A comparison of current sea ice thickness products during the freeze-up period in the Arctic
2019 Living Planet Symposium, 13-17 May 2019, Milan, Italy Arctic sea ice is going through a dramatic change in its extent and volume at an unprecedented rate. A retreating Arctic sea ice cover has a marked impact on regional and global climate, through many feedback mechanisms and interactions with...
Main Authors: | , , , , , , , |
---|---|
Format: | Conference Object |
Language: | unknown |
Published: |
European Space Agency
2019
|
Subjects: | |
Online Access: | http://hdl.handle.net/10261/205002 |
id |
ftcsic:oai:digital.csic.es:10261/205002 |
---|---|
record_format |
openpolar |
spelling |
ftcsic:oai:digital.csic.es:10261/205002 2024-02-11T10:00:30+01:00 A comparison of current sea ice thickness products during the freeze-up period in the Arctic Sánchez-Gamez, Pablo Gabarró, Carolina Gupta, Mukesh Martínez, Justino Turiel, Antonio Portabella, Marcos González Gambau, Verónica Olmedo, Estrella 2019-05 http://hdl.handle.net/10261/205002 unknown European Space Agency Sí 2019 Living Planet Symposium (2019) http://hdl.handle.net/10261/205002 none comunicación de congreso http://purl.org/coar/resource_type/c_5794 2019 ftcsic 2024-01-16T10:50:36Z 2019 Living Planet Symposium, 13-17 May 2019, Milan, Italy Arctic sea ice is going through a dramatic change in its extent and volume at an unprecedented rate. A retreating Arctic sea ice cover has a marked impact on regional and global climate, through many feedback mechanisms and interactions with the climate system. It has been identified a clear reduction on the Arctic sea ice thickness within the last decades. Therefore, Sea Ice Thickness (SIT) monitoring is essential to better understand the changes the Arctic is experiencing. SIT can be measured with remote sensing platforms, mainly with the freeboard measurements from radar/laser altimeter instruments (only for ice thicker than 1 m (Laxon et al. 2013) and with L-band passive radiometers (only valid for the thin ice (Kaleschke et al. 2012)), making both instruments complementary. We present a new empirical algorithm that can retrieve SIT from Soil Moisture Ocean Salinity (SMOS) brightness temperatures (TB). Other SMOS SIT products which are currently being distributed use two different methodologies: one computes SIT based on theoretical sea ice models (Tian-Kunze et al. 2014), and the other uses a regression function with SIT data obtained from models (Huntemann et al. 2014). Therefore, this is the first time that the model function needed to derive the SIT has been obtained exclusively using in-situ SIT data from various field campaigns (i.e. Electromagnetic bird and Operation IceBridge) in the Arctic during 2011-2015. The available in-situ dataset has been divided into two groups, one is used to compute the model function and the other has been used to validate the SIT products. The computed SIT has a root-mean-square error of 0.24 m, which seems reasonably good for analysis at 25 km grid. Moreover, this algorithm minimizes the error produced by the difficulty on discriminating between TB signature of thin SIT versus the signature due to low sea ice concentration. The retrieved SIT is expected to serve as an operational product for data assimilation ... Conference Object Arctic Sea ice Digital.CSIC (Spanish National Research Council) Arctic |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
unknown |
description |
2019 Living Planet Symposium, 13-17 May 2019, Milan, Italy Arctic sea ice is going through a dramatic change in its extent and volume at an unprecedented rate. A retreating Arctic sea ice cover has a marked impact on regional and global climate, through many feedback mechanisms and interactions with the climate system. It has been identified a clear reduction on the Arctic sea ice thickness within the last decades. Therefore, Sea Ice Thickness (SIT) monitoring is essential to better understand the changes the Arctic is experiencing. SIT can be measured with remote sensing platforms, mainly with the freeboard measurements from radar/laser altimeter instruments (only for ice thicker than 1 m (Laxon et al. 2013) and with L-band passive radiometers (only valid for the thin ice (Kaleschke et al. 2012)), making both instruments complementary. We present a new empirical algorithm that can retrieve SIT from Soil Moisture Ocean Salinity (SMOS) brightness temperatures (TB). Other SMOS SIT products which are currently being distributed use two different methodologies: one computes SIT based on theoretical sea ice models (Tian-Kunze et al. 2014), and the other uses a regression function with SIT data obtained from models (Huntemann et al. 2014). Therefore, this is the first time that the model function needed to derive the SIT has been obtained exclusively using in-situ SIT data from various field campaigns (i.e. Electromagnetic bird and Operation IceBridge) in the Arctic during 2011-2015. The available in-situ dataset has been divided into two groups, one is used to compute the model function and the other has been used to validate the SIT products. The computed SIT has a root-mean-square error of 0.24 m, which seems reasonably good for analysis at 25 km grid. Moreover, this algorithm minimizes the error produced by the difficulty on discriminating between TB signature of thin SIT versus the signature due to low sea ice concentration. The retrieved SIT is expected to serve as an operational product for data assimilation ... |
format |
Conference Object |
author |
Sánchez-Gamez, Pablo Gabarró, Carolina Gupta, Mukesh Martínez, Justino Turiel, Antonio Portabella, Marcos González Gambau, Verónica Olmedo, Estrella |
spellingShingle |
Sánchez-Gamez, Pablo Gabarró, Carolina Gupta, Mukesh Martínez, Justino Turiel, Antonio Portabella, Marcos González Gambau, Verónica Olmedo, Estrella A comparison of current sea ice thickness products during the freeze-up period in the Arctic |
author_facet |
Sánchez-Gamez, Pablo Gabarró, Carolina Gupta, Mukesh Martínez, Justino Turiel, Antonio Portabella, Marcos González Gambau, Verónica Olmedo, Estrella |
author_sort |
Sánchez-Gamez, Pablo |
title |
A comparison of current sea ice thickness products during the freeze-up period in the Arctic |
title_short |
A comparison of current sea ice thickness products during the freeze-up period in the Arctic |
title_full |
A comparison of current sea ice thickness products during the freeze-up period in the Arctic |
title_fullStr |
A comparison of current sea ice thickness products during the freeze-up period in the Arctic |
title_full_unstemmed |
A comparison of current sea ice thickness products during the freeze-up period in the Arctic |
title_sort |
comparison of current sea ice thickness products during the freeze-up period in the arctic |
publisher |
European Space Agency |
publishDate |
2019 |
url |
http://hdl.handle.net/10261/205002 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Sea ice |
genre_facet |
Arctic Sea ice |
op_relation |
Sí 2019 Living Planet Symposium (2019) http://hdl.handle.net/10261/205002 |
op_rights |
none |
_version_ |
1790596210538577920 |