Pan-Arctic Land Surface Temperature from MODIS and AATSR: Product Development and Intercomparison

Models and observations show that the Arctic is experiencing the most rapid changes in global near-surface air temperature. We developed novel EASE-grid Level 3 (L3) land surface temperature (LST) products from Level 2 (L2) AATSR and MODIS data to provide weekly, monthly and annual LST means over th...

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Published in:Remote Sensing
Main Authors: Aiman Soliman, Claude Duguay, William Saunders, Sonia Hachem
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2012
Subjects:
Q
Online Access:https://doi.org/10.3390/rs4123833
https://doaj.org/article/d49d0be97bca4d92aed33466114d7085
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spelling ftdoajarticles:oai:doaj.org/article:d49d0be97bca4d92aed33466114d7085 2023-05-15T14:47:05+02:00 Pan-Arctic Land Surface Temperature from MODIS and AATSR: Product Development and Intercomparison Aiman Soliman Claude Duguay William Saunders Sonia Hachem 2012-12-01T00:00:00Z https://doi.org/10.3390/rs4123833 https://doaj.org/article/d49d0be97bca4d92aed33466114d7085 EN eng MDPI AG http://www.mdpi.com/2072-4292/4/12/3833 https://doaj.org/toc/2072-4292 doi:10.3390/rs4123833 2072-4292 https://doaj.org/article/d49d0be97bca4d92aed33466114d7085 Remote Sensing, Vol 4, Iss 12, Pp 3833-3856 (2012) land surface temperature Arctic AATSR MODIS passive microwave atmospheric reanalysis Science Q article 2012 ftdoajarticles https://doi.org/10.3390/rs4123833 2022-12-30T20:32:59Z Models and observations show that the Arctic is experiencing the most rapid changes in global near-surface air temperature. We developed novel EASE-grid Level 3 (L3) land surface temperature (LST) products from Level 2 (L2) AATSR and MODIS data to provide weekly, monthly and annual LST means over the pan-Arctic region at various grid resolutions (1–25 km) for the past decade (2000–2010). In this paper, we provide: (1) a review of previous validation of MODIS/AATSR L2; (2) a description of the processing chain of L3 products; (3) an assessment of the 25 km products uncertainty, and; (4) a quantification of the bias introduced by over-representing clear-sky days in MODIS L3 products. In addition, we generated uncertainty maps by comparing L3 products with LST from passive microwave sensors (AMSR-E and SSM/I) and the North American Regional Reanalysis (NARR). Results show a close correspondence between MODIS and AATSR monthly products with a mean-difference (MD) of −1.1 K. Comparing L3 products with NARR indicates a close agreement in summer and a systematic bias in winter, which is entirely negative with respect to MODIS L3 (MD: −3.6, Min: −6.8, Max: −1 K). Comparing monthly averaged MODIS L3 to NARR clear-sky to quantify over-representing clear-sky days indicates a decrease of winter and an increase of summer difference compared to NARR all-sky. Finally, we provide suggestions to improve LST retrieval over Arctic regions. Article in Journal/Newspaper Arctic Directory of Open Access Journals: DOAJ Articles Arctic Remote Sensing 4 12 3833 3856
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic land surface temperature
Arctic
AATSR
MODIS
passive microwave
atmospheric reanalysis
Science
Q
spellingShingle land surface temperature
Arctic
AATSR
MODIS
passive microwave
atmospheric reanalysis
Science
Q
Aiman Soliman
Claude Duguay
William Saunders
Sonia Hachem
Pan-Arctic Land Surface Temperature from MODIS and AATSR: Product Development and Intercomparison
topic_facet land surface temperature
Arctic
AATSR
MODIS
passive microwave
atmospheric reanalysis
Science
Q
description Models and observations show that the Arctic is experiencing the most rapid changes in global near-surface air temperature. We developed novel EASE-grid Level 3 (L3) land surface temperature (LST) products from Level 2 (L2) AATSR and MODIS data to provide weekly, monthly and annual LST means over the pan-Arctic region at various grid resolutions (1–25 km) for the past decade (2000–2010). In this paper, we provide: (1) a review of previous validation of MODIS/AATSR L2; (2) a description of the processing chain of L3 products; (3) an assessment of the 25 km products uncertainty, and; (4) a quantification of the bias introduced by over-representing clear-sky days in MODIS L3 products. In addition, we generated uncertainty maps by comparing L3 products with LST from passive microwave sensors (AMSR-E and SSM/I) and the North American Regional Reanalysis (NARR). Results show a close correspondence between MODIS and AATSR monthly products with a mean-difference (MD) of −1.1 K. Comparing L3 products with NARR indicates a close agreement in summer and a systematic bias in winter, which is entirely negative with respect to MODIS L3 (MD: −3.6, Min: −6.8, Max: −1 K). Comparing monthly averaged MODIS L3 to NARR clear-sky to quantify over-representing clear-sky days indicates a decrease of winter and an increase of summer difference compared to NARR all-sky. Finally, we provide suggestions to improve LST retrieval over Arctic regions.
format Article in Journal/Newspaper
author Aiman Soliman
Claude Duguay
William Saunders
Sonia Hachem
author_facet Aiman Soliman
Claude Duguay
William Saunders
Sonia Hachem
author_sort Aiman Soliman
title Pan-Arctic Land Surface Temperature from MODIS and AATSR: Product Development and Intercomparison
title_short Pan-Arctic Land Surface Temperature from MODIS and AATSR: Product Development and Intercomparison
title_full Pan-Arctic Land Surface Temperature from MODIS and AATSR: Product Development and Intercomparison
title_fullStr Pan-Arctic Land Surface Temperature from MODIS and AATSR: Product Development and Intercomparison
title_full_unstemmed Pan-Arctic Land Surface Temperature from MODIS and AATSR: Product Development and Intercomparison
title_sort pan-arctic land surface temperature from modis and aatsr: product development and intercomparison
publisher MDPI AG
publishDate 2012
url https://doi.org/10.3390/rs4123833
https://doaj.org/article/d49d0be97bca4d92aed33466114d7085
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Remote Sensing, Vol 4, Iss 12, Pp 3833-3856 (2012)
op_relation http://www.mdpi.com/2072-4292/4/12/3833
https://doaj.org/toc/2072-4292
doi:10.3390/rs4123833
2072-4292
https://doaj.org/article/d49d0be97bca4d92aed33466114d7085
op_doi https://doi.org/10.3390/rs4123833
container_title Remote Sensing
container_volume 4
container_issue 12
container_start_page 3833
op_container_end_page 3856
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