Sentinel-1 detection of ice slabs on the Greenland Ice Sheet
Ice slabs are multi-meter-thick layers of refrozen ice that limit meltwater storage in firn, leading to enhanced surface runoff and ice sheet mass loss. To date, ice slabs have primarily been mapped using airborne ice-penetrating radar, which has limited spatial and temporal coverage. This makes it...
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Online Access: | https://doi.org/10.5194/tc-18-2531-2024 https://tc.copernicus.org/articles/18/2531/2024/ |
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ftcopernicus:oai:publications.copernicus.org:tc115896 2024-06-23T07:53:14+00:00 Sentinel-1 detection of ice slabs on the Greenland Ice Sheet Culberg, Riley Michaelides, Roger J. Miller, Julie Z. 2024-05-23 application/pdf https://doi.org/10.5194/tc-18-2531-2024 https://tc.copernicus.org/articles/18/2531/2024/ eng eng doi:10.5194/tc-18-2531-2024 https://tc.copernicus.org/articles/18/2531/2024/ eISSN: 1994-0424 Text 2024 ftcopernicus https://doi.org/10.5194/tc-18-2531-2024 2024-06-13T01:24:17Z Ice slabs are multi-meter-thick layers of refrozen ice that limit meltwater storage in firn, leading to enhanced surface runoff and ice sheet mass loss. To date, ice slabs have primarily been mapped using airborne ice-penetrating radar, which has limited spatial and temporal coverage. This makes it difficult to fully assess the current extent and continuity of ice slabs or to validate predictive models of ice slab evolution that are key to understanding their impact on Greenland's surface mass balance. Here, for the first time, we map the extent of ice slabs and superimposed ice facies across the entire Greenland Ice Sheet at 500 m resolution using dual-polarization Sentinel-1 ( S-1 ) synthetic-aperture radar (SAR) data collected in winter 2016–2017. We do this by selecting empirical thresholds for the cross-polarized backscatter ratio and HV backscattered power that jointly optimize the agreement between airborne ice-penetrating radar data detections of ice slabs and the S-1 estimates of ice slab extent. Our results show that there is a strong correlation between C-band backscatter and the ice content of the upper ∼ 7 m of the firn column that enables ice slab mapping with S-1 . Our new mapping shows that ice slabs are nearly continuous around the entire margin of the ice sheet. This includes regions in southwest Greenland where ice slabs have not been previously identified by ice-penetrating radar but where the S-1 -inferred ice slab extent shows strong agreement with the extent of visible runoff mapped from optical imagery. The algorithm developed here lays the groundwork for the long-term monitoring of ice slab expansion with current and future C-band satellite systems and highlights the potential added value of future L-band missions for near-surface studies in Greenland. Text Greenland Ice Sheet Copernicus Publications: E-Journals Greenland The Cryosphere 18 5 2531 2555 |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
Ice slabs are multi-meter-thick layers of refrozen ice that limit meltwater storage in firn, leading to enhanced surface runoff and ice sheet mass loss. To date, ice slabs have primarily been mapped using airborne ice-penetrating radar, which has limited spatial and temporal coverage. This makes it difficult to fully assess the current extent and continuity of ice slabs or to validate predictive models of ice slab evolution that are key to understanding their impact on Greenland's surface mass balance. Here, for the first time, we map the extent of ice slabs and superimposed ice facies across the entire Greenland Ice Sheet at 500 m resolution using dual-polarization Sentinel-1 ( S-1 ) synthetic-aperture radar (SAR) data collected in winter 2016–2017. We do this by selecting empirical thresholds for the cross-polarized backscatter ratio and HV backscattered power that jointly optimize the agreement between airborne ice-penetrating radar data detections of ice slabs and the S-1 estimates of ice slab extent. Our results show that there is a strong correlation between C-band backscatter and the ice content of the upper ∼ 7 m of the firn column that enables ice slab mapping with S-1 . Our new mapping shows that ice slabs are nearly continuous around the entire margin of the ice sheet. This includes regions in southwest Greenland where ice slabs have not been previously identified by ice-penetrating radar but where the S-1 -inferred ice slab extent shows strong agreement with the extent of visible runoff mapped from optical imagery. The algorithm developed here lays the groundwork for the long-term monitoring of ice slab expansion with current and future C-band satellite systems and highlights the potential added value of future L-band missions for near-surface studies in Greenland. |
format |
Text |
author |
Culberg, Riley Michaelides, Roger J. Miller, Julie Z. |
spellingShingle |
Culberg, Riley Michaelides, Roger J. Miller, Julie Z. Sentinel-1 detection of ice slabs on the Greenland Ice Sheet |
author_facet |
Culberg, Riley Michaelides, Roger J. Miller, Julie Z. |
author_sort |
Culberg, Riley |
title |
Sentinel-1 detection of ice slabs on the Greenland Ice Sheet |
title_short |
Sentinel-1 detection of ice slabs on the Greenland Ice Sheet |
title_full |
Sentinel-1 detection of ice slabs on the Greenland Ice Sheet |
title_fullStr |
Sentinel-1 detection of ice slabs on the Greenland Ice Sheet |
title_full_unstemmed |
Sentinel-1 detection of ice slabs on the Greenland Ice Sheet |
title_sort |
sentinel-1 detection of ice slabs on the greenland ice sheet |
publishDate |
2024 |
url |
https://doi.org/10.5194/tc-18-2531-2024 https://tc.copernicus.org/articles/18/2531/2024/ |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Ice Sheet |
genre_facet |
Greenland Ice Sheet |
op_source |
eISSN: 1994-0424 |
op_relation |
doi:10.5194/tc-18-2531-2024 https://tc.copernicus.org/articles/18/2531/2024/ |
op_doi |
https://doi.org/10.5194/tc-18-2531-2024 |
container_title |
The Cryosphere |
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18 |
container_issue |
5 |
container_start_page |
2531 |
op_container_end_page |
2555 |
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1802644807402651648 |