Classification of new-ice in the Greenland Sea using Satellite SSM/I radiometer and SeaWinds scatterometer data and comparison with ice model
In the ice covered waters of the Greenland Sea the polarisation ratio of QuikSCAT SeaWinds Ku-band (13.4 GHz) scatterometer measurements and the polarisation ratio of DMSP-SSM/I 19 GHz radiometer measurements are used in combination to classify new-ice and mature ice. In particular, the formation of...
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Language: | English |
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Online Access: | https://orbit.dtu.dk/en/publications/649ab47d-7441-472a-813b-2e64aee18352 https://doi.org/10.1016/j.rse.2005.05.012 |
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ftdtupubl:oai:pure.atira.dk:publications/649ab47d-7441-472a-813b-2e64aee18352 2023-05-15T16:26:21+02:00 Classification of new-ice in the Greenland Sea using Satellite SSM/I radiometer and SeaWinds scatterometer data and comparison with ice model Tonboe, Rasmus Pedersen, Leif Toudal 2005 https://orbit.dtu.dk/en/publications/649ab47d-7441-472a-813b-2e64aee18352 https://doi.org/10.1016/j.rse.2005.05.012 eng eng info:eu-repo/semantics/restrictedAccess Tonboe , R & Pedersen , L T 2005 , ' Classification of new-ice in the Greenland Sea using Satellite SSM/I radiometer and SeaWinds scatterometer data and comparison with ice model ' , Remote Sensing of Environment , vol. 97 , no. 3 , pp. 277-287 . https://doi.org/10.1016/j.rse.2005.05.012 article 2005 ftdtupubl https://doi.org/10.1016/j.rse.2005.05.012 2023-01-11T23:51:54Z In the ice covered waters of the Greenland Sea the polarisation ratio of QuikSCAT SeaWinds Ku-band (13.4 GHz) scatterometer measurements and the polarisation ratio of DMSP-SSM/I 19 GHz radiometer measurements are used in combination to classify new-ice and mature ice. In particular, the formation of the new-(frazil/pancake)-ice FOdden_ (8- W, 75- N) March 11th 18th, 2001, is used in the study. The results of the ice cover classification in the Greenland Sea are compared to model parameters from a sea ice model. The classification of each ice pixel is performed using its backscatter and radiative properties as reflected in the polarisation ratio. Our results based on these comparisons show that the transformation into older mature (sheet) ice occurs within 5 10 days. During one day the new-ice cover increased by 33000 km2. The new-ice appears in March 2001 as a peninsula (maximum extent 56000 km2) appended to the belt of older ice drifting along the East Coast of Greenland. These results are consistent with the ice model and with Radarsat images. Furthermore, using the ice model it is demonstrated that the new-ice/mature ice threshold in the classification corresponds to the physical transition of the ice cover from pancake ice to a consolidated young-ice sheet. The classification of each pixel into ice or water is done using two scatterometer parameters, namely the polarisation ratio and the daily standard deviation of the backscatter. In the ice covered waters of the Greenland Sea the polarisation ratio of QuikSCAT SeaWinds Ku-band (13.4 GHz) scatterometer measurements and the polarisation ratio of DMSP-SSM/I 19 GHz radiometer measurements are used in combination to classify new-ice and mature ice. In particular, the formation of the new-(frazil/pancake)-ice 'Odden' (8 degrees W, 75 degrees N) March 11th-18th, 2001, is used in the study. The results of the ice cover classification in the Greenland Sea are compared to model parameters from a sea ice model. The classification of each ice pixel is performed ... Article in Journal/Newspaper Greenland Greenland Sea Ice Sheet Sea ice ice covered waters Technical University of Denmark: DTU Orbit Greenland Pancake ENVELOPE(-55.815,-55.815,52.600,52.600) Remote Sensing of Environment 97 3 277 287 |
institution |
Open Polar |
collection |
Technical University of Denmark: DTU Orbit |
op_collection_id |
ftdtupubl |
language |
English |
description |
