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...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Authors: PHILIP CRIVELLI, ENRICO PATERNA, MICHAEL LEHNING
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2019
Subjects:
Online Access:https://doi.org/10.1017/jog.2019.3
https://doaj.org/article/c2ba9feaaf8a42a9a84a28d3cf6fa24b
id ftdoajarticles:oai:doaj.org/article:c2ba9feaaf8a42a9a84a28d3cf6fa24b
record_format openpolar
spelling 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