A dual-tube sampling technique for snowpack studies

The validity of any glaciological paleo proxy used to interpret climate records is based on the level of understanding of their transfer from the atmosphere into the ice sheet and their recording in the snowpack. Large spatial noise in snow properties is observed, as the wind constantly redistribute...

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Published in:Journal of Glaciology
Main Authors: Remi Dallmayr, Johannes Freitag, Maria Hörhold, Thomas Laepple, Johannes Lemburg, Damiano Della-Lunga, Frank Wilhelms
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2021
Subjects:
Online Access:https://doi.org/10.1017/jog.2020.85
https://doaj.org/article/a56a590acc1444d08f55741bedb7a399
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spelling ftdoajarticles:oai:doaj.org/article:a56a590acc1444d08f55741bedb7a399 2023-05-15T14:13:28+02:00 A dual-tube sampling technique for snowpack studies Remi Dallmayr Johannes Freitag Maria Hörhold Thomas Laepple Johannes Lemburg Damiano Della-Lunga Frank Wilhelms 2021-02-01T00:00:00Z https://doi.org/10.1017/jog.2020.85 https://doaj.org/article/a56a590acc1444d08f55741bedb7a399 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143020000854/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2020.85 0022-1430 1727-5652 https://doaj.org/article/a56a590acc1444d08f55741bedb7a399 Journal of Glaciology, Vol 67, Pp 84-90 (2021) Efficiency isotopic composition and topography sampling snowpack Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2021 ftdoajarticles https://doi.org/10.1017/jog.2020.85 2023-03-12T01:30:57Z The validity of any glaciological paleo proxy used to interpret climate records is based on the level of understanding of their transfer from the atmosphere into the ice sheet and their recording in the snowpack. Large spatial noise in snow properties is observed, as the wind constantly redistributes the deposited snow at the surface routed by the local topography. To increase the signal-to-noise ratio and getting a representative estimate of snow properties with respect to the high spatial variability, a large number of snow profiles is needed. However, the classical way of obtaining profiles via snow-pits is time and energy-consuming, and thus unfavourable for large surface sampling programs. In response, we present a dual-tube technique to sample the upper metre of the snowpack at a variable depth resolution with high efficiency. The developed device is robust and avoids contact with the samples by exhibiting two tubes attached alongside each other in order to (1) contain the snow core sample and (2) to access the bottom of the sample, respectively. We demonstrate the performance of the technique through two case studies in East Antarctica where we analysed the variability of water isotopes at a 100 m and 5 km spatial scales. Article in Journal/Newspaper Antarc* Antarctica East Antarctica Ice Sheet Journal of Glaciology Directory of Open Access Journals: DOAJ Articles East Antarctica Journal of Glaciology 67 261 84 90
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Efficiency
isotopic composition and topography
sampling
snowpack
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Efficiency
isotopic composition and topography
sampling
snowpack
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Remi Dallmayr
Johannes Freitag
Maria Hörhold
Thomas Laepple
Johannes Lemburg
Damiano Della-Lunga
Frank Wilhelms
A dual-tube sampling technique for snowpack studies
topic_facet Efficiency
isotopic composition and topography
sampling
snowpack
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description The validity of any glaciological paleo proxy used to interpret climate records is based on the level of understanding of their transfer from the atmosphere into the ice sheet and their recording in the snowpack. Large spatial noise in snow properties is observed, as the wind constantly redistributes the deposited snow at the surface routed by the local topography. To increase the signal-to-noise ratio and getting a representative estimate of snow properties with respect to the high spatial variability, a large number of snow profiles is needed. However, the classical way of obtaining profiles via snow-pits is time and energy-consuming, and thus unfavourable for large surface sampling programs. In response, we present a dual-tube technique to sample the upper metre of the snowpack at a variable depth resolution with high efficiency. The developed device is robust and avoids contact with the samples by exhibiting two tubes attached alongside each other in order to (1) contain the snow core sample and (2) to access the bottom of the sample, respectively. We demonstrate the performance of the technique through two case studies in East Antarctica where we analysed the variability of water isotopes at a 100 m and 5 km spatial scales.
format Article in Journal/Newspaper
author Remi Dallmayr
Johannes Freitag
Maria Hörhold
Thomas Laepple
Johannes Lemburg
Damiano Della-Lunga
Frank Wilhelms
author_facet Remi Dallmayr
Johannes Freitag
Maria Hörhold
Thomas Laepple
Johannes Lemburg
Damiano Della-Lunga
Frank Wilhelms
author_sort Remi Dallmayr
title A dual-tube sampling technique for snowpack studies
title_short A dual-tube sampling technique for snowpack studies
title_full A dual-tube sampling technique for snowpack studies
title_fullStr A dual-tube sampling technique for snowpack studies
title_full_unstemmed A dual-tube sampling technique for snowpack studies
title_sort dual-tube sampling technique for snowpack studies
publisher Cambridge University Press
publishDate 2021
url https://doi.org/10.1017/jog.2020.85
https://doaj.org/article/a56a590acc1444d08f55741bedb7a399
geographic East Antarctica
geographic_facet East Antarctica
genre Antarc*
Antarctica
East Antarctica
Ice Sheet
Journal of Glaciology
genre_facet Antarc*
Antarctica
East Antarctica
Ice Sheet
Journal of Glaciology
op_source Journal of Glaciology, Vol 67, Pp 84-90 (2021)
op_relation https://www.cambridge.org/core/product/identifier/S0022143020000854/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2020.85
0022-1430
1727-5652
https://doaj.org/article/a56a590acc1444d08f55741bedb7a399
op_doi https://doi.org/10.1017/jog.2020.85
container_title Journal of Glaciology
container_volume 67
container_issue 261
container_start_page 84
op_container_end_page 90
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