@article{dac2a87f16144c10a4fba5bb3f6a1afe,
title = "Retrieval of Snow Properties from the Sentinel-3 Ocean and Land Colour Instrument",
abstract = "The Sentinel Application Platform (SNAP) architecture facilitates Earth Observation data processing. In this work, we present results from a new Snow Processor for SNAP. We also describe physical principles behind the developed snow property retrieval technique based on the analysis of Ocean and Land Colour Instrument (OLCI) onboard Sentinel-3A/B measurements over clean and polluted snow fields. Using OLCI spectral reflectance measurements in the range 400'1020 nm, we derived important snow properties such as spectral and broadband albedo, snow specific surface area, snow extent and grain size on a spatial grid of 300 m. The algorithm also incorporated cloud screening and atmospheric correction procedures over snow surfaces. We present validation results using ground measurements from Antarctica, the Greenland ice sheet and the French Alps. We find the spectral albedo retrieved with accuracy of better than 3% on average, making our retrievals sufficient for a variety of applications. Broadband albedo is retrieved with the average accuracy of about 5% over snow. Therefore, the uncertainties of satellite retrievals are close to experimental errors of ground measurements. The retrieved surface grain size shows good agreement with ground observations. Snow specific surface area observations are also consistent with our OLCI retrievals. We present snow albedo and grain size mapping over the inland ice sheet of Greenland for areas including dry snow, melted/melting snow and impurity rich bare ice. The algorithm can be applied to OLCI Sentinel-3 measurements providing an opportunity for creation of long-term snow property records essential for climate monitoring and data assimilation studies'especially in the Arctic region, where we face rapid environmental changes including reduction of snow/ice extent and, therefore, planetary albedo.",
keywords = "Albedo, OLCI, Optical remote sensing, Sentinel 3, Snow characteristics, Snow grain size, Specific surface area",
author = "Alexander Kokhanovsky and Maxim Lamare and Olaf Danne and Carsten Brockmann and Marie Dumont and Ghislain Picard and Laurent Arnaud and Vincent Favier and Bruno Jourdain and {Le Meur}, Emmanuel and {Di Mauro}, Biagio and Teruo Aoki and Masashi Niwano and Vladimir Rozanov and Serge Korkin and Sepp Kipfstuhl and Johannes Freitag and Maria Hoerhold and Alexander Zuhr and Diana Vladimirova and Anne-Katrine Faber and Steen-Larsen, {Hans Christian} and Sonja Wahl and Andersen, {Jonas K.} and Baptiste Vandecrux and {van As}, Dirk and Mankoff, {Kenneth D.} and Michael Kern and Eleonora Zege and Box, {Jason E.}",
note = "Funding Information: Acknowledgments: Agency (ESA) studies; the Scientific Exploitation of Operational Missions (SEOM) Sentinel-3 Snow (Sentinel-3 for Science, Land Study 1: Snow), ESRIN contract 4000118926/16/I-NB and the ESRIN contract 4000125043 - ESA/AO/1-9101/17/I-NB EO SCIENCE FOR SOCIETY. Additional support came from The Program for the Monitoring of the Greenland Ice Sheet (PROMICE), part of the Danish Energy Agency through the DANCEA program. The work of Sergey Korkin is supported by grant “NASA Science for Terra, Aqua and SNPP” (PI: Alexei Lyapustin, 17-TASNPP17-0116; solicitation NNH17ZDA001NTASNPP). EGRIP is directed and organized by the Center of Ice and Climate at the Niels Bohr Institute. It is supported by funding agencies and institutions in Denmark (A. P. M{\o}ller Foundation, UCPH), USA (US National Science Foundation, Office of Polar Programs), Germany (AWI), Japan (NIPR and ArCS), Norway (UiB and BFS), Switzerland (SNF), France (IPEV, IGE) and China (CAS and BNU). This work was conducted as a part of the GCOM-C/SGLI Project supported by the Japan Aerospace Exploration Agency (JAXA). The authors acknowledge the support from Agence Nationale de la Recherche Scientifique for the scientific traverse in Antarctica and the associated research: project ANR-14-CE01-0001 (ASUMA). The authors are grateful to S. Delwart and S. Warren for important discussions related to peculiarities of snow remote sensing from space and snow optical properties. Funding Information: This research has been funded by ESRINcontract 4000118926/16/I-NB and the ESRIN contract 4000125043-ESA/AO/1-9101/17/I-NB EO SCIENCE FOR SOCIETY. Agency (ESA) studies; the Scientific Exploitation of Operational Missions (SEOM) Sentinel-3 Snow (Sentinel-3 for Science, Land Study 1: Snow), ESRIN contract 4000118926/16/I-NB and the ESRIN contract 4000125043-ESA/AO/1-9101/17/I-NB EO SCIENCE FOR SOCIETY. Additional support came from The Program for the Monitoring of the Greenland Ice Sheet (PROMICE), part of the Danish Energy Agency through the DANCEA program. The work of Sergey Korkin is supported by grant 'NASA Science for Terra, Aqua and SNPP' (PI: Alexei Lyapustin, 17-TASNPP17-0116; solicitation NNH17ZDA001NTASNPP). EGRIP is directed and organized by the Center of Ice and Climate at the Niels Bohr Institute. It is supported by funding agencies and institutions in Denmark (A. P. M'ller Foundation, UCPH), USA (US National Science Foundation, Office of Polar Programs), Germany (AWI), Japan (NIPR and ArCS), Norway (UiB and BFS), Switzerland (SNF), France (IPEV, IGE) and China (CAS and BNU). This work was conducted as a part of theGCOM-C/SGLI Project supported by the Japan Aerospace Exploration Agency (JAXA). The authors acknowledge the support from Agence Nationale de la Recherche Scientifique for the scientific traverse in Antarctica and the associated research: project ANR-14-CE01-0001 (ASUMA). The authors are grateful to S. Delwart and S. Warren for important discussions related to peculiarities of snow remote sensing from space and snow optical properties. Publisher Copyright: {\textcopyright} 2019 by the authors.",
year = "2019",
month = oct,
day = "1",
doi = "10.3390/rs11192280",
language = "English",
volume = "11",
journal = "Remote Sensing",
issn = "2072-4292",
publisher = "MDPI",
number = "19",
}