakes in Greenland
title_short Dual-satellite (Sentinel-2 and Landsat 8) remote sensing of supraglacial lakes in Greenland
title_full Dual-satellite (Sentinel-2 and Landsat 8) remote sensing of supraglacial lakes in Greenland
title_fullStr Dual-satellite (Sentinel-2 and Landsat 8) remote sensing of supraglacial lakes in Greenland
title_full_unstemmed Dual-satellite (Sentinel-2 and Landsat 8) remote sensing of supraglacial lakes in Greenland
title_sort dual-satellite (sentinel-2 and landsat 8) remote sensing of supraglacial lakes in greenland
publisher Copernicus Publications
publishDate 2018
url https://www.repository.cam.ac.uk/handle/1810/285168
https://doi.org/10.17863/CAM.32538
long_lat ENVELOPE(177.619,177.619,52.064,52.064)
geographic Greenland
Rapid Lake
geographic_facet Greenland
Rapid Lake
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_relation https://doi.org/10.17863/CAM.25769
https://www.repository.cam.ac.uk/handle/1810/285168
doi:10.17863/CAM.32538
op_rights Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.17863/CAM.3253810.17863/CAM.25769
_version_ 1788061687566303232