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1000 Titel
  • Sentinel-1 detection of ice slabs on the Greenland Ice Sheet
1000 Autor/in
  1. Culberg, Riley |
  2. Michaelides, Roger J. |
  3. Miller, Julie Z. |
1000 Verlag Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-05-23
1000 Erschienen in
1000 Quellenangabe
  • 18(5):2531-2555
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/tc-18-2531-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. 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. </jats:p>
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  1. https://orcid.org/0000-0002-4460-2359|https://frl.publisso.de/adhoc/uri/TWljaGFlbGlkZXMsIFJvZ2VyIEou|https://orcid.org/0000-0003-1452-1627
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  • DeepGreen-ID: 73683e594e4b4d2bb5846311026752b5 ; metadata provieded by: DeepGreen (https://www.oa-deepgreen.de/api/v1/), LIVIVO search scope life sciences (http://z3950.zbmed.de:6210/livivo), Crossref Unified Resource API (https://api.crossref.org/swagger-ui/index.html), to.science.api (https://frl.publisso.de/), ZDB JSON-API (beta) (https://zeitschriftendatenbank.de/api/), lobid - Dateninfrastruktur für Bibliotheken (https://lobid.org/resources/search)
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  1. National Aeronautics and Space Administration |
1000 Fördernummer
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1000 Förderprogramm
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1000 Dateien
  1. Sentinel-1 detection of ice slabs on the Greenland Ice Sheet
1000 Förderung
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    1000 Förderer National Aeronautics and Space Administration |
    1000 Förderprogramm -
    1000 Fördernummer -
1000 Objektart article
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1000 @id frl:6486683.rdf
1000 Erstellt am 2024-10-03T03:07:44.523+0200
1000 Erstellt von 322
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1000 Zuletzt bearbeitet 2025-08-13T23:29:55.341+0200
1000 Objekt bearb. Wed Aug 13 23:29:55 CEST 2025
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