An Inexpensive Remote Snow-Depth Gauge based on Ultrasonic Wave Reflection from the Snow Surface

Abstract Total snow depth is determined by measuring the time of flight of an ultrasonic wave packet emitted from a sonic transmitter above the snow surface and reflected from the snow surface back to the receiver/transmitter system. The light-weight system is battery powered (operating time without...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Gubler, H.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1981
Subjects:
Online Access:http://dx.doi.org/10.1017/s002214300001131x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300001131X
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spelling crcambridgeupr:10.1017/s002214300001131x 2024-09-15T18:15:39+00:00 An Inexpensive Remote Snow-Depth Gauge based on Ultrasonic Wave Reflection from the Snow Surface Gubler, H. 1981 http://dx.doi.org/10.1017/s002214300001131x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300001131X en eng Cambridge University Press (CUP) Journal of Glaciology volume 27, issue 95, page 157-163 ISSN 0022-1430 1727-5652 journal-article 1981 crcambridgeupr https://doi.org/10.1017/s002214300001131x 2024-07-03T04:04:11Z Abstract Total snow depth is determined by measuring the time of flight of an ultrasonic wave packet emitted from a sonic transmitter above the snow surface and reflected from the snow surface back to the receiver/transmitter system. The light-weight system is battery powered (operating time without battery change at least 8 months) and can be fixed to any post above the snow surface. The absolute precision is better than ±0.03 m. Data and commands are transmitted by a single two-wire system up to several kilometres. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 27 95 157 163
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Total snow depth is determined by measuring the time of flight of an ultrasonic wave packet emitted from a sonic transmitter above the snow surface and reflected from the snow surface back to the receiver/transmitter system. The light-weight system is battery powered (operating time without battery change at least 8 months) and can be fixed to any post above the snow surface. The absolute precision is better than ±0.03 m. Data and commands are transmitted by a single two-wire system up to several kilometres.
format Article in Journal/Newspaper
author Gubler, H.
spellingShingle Gubler, H.
An Inexpensive Remote Snow-Depth Gauge based on Ultrasonic Wave Reflection from the Snow Surface
author_facet Gubler, H.
author_sort Gubler, H.
title An Inexpensive Remote Snow-Depth Gauge based on Ultrasonic Wave Reflection from the Snow Surface
title_short An Inexpensive Remote Snow-Depth Gauge based on Ultrasonic Wave Reflection from the Snow Surface
title_full An Inexpensive Remote Snow-Depth Gauge based on Ultrasonic Wave Reflection from the Snow Surface
title_fullStr An Inexpensive Remote Snow-Depth Gauge based on Ultrasonic Wave Reflection from the Snow Surface
title_full_unstemmed An Inexpensive Remote Snow-Depth Gauge based on Ultrasonic Wave Reflection from the Snow Surface
title_sort inexpensive remote snow-depth gauge based on ultrasonic wave reflection from the snow surface
publisher Cambridge University Press (CUP)
publishDate 1981
url http://dx.doi.org/10.1017/s002214300001131x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300001131X
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 27, issue 95, page 157-163
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s002214300001131x
container_title Journal of Glaciology
container_volume 27
container_issue 95
container_start_page 157
op_container_end_page 163
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