Impact of Sea Ice Drift Retrieval Errors, Discretization and Grid Type on Calculations of Ice Deformation

We studied two issues to be considered in the calculation of parameters characterizing sea ice deformation: the effect of uncertainties in an automatically retrieved sea ice drift field, and the influence of the type of drift vector grid. Sea ice deformation changes the local ice mass balance and th...

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Published in:Remote Sensing
Main Authors: Jakob Griebel, Wolfgang Dierking
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2018
Subjects:
SAR
Online Access:https://doi.org/10.3390/rs10030393
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spelling ftmdpi:oai:mdpi.com:/2072-4292/10/3/393/ 2023-10-09T21:55:51+02:00 Impact of Sea Ice Drift Retrieval Errors, Discretization and Grid Type on Calculations of Ice Deformation Jakob Griebel Wolfgang Dierking agris 2018-03-03 application/pdf https://doi.org/10.3390/rs10030393 eng eng Multidisciplinary Digital Publishing Institute Ocean Remote Sensing https://dx.doi.org/10.3390/rs10030393 https://creativecommons.org/licenses/by/4.0/ Remote Sensing Volume 10 Issue 3 Pages: 393 sea ice deformation drift SAR uncertainties error analysis Text 2018 ftmdpi https://doi.org/10.3390/rs10030393 2023-09-10T23:55:36Z We studied two issues to be considered in the calculation of parameters characterizing sea ice deformation: the effect of uncertainties in an automatically retrieved sea ice drift field, and the influence of the type of drift vector grid. Sea ice deformation changes the local ice mass balance and the interaction between atmosphere, ice, and ocean, and constitutes a hazard to marine traffic and operations. Due to numerical effects, the results of deformation retrievals may predict, e.g., openings and closings of the ice cover that do not exist in reality. We focus specifically on fields of ice drift obtained from synthetic aperture radar (SAR) imagery and analyze the Propagated Drift Retrieval Error (PDRE) and the Boundary Definition Error (BDE). From the theory of error propagation, the PDRE for the calculated deformation parameters can be estimated. To quantify the BDE, we devise five different grid types and compare theoretical expectation and numerical results for different deformation parameters assuming three scenarios: pure divergence, pure shear, and a mixture of both. Our findings for both sources of error help to set up optimal deformation retrieval schemes and are also useful for other applications working with vector fields and scalar parameters derived therefrom. Text Sea ice MDPI Open Access Publishing Remote Sensing 10 3 393
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic sea ice
deformation
drift
SAR
uncertainties
error analysis
spellingShingle sea ice
deformation
drift
SAR
uncertainties
error analysis
Jakob Griebel
Wolfgang Dierking
Impact of Sea Ice Drift Retrieval Errors, Discretization and Grid Type on Calculations of Ice Deformation
topic_facet sea ice
deformation
drift
SAR
uncertainties
error analysis
description We studied two issues to be considered in the calculation of parameters characterizing sea ice deformation: the effect of uncertainties in an automatically retrieved sea ice drift field, and the influence of the type of drift vector grid. Sea ice deformation changes the local ice mass balance and the interaction between atmosphere, ice, and ocean, and constitutes a hazard to marine traffic and operations. Due to numerical effects, the results of deformation retrievals may predict, e.g., openings and closings of the ice cover that do not exist in reality. We focus specifically on fields of ice drift obtained from synthetic aperture radar (SAR) imagery and analyze the Propagated Drift Retrieval Error (PDRE) and the Boundary Definition Error (BDE). From the theory of error propagation, the PDRE for the calculated deformation parameters can be estimated. To quantify the BDE, we devise five different grid types and compare theoretical expectation and numerical results for different deformation parameters assuming three scenarios: pure divergence, pure shear, and a mixture of both. Our findings for both sources of error help to set up optimal deformation retrieval schemes and are also useful for other applications working with vector fields and scalar parameters derived therefrom.
format Text
author Jakob Griebel
Wolfgang Dierking
author_facet Jakob Griebel
Wolfgang Dierking
author_sort Jakob Griebel
title Impact of Sea Ice Drift Retrieval Errors, Discretization and Grid Type on Calculations of Ice Deformation
title_short Impact of Sea Ice Drift Retrieval Errors, Discretization and Grid Type on Calculations of Ice Deformation
title_full Impact of Sea Ice Drift Retrieval Errors, Discretization and Grid Type on Calculations of Ice Deformation
title_fullStr Impact of Sea Ice Drift Retrieval Errors, Discretization and Grid Type on Calculations of Ice Deformation
title_full_unstemmed Impact of Sea Ice Drift Retrieval Errors, Discretization and Grid Type on Calculations of Ice Deformation
title_sort impact of sea ice drift retrieval errors, discretization and grid type on calculations of ice deformation
publisher Multidisciplinary Digital Publishing Institute
publishDate 2018
url https://doi.org/10.3390/rs10030393
op_coverage agris
genre Sea ice
genre_facet Sea ice
op_source Remote Sensing
Volume 10
Issue 3
Pages: 393
op_relation Ocean Remote Sensing
https://dx.doi.org/10.3390/rs10030393
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs10030393
container_title Remote Sensing
container_volume 10
container_issue 3
container_start_page 393
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