Photogrammetry Applied to Avalanche Studies

Stereophotogrammetric techniques were used for a study of snow avalanches. The contour lines of the avalanche slope were mapped from stereo-photographs taken before and after the occurrence of the avalanche. The outline of the avalanche front at certain time intervals and the contours of the snow cl...

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Published in:Journal of Glaciology
Main Author: van Wijk, M. C.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1967
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000020219
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000020219
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spelling crcambridgeupr:10.1017/s0022143000020219 2024-09-15T18:15:37+00:00 Photogrammetry Applied to Avalanche Studies van Wijk, M. C. 1967 http://dx.doi.org/10.1017/s0022143000020219 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000020219 en eng Cambridge University Press (CUP) Journal of Glaciology volume 6, issue 48, page 917-933 ISSN 0022-1430 1727-5652 journal-article 1967 crcambridgeupr https://doi.org/10.1017/s0022143000020219 2024-07-24T04:03:07Z Stereophotogrammetric techniques were used for a study of snow avalanches. The contour lines of the avalanche slope were mapped from stereo-photographs taken before and after the occurrence of the avalanche. The outline of the avalanche front at certain time intervals and the contours of the snow cloud were also plotted. A relative accuracy for the different maps of 0.7 m. on the terrain was established. The volume of the snow cloud at four different stages of the avalanche was determined from the maps. These volumes were also computed independently from coordinate readings that were made in the stereo models. The standard errors of both methods of volume determination were estimated to be 450 m. 3 and 290 m. 3 respectively, representing errors of 5 per cent and 3 per cent of the average cloud volume. The photographs were taken with an accurately determined time interval. Therefore, the velocity of the avalanche front could be determined from the photogrammetric measurements. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 6 48 917 933
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Stereophotogrammetric techniques were used for a study of snow avalanches. The contour lines of the avalanche slope were mapped from stereo-photographs taken before and after the occurrence of the avalanche. The outline of the avalanche front at certain time intervals and the contours of the snow cloud were also plotted. A relative accuracy for the different maps of 0.7 m. on the terrain was established. The volume of the snow cloud at four different stages of the avalanche was determined from the maps. These volumes were also computed independently from coordinate readings that were made in the stereo models. The standard errors of both methods of volume determination were estimated to be 450 m. 3 and 290 m. 3 respectively, representing errors of 5 per cent and 3 per cent of the average cloud volume. The photographs were taken with an accurately determined time interval. Therefore, the velocity of the avalanche front could be determined from the photogrammetric measurements.
format Article in Journal/Newspaper
author van Wijk, M. C.
spellingShingle van Wijk, M. C.
Photogrammetry Applied to Avalanche Studies
author_facet van Wijk, M. C.
author_sort van Wijk, M. C.
title Photogrammetry Applied to Avalanche Studies
title_short Photogrammetry Applied to Avalanche Studies
title_full Photogrammetry Applied to Avalanche Studies
title_fullStr Photogrammetry Applied to Avalanche Studies
title_full_unstemmed Photogrammetry Applied to Avalanche Studies
title_sort photogrammetry applied to avalanche studies
publisher Cambridge University Press (CUP)
publishDate 1967
url http://dx.doi.org/10.1017/s0022143000020219
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000020219
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 6, issue 48, page 917-933
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000020219
container_title Journal of Glaciology
container_volume 6
container_issue 48
container_start_page 917
op_container_end_page 933
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