Arctic sea surface height maps from multi-altimeter combination
We present a new Arctic sea level anomaly dataset based on the combination of three altimeter missions using an optimal interpolation scheme. Measurements from SARAL/AltiKa, CryoSat-2 and Sentinel-3A are blended together, providing an unprecedented resolution for this type of product. Such high-reso...
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ftdoajarticles:oai:doaj.org/article:702bd31bdcdc400a88e8665432954f68 2023-05-15T14:54:16+02:00 Arctic sea surface height maps from multi-altimeter combination P. Prandi J.-C. Poisson Y. Faugère A. Guillot G. Dibarboure 2021-11-01T00:00:00Z https://doi.org/10.5194/essd-13-5469-2021 https://doaj.org/article/702bd31bdcdc400a88e8665432954f68 EN eng Copernicus Publications https://essd.copernicus.org/articles/13/5469/2021/essd-13-5469-2021.pdf https://doaj.org/toc/1866-3508 https://doaj.org/toc/1866-3516 doi:10.5194/essd-13-5469-2021 1866-3508 1866-3516 https://doaj.org/article/702bd31bdcdc400a88e8665432954f68 Earth System Science Data, Vol 13, Pp 5469-5482 (2021) Environmental sciences GE1-350 Geology QE1-996.5 article 2021 ftdoajarticles https://doi.org/10.5194/essd-13-5469-2021 2022-12-31T09:00:22Z We present a new Arctic sea level anomaly dataset based on the combination of three altimeter missions using an optimal interpolation scheme. Measurements from SARAL/AltiKa, CryoSat-2 and Sentinel-3A are blended together, providing an unprecedented resolution for this type of product. Such high-resolution products are necessary to tackle some contemporaneous science questions in the basin. We use the adaptive retracker to process both open ocean and lead echoes on SARAL/AltiKa, thus removing the need to estimate a bias between open ocean and ice-covered areas. The usual processing approach, involving an empirical retracking algorithm on specular echoes, is applied on CryoSat-2 and Sentinel-3A synthetic aperture radar (SAR) mode echoes. SARAL/AltiKa also provides the baseline for the cross-calibration of CryoSat-2 and Sentinel-3A data. The final gridded fields cover all latitudes north of 50 ∘ N, on a 25 km EASE2 grid, with one grid every 3 d over 3 years from July 2016 to April 2019. When compared to tide gauge measurements available in the Arctic Ocean, the combined product exhibits a much better performance than mono-mission datasets with a mean correlation of 0.78 and a mean root-mean-square deviation (RMSd) of 5 cm . The effective temporal resolution of the combined product is 3 times better than a single mission analysis. This dataset can be downloaded from https://doi.org/10.24400/527896/a01-2020.001 ( Prandi , 2020 ) . Article in Journal/Newspaper Arctic Arctic Ocean ice covered areas Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Earth System Science Data 13 12 5469 5482 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Environmental sciences GE1-350 Geology QE1-996.5 |
spellingShingle |
Environmental sciences GE1-350 Geology QE1-996.5 P. Prandi J.-C. Poisson Y. Faugère A. Guillot G. Dibarboure Arctic sea surface height maps from multi-altimeter combination |
topic_facet |
Environmental sciences GE1-350 Geology QE1-996.5 |
description |
We present a new Arctic sea level anomaly dataset based on the combination of three altimeter missions using an optimal interpolation scheme. Measurements from SARAL/AltiKa, CryoSat-2 and Sentinel-3A are blended together, providing an unprecedented resolution for this type of product. Such high-resolution products are necessary to tackle some contemporaneous science questions in the basin. We use the adaptive retracker to process both open ocean and lead echoes on SARAL/AltiKa, thus removing the need to estimate a bias between open ocean and ice-covered areas. The usual processing approach, involving an empirical retracking algorithm on specular echoes, is applied on CryoSat-2 and Sentinel-3A synthetic aperture radar (SAR) mode echoes. SARAL/AltiKa also provides the baseline for the cross-calibration of CryoSat-2 and Sentinel-3A data. The final gridded fields cover all latitudes north of 50 ∘ N, on a 25 km EASE2 grid, with one grid every 3 d over 3 years from July 2016 to April 2019. When compared to tide gauge measurements available in the Arctic Ocean, the combined product exhibits a much better performance than mono-mission datasets with a mean correlation of 0.78 and a mean root-mean-square deviation (RMSd) of 5 cm . The effective temporal resolution of the combined product is 3 times better than a single mission analysis. This dataset can be downloaded from https://doi.org/10.24400/527896/a01-2020.001 ( Prandi , 2020 ) . |
format |
Article in Journal/Newspaper |
author |
P. Prandi J.-C. Poisson Y. Faugère A. Guillot G. Dibarboure |
author_facet |
P. Prandi J.-C. Poisson Y. Faugère A. Guillot G. Dibarboure |
author_sort |
P. Prandi |
title |
Arctic sea surface height maps from multi-altimeter combination |
title_short |
Arctic sea surface height maps from multi-altimeter combination |
title_full |
Arctic sea surface height maps from multi-altimeter combination |
title_fullStr |
Arctic sea surface height maps from multi-altimeter combination |
title_full_unstemmed |
Arctic sea surface height maps from multi-altimeter combination |
title_sort |
arctic sea surface height maps from multi-altimeter combination |
publisher |
Copernicus Publications |
publishDate |
2021 |
url |
https://doi.org/10.5194/essd-13-5469-2021 https://doaj.org/article/702bd31bdcdc400a88e8665432954f68 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean ice covered areas |
genre_facet |
Arctic Arctic Ocean ice covered areas |
op_source |
Earth System Science Data, Vol 13, Pp 5469-5482 (2021) |
op_relation |
https://essd.copernicus.org/articles/13/5469/2021/essd-13-5469-2021.pdf https://doaj.org/toc/1866-3508 https://doaj.org/toc/1866-3516 doi:10.5194/essd-13-5469-2021 1866-3508 1866-3516 https://doaj.org/article/702bd31bdcdc400a88e8665432954f68 |
op_doi |
https://doi.org/10.5194/essd-13-5469-2021 |
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Earth System Science Data |
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13 |
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12 |
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5469 |
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