The Determination of Snow Albedo from Satellite Measurements Using Fast Atmospheric Correction Technique

We present a simplified atmospheric correction algorithm for snow/ice albedo retrievals using single view satellite measurements. The validation of the technique is performed using Ocean and Land Colour Instrument (OLCI) on board Copernicus Sentinel-3 satellite and ground spectral or broadband albed...

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Main Authors: Alexander Kokhanovsky, Jason E. Box, Baptiste Vandecrux, Kenneth D. Mankoff, Maxim Lamare, Alexander Smirnov, Michael Kern
Format: Article
Language:English
Published: MDPI AG 2020-01-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/12/2/234
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spelling doaj-740445e8469247aca292a3685139a7182020-11-25T02:13:32ZengMDPI AGRemote Sensing2072-42922020-01-0112223410.3390/rs12020234rs12020234The Determination of Snow Albedo from Satellite Measurements Using Fast Atmospheric Correction TechniqueAlexander Kokhanovsky0Jason E. Box1Baptiste Vandecrux2Kenneth D. Mankoff3Maxim Lamare4Alexander Smirnov5Michael Kern6VITROCISET, Bratustrasse 7, D-64293 Darmstadt, GermanyGeological Survey of Denmark and Greenland (GEUS), 1050K Copenhagen, DenmarkGeological Survey of Denmark and Greenland (GEUS), 1050K Copenhagen, DenmarkGeological Survey of Denmark and Greenland (GEUS), 1050K Copenhagen, DenmarkMétéo-France, CNRS, CNRM, Centre d’ Etudes de la Neige, 38400 Grenoble, FranceScience Systems and Applications, Inc., Lanham, MD 20706, USAApplications and Climate Department (EOP-SME), ESTEC/ESA, Science, 2200 AG Noordwijk, The NetherlandsWe present a simplified atmospheric correction algorithm for snow/ice albedo retrievals using single view satellite measurements. The validation of the technique is performed using Ocean and Land Colour Instrument (OLCI) on board Copernicus Sentinel-3 satellite and ground spectral or broadband albedo measurements from locations on the Greenland ice sheet and in the French Alps. Through comparison with independent ground observations, the technique is shown to perform accurately in a range of conditions from a 2100 m elevation mid-latitude location in the French Alps to a network of 15 locations across a 2390 m elevation range in seven regions across the Greenland ice sheet. Retrieved broadband albedo is accurate within 5% over a wide (0.5) broadband albedo range of the (N = 4155) Greenland observations and with no apparent bias.https://www.mdpi.com/2072-4292/12/2/234snow characteristicsoptical remote sensingsnow albedopromicesentinel 3olciatmospheric correctionarctic aerosol
collection DOAJ
language English
format Article
sources DOAJ
author Alexander Kokhanovsky
Jason E. Box
Baptiste Vandecrux
Kenneth D. Mankoff
Maxim Lamare
Alexander Smirnov
Michael Kern
spellingShingle Alexander Kokhanovsky
Jason E. Box
Baptiste Vandecrux
Kenneth D. Mankoff
Maxim Lamare
Alexander Smirnov
Michael Kern
The Determination of Snow Albedo from Satellite Measurements Using Fast Atmospheric Correction Technique
Remote Sensing
snow characteristics
optical remote sensing
snow albedo
promice
sentinel 3
olci
atmospheric correction
arctic aerosol
author_facet Alexander Kokhanovsky
Jason E. Box
Baptiste Vandecrux
Kenneth D. Mankoff
Maxim Lamare
Alexander Smirnov
Michael Kern
author_sort Alexander Kokhanovsky
title The Determination of Snow Albedo from Satellite Measurements Using Fast Atmospheric Correction Technique
title_short The Determination of Snow Albedo from Satellite Measurements Using Fast Atmospheric Correction Technique
title_full The Determination of Snow Albedo from Satellite Measurements Using Fast Atmospheric Correction Technique
title_fullStr The Determination of Snow Albedo from Satellite Measurements Using Fast Atmospheric Correction Technique
title_full_unstemmed The Determination of Snow Albedo from Satellite Measurements Using Fast Atmospheric Correction Technique
title_sort determination of snow albedo from satellite measurements using fast atmospheric correction technique
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2020-01-01
description We present a simplified atmospheric correction algorithm for snow/ice albedo retrievals using single view satellite measurements. The validation of the technique is performed using Ocean and Land Colour Instrument (OLCI) on board Copernicus Sentinel-3 satellite and ground spectral or broadband albedo measurements from locations on the Greenland ice sheet and in the French Alps. Through comparison with independent ground observations, the technique is shown to perform accurately in a range of conditions from a 2100 m elevation mid-latitude location in the French Alps to a network of 15 locations across a 2390 m elevation range in seven regions across the Greenland ice sheet. Retrieved broadband albedo is accurate within 5% over a wide (0.5) broadband albedo range of the (N = 4155) Greenland observations and with no apparent bias.
topic snow characteristics
optical remote sensing
snow albedo
promice
sentinel 3
olci
atmospheric correction
arctic aerosol
url https://www.mdpi.com/2072-4292/12/2/234
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