Empirical parametrization of Envisat freeboard retrieval of Arctic and Antarctic sea ice based on CryoSat-2: progress in the ESA Climate Change Initiative

In order to derive long-term changes in sea-ice volume, a multi-decadal sea-ice thickness record is required. CryoSat-2 has showcased the potential of radar altimetry for sea-ice mass-balance estimation over the recent years. However, precursor altimetry missions such as Environmental Satellite (Env...

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Published in:The Cryosphere
Main Authors: Paul, Stephan, Hendricks, Stefan, Ricker, Robert, Kern, Stefan, Rinne, Eero
Format: Text
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.5194/tc-12-2437-2018
https://tc.copernicus.org/articles/12/2437/2018/
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spelling ftcopernicus:oai:publications.copernicus.org:tc66690 2023-05-15T13:55:28+02:00 Empirical parametrization of Envisat freeboard retrieval of Arctic and Antarctic sea ice based on CryoSat-2: progress in the ESA Climate Change Initiative Paul, Stephan Hendricks, Stefan Ricker, Robert Kern, Stefan Rinne, Eero 2019-01-04 application/pdf https://doi.org/10.5194/tc-12-2437-2018 https://tc.copernicus.org/articles/12/2437/2018/ eng eng doi:10.5194/tc-12-2437-2018 https://tc.copernicus.org/articles/12/2437/2018/ eISSN: 1994-0424 Text 2019 ftcopernicus https://doi.org/10.5194/tc-12-2437-2018 2020-07-20T16:23:11Z In order to derive long-term changes in sea-ice volume, a multi-decadal sea-ice thickness record is required. CryoSat-2 has showcased the potential of radar altimetry for sea-ice mass-balance estimation over the recent years. However, precursor altimetry missions such as Environmental Satellite (Envisat) have not been exploited to the same extent so far. Combining both missions to acquire a decadal sea-ice volume data set requires a method to overcome the discrepancies due to different footprint sizes from either pulse-limited or beam-sharpened radar echoes. In this study, we implemented an inter-mission-consistent surface-type classification scheme for both hemispheres, based on the waveform pulse peakiness, leading-edge width, and surface backscatter. In order to achieve a consistent retracking procedure, we adapted the threshold first-maximum retracker algorithm, previously used only for CryoSat-2, to develop an adaptive retracker threshold that depends on waveform characteristics. With our method, we produce a global and consistent freeboard data set for CryoSat-2 and Envisat. This novel data set features a maximum monthly difference in the mission-overlap period of 2.2 cm (2.7 cm ) for the Arctic (Antarctic) based on all gridded values with spatial resolution of 25 km × 25 km and 50 km × 50 km for the Arctic and Antarctic, respectively. Text Antarc* Antarctic Arctic Climate change Sea ice Copernicus Publications: E-Journals Antarctic Arctic The Cryosphere 12 7 2437 2460
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description In order to derive long-term changes in sea-ice volume, a multi-decadal sea-ice thickness record is required. CryoSat-2 has showcased the potential of radar altimetry for sea-ice mass-balance estimation over the recent years. However, precursor altimetry missions such as Environmental Satellite (Envisat) have not been exploited to the same extent so far. Combining both missions to acquire a decadal sea-ice volume data set requires a method to overcome the discrepancies due to different footprint sizes from either pulse-limited or beam-sharpened radar echoes. In this study, we implemented an inter-mission-consistent surface-type classification scheme for both hemispheres, based on the waveform pulse peakiness, leading-edge width, and surface backscatter. In order to achieve a consistent retracking procedure, we adapted the threshold first-maximum retracker algorithm, previously used only for CryoSat-2, to develop an adaptive retracker threshold that depends on waveform characteristics. With our method, we produce a global and consistent freeboard data set for CryoSat-2 and Envisat. This novel data set features a maximum monthly difference in the mission-overlap period of 2.2 cm (2.7 cm ) for the Arctic (Antarctic) based on all gridded values with spatial resolution of 25 km × 25 km and 50 km × 50 km for the Arctic and Antarctic, respectively.
format Text
author Paul, Stephan
Hendricks, Stefan
Ricker, Robert
Kern, Stefan
Rinne, Eero
spellingShingle Paul, Stephan
Hendricks, Stefan
Ricker, Robert
Kern, Stefan
Rinne, Eero
Empirical parametrization of Envisat freeboard retrieval of Arctic and Antarctic sea ice based on CryoSat-2: progress in the ESA Climate Change Initiative
author_facet Paul, Stephan
Hendricks, Stefan
Ricker, Robert
Kern, Stefan
Rinne, Eero
author_sort Paul, Stephan
title Empirical parametrization of Envisat freeboard retrieval of Arctic and Antarctic sea ice based on CryoSat-2: progress in the ESA Climate Change Initiative
title_short Empirical parametrization of Envisat freeboard retrieval of Arctic and Antarctic sea ice based on CryoSat-2: progress in the ESA Climate Change Initiative
title_full Empirical parametrization of Envisat freeboard retrieval of Arctic and Antarctic sea ice based on CryoSat-2: progress in the ESA Climate Change Initiative
title_fullStr Empirical parametrization of Envisat freeboard retrieval of Arctic and Antarctic sea ice based on CryoSat-2: progress in the ESA Climate Change Initiative
title_full_unstemmed Empirical parametrization of Envisat freeboard retrieval of Arctic and Antarctic sea ice based on CryoSat-2: progress in the ESA Climate Change Initiative
title_sort empirical parametrization of envisat freeboard retrieval of arctic and antarctic sea ice based on cryosat-2: progress in the esa climate change initiative
publishDate 2019
url https://doi.org/10.5194/tc-12-2437-2018
https://tc.copernicus.org/articles/12/2437/2018/
geographic Antarctic
Arctic
geographic_facet Antarctic
Arctic
genre Antarc*
Antarctic
Arctic
Climate change
Sea ice
genre_facet Antarc*
Antarctic
Arctic
Climate change
Sea ice
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-12-2437-2018
https://tc.copernicus.org/articles/12/2437/2018/
op_doi https://doi.org/10.5194/tc-12-2437-2018
container_title The Cryosphere
container_volume 12
container_issue 7
container_start_page 2437
op_container_end_page 2460
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