BACK CALCULATION OF AVALANCHE DIMENSIONS FROM LASER SCANNING AND SFM- PHOTOGRAMMETRY

ABSTRACT: After avalanche events happen it is always difficult to collect useful data from the avalanche dimensions such as snow volume that was released in the avalanche starting zone, entrained in the track and deposited in the accumulation zone. Usually rapidly changing weather conditions or meas...

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Main Authors: Alexander Prokop, J.-M Friedt, Ursula Enzenhofer, Florian Tolle
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1045.1488
http://arc.lib.montana.edu/snow-science/objects/ISSW16_P4.35.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.1045.1488 2023-05-15T17:08:28+02:00 BACK CALCULATION OF AVALANCHE DIMENSIONS FROM LASER SCANNING AND SFM- PHOTOGRAMMETRY Alexander Prokop J.-M Friedt Ursula Enzenhofer Florian Tolle The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1045.1488 http://arc.lib.montana.edu/snow-science/objects/ISSW16_P4.35.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1045.1488 http://arc.lib.montana.edu/snow-science/objects/ISSW16_P4.35.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://arc.lib.montana.edu/snow-science/objects/ISSW16_P4.35.pdf text ftciteseerx 2020-04-05T00:17:08Z ABSTRACT: After avalanche events happen it is always difficult to collect useful data from the avalanche dimensions such as snow volume that was released in the avalanche starting zone, entrained in the track and deposited in the accumulation zone. Usually rapidly changing weather conditions or measures taken to remove the snow for emergency rescue preclude the possibility to collect useful data after the avalanche occurred. Snow depth data of the slopes involved prior to the avalanche basically never exists, if the avalanche was not artificially released for a scientific test. But such data is vitally important to calculate avalanche dynamic parameters and in tragic cases such as the avalanche that occurred in Longyearbyen Svalbard on December 19th 2015 for event documentation to improve hazard mapping. In this work we explain how it is possible using sfm-photogrammetry done using pictures from a simple smart phone camera or other cameras using a fixed objective in combination with terrestrial laser scanning to achieve such data. We discuss data accuracy we achieved investigating the Longyearbyen avalanche and explain a methodology that can be used for snow depth mapping for back calculation of avalanche events anywhere in the world. Text Longyearbyen Svalbard Unknown Longyearbyen Svalbard
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description ABSTRACT: After avalanche events happen it is always difficult to collect useful data from the avalanche dimensions such as snow volume that was released in the avalanche starting zone, entrained in the track and deposited in the accumulation zone. Usually rapidly changing weather conditions or measures taken to remove the snow for emergency rescue preclude the possibility to collect useful data after the avalanche occurred. Snow depth data of the slopes involved prior to the avalanche basically never exists, if the avalanche was not artificially released for a scientific test. But such data is vitally important to calculate avalanche dynamic parameters and in tragic cases such as the avalanche that occurred in Longyearbyen Svalbard on December 19th 2015 for event documentation to improve hazard mapping. In this work we explain how it is possible using sfm-photogrammetry done using pictures from a simple smart phone camera or other cameras using a fixed objective in combination with terrestrial laser scanning to achieve such data. We discuss data accuracy we achieved investigating the Longyearbyen avalanche and explain a methodology that can be used for snow depth mapping for back calculation of avalanche events anywhere in the world.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Alexander Prokop
J.-M Friedt
Ursula Enzenhofer
Florian Tolle
spellingShingle Alexander Prokop
J.-M Friedt
Ursula Enzenhofer
Florian Tolle
BACK CALCULATION OF AVALANCHE DIMENSIONS FROM LASER SCANNING AND SFM- PHOTOGRAMMETRY
author_facet Alexander Prokop
J.-M Friedt
Ursula Enzenhofer
Florian Tolle
author_sort Alexander Prokop
title BACK CALCULATION OF AVALANCHE DIMENSIONS FROM LASER SCANNING AND SFM- PHOTOGRAMMETRY
title_short BACK CALCULATION OF AVALANCHE DIMENSIONS FROM LASER SCANNING AND SFM- PHOTOGRAMMETRY
title_full BACK CALCULATION OF AVALANCHE DIMENSIONS FROM LASER SCANNING AND SFM- PHOTOGRAMMETRY
title_fullStr BACK CALCULATION OF AVALANCHE DIMENSIONS FROM LASER SCANNING AND SFM- PHOTOGRAMMETRY
title_full_unstemmed BACK CALCULATION OF AVALANCHE DIMENSIONS FROM LASER SCANNING AND SFM- PHOTOGRAMMETRY
title_sort back calculation of avalanche dimensions from laser scanning and sfm- photogrammetry
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1045.1488
http://arc.lib.montana.edu/snow-science/objects/ISSW16_P4.35.pdf
geographic Longyearbyen
Svalbard
geographic_facet Longyearbyen
Svalbard
genre Longyearbyen
Svalbard
genre_facet Longyearbyen
Svalbard
op_source http://arc.lib.montana.edu/snow-science/objects/ISSW16_P4.35.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1045.1488
http://arc.lib.montana.edu/snow-science/objects/ISSW16_P4.35.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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