Impact of MODIS sensor calibration updates on Greenland Ice Sheet surface reflectance and albedo trends

We evaluate Greenland Ice Sheet (GrIS) surface reflectance and albedo trends using the newly released Collection 6 (C6) MODIS (Moderate Resolution Imaging Spectroradiometer) products over the period 2001–2016. We find that the correction of MODIS sensor degradation provided in the new C6 data produc...

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Main Authors: Casey, Kimberly A., Polashenski, Chris M., Chen, Justin, Tedesco, Marco
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Online Access:https://doi.org/10.7916/D8612BSF
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record_format openpolar
spelling ftcolumbiauniv:oai:academiccommons.columbia.edu:10.7916/D8612BSF 2023-05-15T16:27:11+02:00 Impact of MODIS sensor calibration updates on Greenland Ice Sheet surface reflectance and albedo trends Casey, Kimberly A. Polashenski, Chris M. Chen, Justin Tedesco, Marco 2017 https://doi.org/10.7916/D8612BSF English eng https://doi.org/10.7916/D8612BSF Cryosphere Ice sheets Albedo MODIS (Spectroradiometer) Articles 2017 ftcolumbiauniv https://doi.org/10.7916/D8612BSF 2019-04-04T08:17:04Z We evaluate Greenland Ice Sheet (GrIS) surface reflectance and albedo trends using the newly released Collection 6 (C6) MODIS (Moderate Resolution Imaging Spectroradiometer) products over the period 2001–2016. We find that the correction of MODIS sensor degradation provided in the new C6 data products reduces the magnitude of the surface reflectance and albedo decline trends obtained from previous MODIS data (i.e., Collection 5, C5). Collection 5 and 6 data product analysis over GrIS is characterized by surface (i.e., wet vs. dry) and elevation (i.e., 500–2000 m, 2000 m and greater) conditions over the summer season from 1 June to 31 August. Notably, the visible-wavelength declining reflectance trends identified in several bands of MODIS C5 data from previous studies are only slightly detected at reduced magnitude in the C6 versions over the dry snow area. Declining albedo in the wet snow and ice area remains over the MODIS record in the C6 product, albeit at a lower magnitude than obtained using C5 data. Further analyses of C6 spectral reflectance trends show both reflectance increases and decreases in select bands and regions, suggesting that several competing processes are contributing to Greenland Ice Sheet albedo change. Investigators using MODIS data for other ocean, atmosphere and/or land analyses are urged to consider similar re-examinations of trends previously established using C5 data. Article in Journal/Newspaper Greenland Ice Sheet Columbia University: Academic Commons Greenland
institution Open Polar
collection Columbia University: Academic Commons
op_collection_id ftcolumbiauniv
language English
topic Cryosphere
Ice sheets
Albedo
MODIS (Spectroradiometer)
spellingShingle Cryosphere
Ice sheets
Albedo
MODIS (Spectroradiometer)
Casey, Kimberly A.
Polashenski, Chris M.
Chen, Justin
Tedesco, Marco
Impact of MODIS sensor calibration updates on Greenland Ice Sheet surface reflectance and albedo trends
topic_facet Cryosphere
Ice sheets
Albedo
MODIS (Spectroradiometer)
description We evaluate Greenland Ice Sheet (GrIS) surface reflectance and albedo trends using the newly released Collection 6 (C6) MODIS (Moderate Resolution Imaging Spectroradiometer) products over the period 2001–2016. We find that the correction of MODIS sensor degradation provided in the new C6 data products reduces the magnitude of the surface reflectance and albedo decline trends obtained from previous MODIS data (i.e., Collection 5, C5). Collection 5 and 6 data product analysis over GrIS is characterized by surface (i.e., wet vs. dry) and elevation (i.e., 500–2000 m, 2000 m and greater) conditions over the summer season from 1 June to 31 August. Notably, the visible-wavelength declining reflectance trends identified in several bands of MODIS C5 data from previous studies are only slightly detected at reduced magnitude in the C6 versions over the dry snow area. Declining albedo in the wet snow and ice area remains over the MODIS record in the C6 product, albeit at a lower magnitude than obtained using C5 data. Further analyses of C6 spectral reflectance trends show both reflectance increases and decreases in select bands and regions, suggesting that several competing processes are contributing to Greenland Ice Sheet albedo change. Investigators using MODIS data for other ocean, atmosphere and/or land analyses are urged to consider similar re-examinations of trends previously established using C5 data.
format Article in Journal/Newspaper
author Casey, Kimberly A.
Polashenski, Chris M.
Chen, Justin
Tedesco, Marco
author_facet Casey, Kimberly A.
Polashenski, Chris M.
Chen, Justin
Tedesco, Marco
author_sort Casey, Kimberly A.
title Impact of MODIS sensor calibration updates on Greenland Ice Sheet surface reflectance and albedo trends
title_short Impact of MODIS sensor calibration updates on Greenland Ice Sheet surface reflectance and albedo trends
title_full Impact of MODIS sensor calibration updates on Greenland Ice Sheet surface reflectance and albedo trends
title_fullStr Impact of MODIS sensor calibration updates on Greenland Ice Sheet surface reflectance and albedo trends
title_full_unstemmed Impact of MODIS sensor calibration updates on Greenland Ice Sheet surface reflectance and albedo trends
title_sort impact of modis sensor calibration updates on greenland ice sheet surface reflectance and albedo trends
publishDate 2017
url https://doi.org/10.7916/D8612BSF
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_relation https://doi.org/10.7916/D8612BSF
op_doi https://doi.org/10.7916/D8612BSF
_version_ 1766016265037545472