Instantaneous Top-of-Atmosphere Albedo Comparison between CERES and MISR over the Arctic
The top-of-atmosphere (TOA) albedo is one of the key parameters in determining the Arctic radiation budget, with continued validation of its retrieval accuracy still required. Based on three years (2007, 2015, 2016) of summertime (May⁻September) observations from the Clouds and the Earth’s Radiant E...
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ftdoajarticles:oai:doaj.org/article:f2a45291ec694c658e4af8e544c7014c 2023-05-15T13:10:35+02:00 Instantaneous Top-of-Atmosphere Albedo Comparison between CERES and MISR over the Arctic Yizhe Zhan Larry Di Girolamo Roger Davies Catherine Moroney 2018-11-01T00:00:00Z https://doi.org/10.3390/rs10121882 https://doaj.org/article/f2a45291ec694c658e4af8e544c7014c EN eng MDPI AG https://www.mdpi.com/2072-4292/10/12/1882 https://doaj.org/toc/2072-4292 2072-4292 doi:10.3390/rs10121882 https://doaj.org/article/f2a45291ec694c658e4af8e544c7014c Remote Sensing, Vol 10, Iss 12, p 1882 (2018) Arctic top-of-atmosphere albedo CERES MISR Science Q article 2018 ftdoajarticles https://doi.org/10.3390/rs10121882 2022-12-31T10:53:39Z The top-of-atmosphere (TOA) albedo is one of the key parameters in determining the Arctic radiation budget, with continued validation of its retrieval accuracy still required. Based on three years (2007, 2015, 2016) of summertime (May⁻September) observations from the Clouds and the Earth’s Radiant Energy System (CERES) and the Multi-angle Imaging SpectroRadiometer (MISR), collocated instantaneous albedos for overcast ocean and snow/ice scenes were compared within the Arctic. For samples where both instruments classified the scene as overcast, the relative root-mean-square (RMS) difference between the sample albedos grew as the solar zenith angle (SZA) increased. The RMS differences that were purely due to differential Bidirectional Reflectance Factor (BRF) anisotropic corrections ( <math display="inline"> <semantics> <mrow> <msub> <mi>σ</mi> <mrow> <mi>A</mi> <mi>D</mi> <mi>M</mi> </mrow> </msub> </mrow> </semantics> </math> ) were estimated to be less than 4% for overcast ocean and overcast snow/ice when the SZA ≤ 70°. The significant agreement between the CERES and MISR strongly increased our confidence in using the instruments overcast cloud albedos in Arctic studies. Nevertheless, there was less agreement in the cloud albedos for larger solar zenith angles, where the RMS differences of <math display="inline"> <semantics> <mrow> <msub> <mi>σ</mi> <mrow> <mi>A</mi> <mi>D</mi> <mi>M</mi> </mrow> </msub> </mrow> </semantics> </math> reached 13.5% for overcast ocean scenes when the SZA > 80°. Additionally, inconsistencies between the CERES and MISR scene identifications were examined, resulting in an overall recommendation for improvements to the MISR snow/ice mask and a rework of the MISR Albedo Cloud Designation (ACD) field by incorporating known strengths of the standard MISR cloud masks. Article in Journal/Newspaper albedo Arctic Directory of Open Access Journals: DOAJ Articles Arctic Remote Sensing 10 12 1882 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Arctic top-of-atmosphere albedo CERES MISR Science Q |
spellingShingle |
Arctic top-of-atmosphere albedo CERES MISR Science Q Yizhe Zhan Larry Di Girolamo Roger Davies Catherine Moroney Instantaneous Top-of-Atmosphere Albedo Comparison between CERES and MISR over the Arctic |
topic_facet |
Arctic top-of-atmosphere albedo CERES MISR Science Q |
description |
The top-of-atmosphere (TOA) albedo is one of the key parameters in determining the Arctic radiation budget, with continued validation of its retrieval accuracy still required. Based on three years (2007, 2015, 2016) of summertime (May⁻September) observations from the Clouds and the Earth’s Radiant Energy System (CERES) and the Multi-angle Imaging SpectroRadiometer (MISR), collocated instantaneous albedos for overcast ocean and snow/ice scenes were compared within the Arctic. For samples where both instruments classified the scene as overcast, the relative root-mean-square (RMS) difference between the sample albedos grew as the solar zenith angle (SZA) increased. The RMS differences that were purely due to differential Bidirectional Reflectance Factor (BRF) anisotropic corrections ( <math display="inline"> <semantics> <mrow> <msub> <mi>σ</mi> <mrow> <mi>A</mi> <mi>D</mi> <mi>M</mi> </mrow> </msub> </mrow> </semantics> </math> ) were estimated to be less than 4% for overcast ocean and overcast snow/ice when the SZA ≤ 70°. The significant agreement between the CERES and MISR strongly increased our confidence in using the instruments overcast cloud albedos in Arctic studies. Nevertheless, there was less agreement in the cloud albedos for larger solar zenith angles, where the RMS differences of <math display="inline"> <semantics> <mrow> <msub> <mi>σ</mi> <mrow> <mi>A</mi> <mi>D</mi> <mi>M</mi> </mrow> </msub> </mrow> </semantics> </math> reached 13.5% for overcast ocean scenes when the SZA > 80°. Additionally, inconsistencies between the CERES and MISR scene identifications were examined, resulting in an overall recommendation for improvements to the MISR snow/ice mask and a rework of the MISR Albedo Cloud Designation (ACD) field by incorporating known strengths of the standard MISR cloud masks. |
format |
Article in Journal/Newspaper |
author |
Yizhe Zhan Larry Di Girolamo Roger Davies Catherine Moroney |
author_facet |
Yizhe Zhan Larry Di Girolamo Roger Davies Catherine Moroney |
author_sort |
Yizhe Zhan |
title |
Instantaneous Top-of-Atmosphere Albedo Comparison between CERES and MISR over the Arctic |
title_short |
Instantaneous Top-of-Atmosphere Albedo Comparison between CERES and MISR over the Arctic |
title_full |
Instantaneous Top-of-Atmosphere Albedo Comparison between CERES and MISR over the Arctic |
title_fullStr |
Instantaneous Top-of-Atmosphere Albedo Comparison between CERES and MISR over the Arctic |
title_full_unstemmed |
Instantaneous Top-of-Atmosphere Albedo Comparison between CERES and MISR over the Arctic |
title_sort |
instantaneous top-of-atmosphere albedo comparison between ceres and misr over the arctic |
publisher |
MDPI AG |
publishDate |
2018 |
url |
https://doi.org/10.3390/rs10121882 https://doaj.org/article/f2a45291ec694c658e4af8e544c7014c |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
albedo Arctic |
genre_facet |
albedo Arctic |
op_source |
Remote Sensing, Vol 10, Iss 12, p 1882 (2018) |
op_relation |
https://www.mdpi.com/2072-4292/10/12/1882 https://doaj.org/toc/2072-4292 2072-4292 doi:10.3390/rs10121882 https://doaj.org/article/f2a45291ec694c658e4af8e544c7014c |
op_doi |
https://doi.org/10.3390/rs10121882 |
container_title |
Remote Sensing |
container_volume |
10 |
container_issue |
12 |
container_start_page |
1882 |
_version_ |
1766235134331191296 |