Spatiotemporal dynamics of snow erosion, deposition and horizontal mass flux
The quantification of snow transport, both in wind tunnels and the field, apply particle counting methods limited to punctual sampling of relatively small volumes. Particle counting can only capture horizontal mass fluxes, failing to measure snow erosion or deposition. Herein, we present a novel low...
Published in: | Journal of Glaciology |
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Language: | English |
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Cambridge University Press
2019
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Online Access: | https://doi.org/10.1017/jog.2019.3 https://doaj.org/article/c2ba9feaaf8a42a9a84a28d3cf6fa24b |
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ftdoajarticles:oai:doaj.org/article:c2ba9feaaf8a42a9a84a28d3cf6fa24b 2023-05-15T16:57:33+02:00 Spatiotemporal dynamics of snow erosion, deposition and horizontal mass flux PHILIP CRIVELLI ENRICO PATERNA MICHAEL LEHNING 2019-04-01T00:00:00Z https://doi.org/10.1017/jog.2019.3 https://doaj.org/article/c2ba9feaaf8a42a9a84a28d3cf6fa24b EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143019000030/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2019.3 0022-1430 1727-5652 https://doaj.org/article/c2ba9feaaf8a42a9a84a28d3cf6fa24b Journal of Glaciology, Vol 65, Pp 249-262 (2019) mass-balance reconstruction snow/ice surface processes wind-blown snow Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2019 ftdoajarticles https://doi.org/10.1017/jog.2019.3 2023-03-12T01:30:59Z The quantification of snow transport, both in wind tunnels and the field, apply particle counting methods limited to punctual sampling of relatively small volumes. Particle counting can only capture horizontal mass fluxes, failing to measure snow erosion or deposition. Herein, we present a novel low-cost sensor tool, based on a Microsoft Kinect, adapted to capture snow surface changes during snow drifting at unprecedented spatial and temporal resolutions. In the wind tunnel setting of these experiments we observe a balance between erosion and deposition at low wind speeds, while erosion is dominant at higher wind speeds. Significant differences in power spectral densities of surface mass flux and horizontal particle mass flux are observed. We show that for the saltation-length-scale parameter λ = 1, the integrated particle flux can be used to estimate the total surface mass flux in the wind tunnel. This provides an important basis to interpret mass flux measurements in the field. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 65 250 249 262 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
mass-balance reconstruction snow/ice surface processes wind-blown snow Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
mass-balance reconstruction snow/ice surface processes wind-blown snow Environmental sciences GE1-350 Meteorology. Climatology QC851-999 PHILIP CRIVELLI ENRICO PATERNA MICHAEL LEHNING Spatiotemporal dynamics of snow erosion, deposition and horizontal mass flux |
topic_facet |
mass-balance reconstruction snow/ice surface processes wind-blown snow Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
The quantification of snow transport, both in wind tunnels and the field, apply particle counting methods limited to punctual sampling of relatively small volumes. Particle counting can only capture horizontal mass fluxes, failing to measure snow erosion or deposition. Herein, we present a novel low-cost sensor tool, based on a Microsoft Kinect, adapted to capture snow surface changes during snow drifting at unprecedented spatial and temporal resolutions. In the wind tunnel setting of these experiments we observe a balance between erosion and deposition at low wind speeds, while erosion is dominant at higher wind speeds. Significant differences in power spectral densities of surface mass flux and horizontal particle mass flux are observed. We show that for the saltation-length-scale parameter λ = 1, the integrated particle flux can be used to estimate the total surface mass flux in the wind tunnel. This provides an important basis to interpret mass flux measurements in the field. |
format |
Article in Journal/Newspaper |
author |
PHILIP CRIVELLI ENRICO PATERNA MICHAEL LEHNING |
author_facet |
PHILIP CRIVELLI ENRICO PATERNA MICHAEL LEHNING |
author_sort |
PHILIP CRIVELLI |
title |
Spatiotemporal dynamics of snow erosion, deposition and horizontal mass flux |
title_short |
Spatiotemporal dynamics of snow erosion, deposition and horizontal mass flux |
title_full |
Spatiotemporal dynamics of snow erosion, deposition and horizontal mass flux |
title_fullStr |
Spatiotemporal dynamics of snow erosion, deposition and horizontal mass flux |
title_full_unstemmed |
Spatiotemporal dynamics of snow erosion, deposition and horizontal mass flux |
title_sort |
spatiotemporal dynamics of snow erosion, deposition and horizontal mass flux |
publisher |
Cambridge University Press |
publishDate |
2019 |
url |
https://doi.org/10.1017/jog.2019.3 https://doaj.org/article/c2ba9feaaf8a42a9a84a28d3cf6fa24b |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology, Vol 65, Pp 249-262 (2019) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143019000030/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2019.3 0022-1430 1727-5652 https://doaj.org/article/c2ba9feaaf8a42a9a84a28d3cf6fa24b |
op_doi |
https://doi.org/10.1017/jog.2019.3 |
container_title |
Journal of Glaciology |
container_volume |
65 |
container_issue |
250 |
container_start_page |
249 |
op_container_end_page |
262 |
_version_ |
1766049115046674432 |