In the ice covered waters of the Greenland Sea the polarisation ratio of QuikSCAT SeaWinds Ku-band (13.4 GHz) scatterometer measurements and the polarisation ratio of DMSP-SSM/I 19 GHz radiometer measurements are used in combination to classify new-ice and mature ice. In particular, the formation of the new-(frazil/pancake)-ice FOdden_ (8- W, 75- N) March 11th 18th, 2001, is used in the study. The results of the ice cover classification in the Greenland Sea are compared to model parameters from a sea ice model. The classification of each ice pixel is performed using its backscatter and radiative properties as reflected in the polarisation ratio. Our results based on these comparisons show that the transformation into older mature (sheet) ice occurs within 5 10 days. During one day the new-ice cover increased by 33000 km2. The new-ice appears in March 2001 as a peninsula (maximum extent 56000 km2) appended to the belt of older ice drifting along the East Coast of Greenland. These results are consistent with the ice model and with Radarsat images. Furthermore, using the ice model it is demonstrated that the new-ice/mature ice threshold in the classification corresponds to the physical transition of the ice cover from pancake ice to a consolidated young-ice sheet. The classification of each pixel into ice or water is done using two scatterometer parameters, namely the polarisation ratio and the daily standard deviation of the backscatter. In the ice covered waters of the Greenland Sea the polarisation ratio of QuikSCAT SeaWinds Ku-band (13.4 GHz) scatterometer measurements and the polarisation ratio of DMSP-SSM/I 19 GHz radiometer measurements are used in combination to classify new-ice and mature ice. In particular, the formation of the new-(frazil/pancake)-ice 'Odden' (8 degrees W, 75 degrees N) March 11th-18th, 2001, is used in the study. The results of the ice cover classification in the Greenland Sea are compared to model parameters from a sea ice model. The classification of each ice pixel is performed ... |
format |
Article in Journal/Newspaper |
author |
Tonboe, Rasmus Pedersen, Leif Toudal |
spellingShingle |
Tonboe, Rasmus Pedersen, Leif Toudal Classification of new-ice in the Greenland Sea using Satellite SSM/I radiometer and SeaWinds scatterometer data and comparison with ice model |
author_facet |
Tonboe, Rasmus Pedersen, Leif Toudal |
author_sort |
Tonboe, Rasmus |
title |
Classification of new-ice in the Greenland Sea using Satellite SSM/I radiometer and SeaWinds scatterometer data and comparison with ice model |
title_short |
Classification of new-ice in the Greenland Sea using Satellite SSM/I radiometer and SeaWinds scatterometer data and comparison with ice model |
title_full |
Classification of new-ice in the Greenland Sea using Satellite SSM/I radiometer and SeaWinds scatterometer data and comparison with ice model |
title_fullStr |
Classification of new-ice in the Greenland Sea using Satellite SSM/I radiometer and SeaWinds scatterometer data and comparison with ice model |
title_full_unstemmed |
Classification of new-ice in the Greenland Sea using Satellite SSM/I radiometer and SeaWinds scatterometer data and comparison with ice model |
title_sort |
classification of new-ice in the greenland sea using satellite ssm/i radiometer and seawinds scatterometer data and comparison with ice model |
publishDate |
2005 |
url |
https://orbit.dtu.dk/en/publications/649ab47d-7441-472a-813b-2e64aee18352 https://doi.org/10.1016/j.rse.2005.05.012 |
long_lat |
ENVELOPE(-55.815,-55.815,52.600,52.600) |
geographic |
Greenland Pancake |
geographic_facet |
Greenland Pancake |
genre |
Greenland Greenland Sea Ice Sheet Sea ice ice covered waters |
genre_facet |
Greenland Greenland Sea Ice Sheet Sea ice ice covered waters |
op_source |
Tonboe , R & Pedersen , L T 2005 , ' Classification of new-ice in the Greenland Sea using Satellite SSM/I radiometer and SeaWinds scatterometer data and comparison with ice model ' , Remote Sensing of Environment , vol. 97 , no. 3 , pp. 277-287 . https://doi.org/10.1016/j.rse.2005.05.012 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1016/j.rse.2005.05.012 |
container_title |
Remote Sensing of Environment |
container_volume |
97 |
container_issue |
3 |
container_start_page |
277 |
op_container_end_page |
287 |
_version_ |
1766015260253224960 |