General Terms

In this work, we attempt to extend the body of knowledge on sea ice motion tracking in two specific directions. The first direction is the development of a computationally efficient, high resolution motion tracking system with a resolution of 400m, which is an order of magnitude greater than the cur...

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Main Authors: M. Thomas, C. Kambhamettu, C. A. Geiger
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.139.145
http://vims.cis.udel.edu/~mani/publications/ACMGIS08-sig-alternate.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.139.145 2023-05-15T18:17:50+02:00 General Terms M. Thomas C. Kambhamettu C. A. Geiger The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.139.145 http://vims.cis.udel.edu/~mani/publications/ACMGIS08-sig-alternate.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.139.145 http://vims.cis.udel.edu/~mani/publications/ACMGIS08-sig-alternate.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://vims.cis.udel.edu/~mani/publications/ACMGIS08-sig-alternate.pdf Design Algorithms Measurement Performance Keywords Cryosphere mapping near real time motion analysis Fourier theory discontinuity identification line integral convolution text ftciteseerx 2016-01-07T14:49:46Z In this work, we attempt to extend the body of knowledge on sea ice motion tracking in two specific directions. The first direction is the development of a computationally efficient, high resolution motion tracking system with a resolution of 400m, which is an order of magnitude greater than the currently available standard data products (3- 5km). Validation of this method using GPS measurements shows an average error that is less than 0.06cm/s. The second direction is the development of objective analysis technique to handle motion at close proximity to discontinuities. The goal of this second direction is to identify and track discontinuous features such as cracks, leads, ridges and other material damage zones. These developments allow motion to be estimated at a high resolution in a robust manner (validated against various noise models). With the observed changes in global climate, sparked by variations in the sea ice thickness and extent, our long term goal is to use this system to merge the “temporally rich ” GPS measurements with the “spatially rich ” measurements from satellite images. Categories and Subject Descriptors Text Sea ice Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic Design
Algorithms
Measurement
Performance Keywords Cryosphere
mapping
near real time motion analysis
Fourier theory
discontinuity identification
line integral convolution
spellingShingle Design
Algorithms
Measurement
Performance Keywords Cryosphere
mapping
near real time motion analysis
Fourier theory
discontinuity identification
line integral convolution
M. Thomas
C. Kambhamettu
C. A. Geiger
General Terms
topic_facet Design
Algorithms
Measurement
Performance Keywords Cryosphere
mapping
near real time motion analysis
Fourier theory
discontinuity identification
line integral convolution
description In this work, we attempt to extend the body of knowledge on sea ice motion tracking in two specific directions. The first direction is the development of a computationally efficient, high resolution motion tracking system with a resolution of 400m, which is an order of magnitude greater than the currently available standard data products (3- 5km). Validation of this method using GPS measurements shows an average error that is less than 0.06cm/s. The second direction is the development of objective analysis technique to handle motion at close proximity to discontinuities. The goal of this second direction is to identify and track discontinuous features such as cracks, leads, ridges and other material damage zones. These developments allow motion to be estimated at a high resolution in a robust manner (validated against various noise models). With the observed changes in global climate, sparked by variations in the sea ice thickness and extent, our long term goal is to use this system to merge the “temporally rich ” GPS measurements with the “spatially rich ” measurements from satellite images. Categories and Subject Descriptors
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author M. Thomas
C. Kambhamettu
C. A. Geiger
author_facet M. Thomas
C. Kambhamettu
C. A. Geiger
author_sort M. Thomas
title General Terms
title_short General Terms
title_full General Terms
title_fullStr General Terms
title_full_unstemmed General Terms
title_sort general terms
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.139.145
http://vims.cis.udel.edu/~mani/publications/ACMGIS08-sig-alternate.pdf
genre Sea ice
genre_facet Sea ice
op_source http://vims.cis.udel.edu/~mani/publications/ACMGIS08-sig-alternate.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.139.145
http://vims.cis.udel.edu/~mani/publications/ACMGIS08-sig-alternate.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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