Landsat 8 OLI Broadband Albedo Validation in Antarctica and Greenland

The albedo is a fundamental component of the processes that govern the energy budget, and particularly important in the context of climate change. However, a satellite-based high-resolution (30 m) albedo product which can be used in the polar regions up to 82.5° latitude during the summer seasons is...

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Published in:Remote Sensing
Main Authors: Giacomo Traversa, Davide Fugazza, Antonella Senese, Massimo Frezzotti
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/rs13040799
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spelling ftmdpi:oai:mdpi.com:/2072-4292/13/4/799/ 2023-08-20T04:01:31+02:00 Landsat 8 OLI Broadband Albedo Validation in Antarctica and Greenland Giacomo Traversa Davide Fugazza Antonella Senese Massimo Frezzotti agris 2021-02-22 application/pdf https://doi.org/10.3390/rs13040799 EN eng Multidisciplinary Digital Publishing Institute Remote Sensing in Geology, Geomorphology and Hydrology https://dx.doi.org/10.3390/rs13040799 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 13; Issue 4; Pages: 799 albedo remote sensing Landsat cryosphere polar regions Antarctica Greenland Text 2021 ftmdpi https://doi.org/10.3390/rs13040799 2023-08-01T01:07:19Z The albedo is a fundamental component of the processes that govern the energy budget, and particularly important in the context of climate change. However, a satellite-based high-resolution (30 m) albedo product which can be used in the polar regions up to 82.5° latitude during the summer seasons is lacking. To cover this gap, in this study we calculate satellite-based broadband albedo from Landsat 8 OLI and validate it against broadband albedo measurements from in situ stations located on the Antarctic and Greenland icesheets. The model to derive the albedo from raw satellite data includes an atmospheric and topographic correction and conversion from narrow-band to broadband albedo, and at each step different options were taken into account, in order to provide the best combination of corrections. Results, after being cleaned from anomalous data, show a good agreement with in situ albedo measurements, with a mean absolute error between in situ and satellite albedo of 0.021, a root mean square error of 0.026, a standard deviation of 0.015, a correlation coefficient of 0.995 (p < 0.01) and a bias estimate of −0.005. Considering the structure of the model, it could be applied to data from previous sensors of the Landsat family and help construct a record to analyze albedo variations in the polar regions. Text Antarc* Antarctic Antarctica Greenland MDPI Open Access Publishing Antarctic The Antarctic Greenland Remote Sensing 13 4 799
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic albedo
remote sensing
Landsat
cryosphere
polar regions
Antarctica
Greenland
spellingShingle albedo
remote sensing
Landsat
cryosphere
polar regions
Antarctica
Greenland
Giacomo Traversa
Davide Fugazza
Antonella Senese
Massimo Frezzotti
Landsat 8 OLI Broadband Albedo Validation in Antarctica and Greenland
topic_facet albedo
remote sensing
Landsat
cryosphere
polar regions
Antarctica
Greenland
description The albedo is a fundamental component of the processes that govern the energy budget, and particularly important in the context of climate change. However, a satellite-based high-resolution (30 m) albedo product which can be used in the polar regions up to 82.5° latitude during the summer seasons is lacking. To cover this gap, in this study we calculate satellite-based broadband albedo from Landsat 8 OLI and validate it against broadband albedo measurements from in situ stations located on the Antarctic and Greenland icesheets. The model to derive the albedo from raw satellite data includes an atmospheric and topographic correction and conversion from narrow-band to broadband albedo, and at each step different options were taken into account, in order to provide the best combination of corrections. Results, after being cleaned from anomalous data, show a good agreement with in situ albedo measurements, with a mean absolute error between in situ and satellite albedo of 0.021, a root mean square error of 0.026, a standard deviation of 0.015, a correlation coefficient of 0.995 (p < 0.01) and a bias estimate of −0.005. Considering the structure of the model, it could be applied to data from previous sensors of the Landsat family and help construct a record to analyze albedo variations in the polar regions.
format Text
author Giacomo Traversa
Davide Fugazza
Antonella Senese
Massimo Frezzotti
author_facet Giacomo Traversa
Davide Fugazza
Antonella Senese
Massimo Frezzotti
author_sort Giacomo Traversa
title Landsat 8 OLI Broadband Albedo Validation in Antarctica and Greenland
title_short Landsat 8 OLI Broadband Albedo Validation in Antarctica and Greenland
title_full Landsat 8 OLI Broadband Albedo Validation in Antarctica and Greenland
title_fullStr Landsat 8 OLI Broadband Albedo Validation in Antarctica and Greenland
title_full_unstemmed Landsat 8 OLI Broadband Albedo Validation in Antarctica and Greenland
title_sort landsat 8 oli broadband albedo validation in antarctica and greenland
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/rs13040799
op_coverage agris
geographic Antarctic
The Antarctic
Greenland
geographic_facet Antarctic
The Antarctic
Greenland
genre Antarc*
Antarctic
Antarctica
Greenland
genre_facet Antarc*
Antarctic
Antarctica
Greenland
op_source Remote Sensing; Volume 13; Issue 4; Pages: 799
op_relation Remote Sensing in Geology, Geomorphology and Hydrology
https://dx.doi.org/10.3390/rs13040799
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs13040799
container_title Remote Sensing
container_volume 13
container_issue 4
container_start_page 799
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