Research

Glacier surface motion computation from digital image sequences


Reference:

Evans, A. N., 2000. Glacier surface motion computation from digital image sequences. IEEE Transactions on Geoscience and Remote Sensing, 38 (2), pp. 1064-1072.

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    Official URL:

    http://dx.doi.org/10.1109/36.841985

    Abstract

    A technique for computing the field of short-term glacier surface motion on a local scale is presented. Time-lapsed image negatives, digitized to a high resolution, provide the raw data for the three-stage technique. First, cross-correlation is used to establish a number of candidate displacement vectors for a series of regularly spaced templates. A relaxation-labeling routine is then applied to select the most appropriate candidate vectors, according to the local flow. Novel aspects of the relaxation algorithm include a new, efficient form of the support function and the absence of a null-match category. A new development is the application of a post filter to the resultant flow field, providing suitable displacement vectors for templates that were originally unmatched and correcting vectors that are still inconsistent with the local flow. Results from an image sequence from New Zealand's Mount Cook National Park show the superiority of the technique over the maximum cross-correlation method and demonstrate the effectiveness of the post filter in improving correlation-relaxation labeling

    Details

    Item Type Articles
    CreatorsEvans, A. N.
    DOI10.1109/36.841985
    DepartmentsFaculty of Engineering & Design > Electronic & Electrical Engineering
    Publisher StatementIEEETGRSMar2000.pdf: ©2000 IEEE. Personal use of this material is permitted. However, permission to reprint/republish this material for advertising or promotional purposes or for creating new collective works for resale or redistribution to servers or lists, or to reuse any copyrighted component of this work in other works must be obtained from the IEEE.
    RefereedYes
    StatusPublished
    ID Code14928

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