Estimating statistical errors in retrievals of ice velocity and deformation parameters from satellite images and buoy arrays

The objective of this note is to provide the background and basic tools to estimate the statistical error of deformation parameters that are calculated from displacement fields retrieved from synthetic aperture radar (SAR) imagery or from location changes of position sensors in an array. We focus he...

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Published in:The Cryosphere
Main Authors: Dierking, Wolfgang, Stern, Harry L., Hutchings, Jennifer K.
Format: Text
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.5194/tc-14-2999-2020
https://tc.copernicus.org/articles/14/2999/2020/
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spelling ftcopernicus:oai:publications.copernicus.org:tc82870 2023-05-15T18:18:32+02:00 Estimating statistical errors in retrievals of ice velocity and deformation parameters from satellite images and buoy arrays Dierking, Wolfgang Stern, Harry L. Hutchings, Jennifer K. 2020-09-15 application/pdf https://doi.org/10.5194/tc-14-2999-2020 https://tc.copernicus.org/articles/14/2999/2020/ eng eng doi:10.5194/tc-14-2999-2020 https://tc.copernicus.org/articles/14/2999/2020/ eISSN: 1994-0424 Text 2020 ftcopernicus https://doi.org/10.5194/tc-14-2999-2020 2020-09-21T16:22:14Z The objective of this note is to provide the background and basic tools to estimate the statistical error of deformation parameters that are calculated from displacement fields retrieved from synthetic aperture radar (SAR) imagery or from location changes of position sensors in an array. We focus here specifically on sea ice drift and deformation. In the most general case, the uncertainties of divergence/convergence, shear, vorticity, and total deformation are dependent on errors in coordinate measurements, the size of the area and the time interval over which these parameters are determined, as well as the velocity gradients within the boundary of the area. If displacements are calculated from sequences of SAR images, a tracking error also has to be considered. Timing errors in position readings are usually very small and can be neglected. We give examples for magnitudes of position and timing errors typical for buoys and SAR sensors, in the latter case supplemented by magnitudes of the tracking error, and apply the derived equations on geometric shapes frequently used for deriving deformation from SAR images and buoy arrays. Our case studies show that the size of the area and the time interval for calculating deformation parameters have to be chosen within certain limits to make sure that the uncertainties are smaller than the magnitude of deformation parameters. Text Sea ice Copernicus Publications: E-Journals The Cryosphere 14 9 2999 3016
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The objective of this note is to provide the background and basic tools to estimate the statistical error of deformation parameters that are calculated from displacement fields retrieved from synthetic aperture radar (SAR) imagery or from location changes of position sensors in an array. We focus here specifically on sea ice drift and deformation. In the most general case, the uncertainties of divergence/convergence, shear, vorticity, and total deformation are dependent on errors in coordinate measurements, the size of the area and the time interval over which these parameters are determined, as well as the velocity gradients within the boundary of the area. If displacements are calculated from sequences of SAR images, a tracking error also has to be considered. Timing errors in position readings are usually very small and can be neglected. We give examples for magnitudes of position and timing errors typical for buoys and SAR sensors, in the latter case supplemented by magnitudes of the tracking error, and apply the derived equations on geometric shapes frequently used for deriving deformation from SAR images and buoy arrays. Our case studies show that the size of the area and the time interval for calculating deformation parameters have to be chosen within certain limits to make sure that the uncertainties are smaller than the magnitude of deformation parameters.
format Text
author Dierking, Wolfgang
Stern, Harry L.
Hutchings, Jennifer K.
spellingShingle Dierking, Wolfgang
Stern, Harry L.
Hutchings, Jennifer K.
Estimating statistical errors in retrievals of ice velocity and deformation parameters from satellite images and buoy arrays
author_facet Dierking, Wolfgang
Stern, Harry L.
Hutchings, Jennifer K.
author_sort Dierking, Wolfgang
title Estimating statistical errors in retrievals of ice velocity and deformation parameters from satellite images and buoy arrays
title_short Estimating statistical errors in retrievals of ice velocity and deformation parameters from satellite images and buoy arrays
title_full Estimating statistical errors in retrievals of ice velocity and deformation parameters from satellite images and buoy arrays
title_fullStr Estimating statistical errors in retrievals of ice velocity and deformation parameters from satellite images and buoy arrays
title_full_unstemmed Estimating statistical errors in retrievals of ice velocity and deformation parameters from satellite images and buoy arrays
title_sort estimating statistical errors in retrievals of ice velocity and deformation parameters from satellite images and buoy arrays
publishDate 2020
url https://doi.org/10.5194/tc-14-2999-2020
https://tc.copernicus.org/articles/14/2999/2020/
genre Sea ice
genre_facet Sea ice
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-14-2999-2020
https://tc.copernicus.org/articles/14/2999/2020/
op_doi https://doi.org/10.5194/tc-14-2999-2020
container_title The Cryosphere
container_volume 14
container_issue 9
container_start_page 2999
op_container_end_page 3016
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