Di Mauro, B.; Cogliati, S.; Bohn, N.; Traversa, G.; Garzonio, R.; Tagliabue, G.; Bramati, G.... (2024). Evaluation of PRISMA Products Over Snow in the Alps and Antarctica. EARTH AND SPACE SCIENCE. 11(7). https://doi.org/10.1029/2023EA003482
Por favor, use este identificador para citar o enlazar este ítem: http://hdl.handle.net/10251/209292
Título:
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Evaluation of PRISMA Products Over Snow in the Alps and Antarctica
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Autor:
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Di Mauro, Biagio
Cogliati, Sergio
Bohn, Niklas
Traversa, G.
Garzonio, R.
Tagliabue, Giulia
Bramati, G.
Cremonese, E.
Julitta, Tommaso
Guanter-Palomar, Luis María
Kokhanovsky, A.
Giardino, Claudia
Panigada, Cinzia
Rossini, Micol
Colombo, Roberto
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Entidad UPV:
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Universitat Politècnica de València. Escuela Técnica Superior de Ingenieros de Telecomunicación - Escola Tècnica Superior d'Enginyers de Telecomunicació
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Fecha difusión:
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Resumen:
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[EN] PRISMA is a hyperspectral satellite mission launched by the Italian Space Agency (ASI) in April 2019. The mission is designed to collect data at global scale for a variety of applications, including those related to ...[+]
[EN] PRISMA is a hyperspectral satellite mission launched by the Italian Space Agency (ASI) in April 2019. The mission is designed to collect data at global scale for a variety of applications, including those related to the cryosphere. This study presents an evaluation of PRISMA Level 1 (L1) and Level 2 (L2D) products for different snow conditions. To the aim, PRISMA data were collected at three sites: two in the Western European Alps (Torgnon and Plateau Rosa) and one in East Antarctica (Nansen Ice Shelf). PRISMA data were acquired contemporary to both field measurements and Sentinel-2 data. Simulated Top of the Atmosphere (TOA) radiance data were then compared to L1 PRISMA and Sentinel-2 TOA radiance. Bottom Of Atmosphere (BOA) reflectance from PRISMA L2D and Sentinel-2 L2A data were then evaluated by direct comparison with field data. Both TOA radiance and BOA reflectance PRISMA products were generally in good agreement with field data, showing a Mean Absolute Difference (MAD) lower than 5%. L1 PRISMA TOA radiance products resulted in higher MAD for the site of Torgnon, which features the highest topographic complexity within the investigated areas. In Plateau Rosa we obtained the best comparison between PRISMA L2D reflectance data and in situ measurements, with MAD values lower than 5% for the 400-900 nm range. The Nansen Ice Shelf instead resulted in MAD values <10% between PRISMA L2D and field data, while Sentinel-2 BOA reflectance showed higher values than other data sources. Plain Language Summary Satellite imaging spectroscopy data provide valuable information on Earth surface processes. In this study we evaluated data acquired from the PRISMA satellite mission in the Alps and Antarctica. Those studies are important to validate satellite observations with contemporary field measurements since they open the possibility of quantitatively use PRISMA data for cryosphere monitoring.
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Palabras clave:
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Snow
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Remote sensing
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Hyperspectral imaging
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Cal/val
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Spectroscopy
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PRISMA
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Derechos de uso:
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Reconocimiento - No comercial - Sin obra derivada (by-nc-nd)
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Fuente:
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EARTH AND SPACE SCIENCE. (eissn:
2333-5084
)
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DOI:
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10.1029/2023EA003482
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Editorial:
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American Geophysical Union
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Versión del editor:
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https://doi.org/10.1029/2023EA003482
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Código del Proyecto:
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info:eu-repo/grantAgreement/BMBF//50EE1923/
info:eu-repo/grantAgreement/MIUR//PNRA18_00222/
info:eu-repo/grantAgreement/NASA//80NM0018D0004/
info:eu-repo/grantAgreement/ASI//2019-5-HH.O/
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Agradecimientos:
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This research was funded by Agenzia Spaziale Italiana (ASI), in the context of PRISCAV project (Attivita scientifica di CAL/VAL della missione PRISMA) Grant 2019-5-HH.O. The Antarctic campaign was conducted within the ...[+]
This research was funded by Agenzia Spaziale Italiana (ASI), in the context of PRISCAV project (Attivita scientifica di CAL/VAL della missione PRISMA) Grant 2019-5-HH.O. The Antarctic campaign was conducted within the BioGeoAlbedo project (PNRA18_00222), funded by Programma Nazionale di Ricerca in Antartide (PNRA). Genesio L. (CNR-IBE), Matta E. (CNR-IRPI) and Pepe M. (CNR-IREA) are acknowledged for tasking PRISMA acquisitions. RoX data processing was made by using two R packages (FieldSpectrocospyCC and FieldSpectrocospyDP) available at . A. Kokhanovsky acknowledges the support of the EnMAP science program under the Space Agency at the DLR with resources from the German Federal Ministry of Economic Affairs and Climate Action (Grant 50EE1923). A portion of this research took place at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration (80NM0018D0004). Data/Information generated by Dr. Biagio Di Mauro under an ASI License to Use; Original PRISMA Product-(c) ASI-(2020, 2022).
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Tipo:
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Artículo
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