Effects of meteorology and soil moisture on the spatio-temporal evolution of the depth hoar layer in the polar desert snowpack
In polar deserts, depth hoar (hereinafter: DH) growth is not systematic unlike on tundra and this is critical for snowpack properties. Here, we address the spatio-temporal variability of the DH layer in the polar desert at two sites in the Canadian High Arctic: Ward Hunt Island (83° N) and Resolute...
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Cambridge University Press
2022
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Online Access: | https://doi.org/10.1017/jog.2021.105 https://doaj.org/article/a738ca8fa0fb4a3396ccd7d7deb5358e |
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ftdoajarticles:oai:doaj.org/article:a738ca8fa0fb4a3396ccd7d7deb5358e 2023-05-15T14:57:47+02:00 Effects of meteorology and soil moisture on the spatio-temporal evolution of the depth hoar layer in the polar desert snowpack Gautier Davesne Florent Domine Daniel Fortier 2022-06-01T00:00:00Z https://doi.org/10.1017/jog.2021.105 https://doaj.org/article/a738ca8fa0fb4a3396ccd7d7deb5358e EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143021001052/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2021.105 0022-1430 1727-5652 https://doaj.org/article/a738ca8fa0fb4a3396ccd7d7deb5358e Journal of Glaciology, Vol 68, Pp 457-472 (2022) Arctic snowpack depth hoar polar desert soil moisture thermal conductivity Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2022 ftdoajarticles https://doi.org/10.1017/jog.2021.105 2023-03-12T01:30:54Z In polar deserts, depth hoar (hereinafter: DH) growth is not systematic unlike on tundra and this is critical for snowpack properties. Here, we address the spatio-temporal variability of the DH layer in the polar desert at two sites in the Canadian High Arctic: Ward Hunt Island (83° N) and Resolute Bay (75° N). Our data show that, over humid areas, DH represented a larger fraction of the snowpack and was characterized by lower density and coarser crystals than over dry gravelly areas. Increased soil moisture extends the zero-curtain period during freeze-up, leading to stronger temperature gradients in the snowpack and greater kinetic metamorphism. Our results also demonstrate that the large inter-annual variability in DH is primarily driven by wind conditions in the fall since this key variable controls the initial snow density and snow onset date. These strong controls exerted by soil moisture and meteorological conditions on DH growth in polar deserts highlight the possibility of major changes in polar snowpacks physical properties in response to the rapid climate and environmental changes currently affecting these regions. Article in Journal/Newspaper Arctic Journal of Glaciology polar desert Resolute Bay Tundra Ward Hunt Island Directory of Open Access Journals: DOAJ Articles Arctic Hunt Island ENVELOPE(-100.601,-100.601,58.788,58.788) Resolute Bay ENVELOPE(-94.842,-94.842,74.677,74.677) Ward Hunt Island ENVELOPE(-74.161,-74.161,83.102,83.102) Journal of Glaciology 68 269 457 472 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Arctic snowpack depth hoar polar desert soil moisture thermal conductivity Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
Arctic snowpack depth hoar polar desert soil moisture thermal conductivity Environmental sciences GE1-350 Meteorology. Climatology QC851-999 Gautier Davesne Florent Domine Daniel Fortier Effects of meteorology and soil moisture on the spatio-temporal evolution of the depth hoar layer in the polar desert snowpack |
topic_facet |
Arctic snowpack depth hoar polar desert soil moisture thermal conductivity Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
In polar deserts, depth hoar (hereinafter: DH) growth is not systematic unlike on tundra and this is critical for snowpack properties. Here, we address the spatio-temporal variability of the DH layer in the polar desert at two sites in the Canadian High Arctic: Ward Hunt Island (83° N) and Resolute Bay (75° N). Our data show that, over humid areas, DH represented a larger fraction of the snowpack and was characterized by lower density and coarser crystals than over dry gravelly areas. Increased soil moisture extends the zero-curtain period during freeze-up, leading to stronger temperature gradients in the snowpack and greater kinetic metamorphism. Our results also demonstrate that the large inter-annual variability in DH is primarily driven by wind conditions in the fall since this key variable controls the initial snow density and snow onset date. These strong controls exerted by soil moisture and meteorological conditions on DH growth in polar deserts highlight the possibility of major changes in polar snowpacks physical properties in response to the rapid climate and environmental changes currently affecting these regions. |
format |
Article in Journal/Newspaper |
author |
Gautier Davesne Florent Domine Daniel Fortier |
author_facet |
Gautier Davesne Florent Domine Daniel Fortier |
author_sort |
Gautier Davesne |
title |
Effects of meteorology and soil moisture on the spatio-temporal evolution of the depth hoar layer in the polar desert snowpack |
title_short |
Effects of meteorology and soil moisture on the spatio-temporal evolution of the depth hoar layer in the polar desert snowpack |
title_full |
Effects of meteorology and soil moisture on the spatio-temporal evolution of the depth hoar layer in the polar desert snowpack |
title_fullStr |
Effects of meteorology and soil moisture on the spatio-temporal evolution of the depth hoar layer in the polar desert snowpack |
title_full_unstemmed |
Effects of meteorology and soil moisture on the spatio-temporal evolution of the depth hoar layer in the polar desert snowpack |
title_sort |
effects of meteorology and soil moisture on the spatio-temporal evolution of the depth hoar layer in the polar desert snowpack |
publisher |
Cambridge University Press |
publishDate |
2022 |
url |
https://doi.org/10.1017/jog.2021.105 https://doaj.org/article/a738ca8fa0fb4a3396ccd7d7deb5358e |
long_lat |
ENVELOPE(-100.601,-100.601,58.788,58.788) ENVELOPE(-94.842,-94.842,74.677,74.677) ENVELOPE(-74.161,-74.161,83.102,83.102) |
geographic |
Arctic Hunt Island Resolute Bay Ward Hunt Island |
geographic_facet |
Arctic Hunt Island Resolute Bay Ward Hunt Island |
genre |
Arctic Journal of Glaciology polar desert Resolute Bay Tundra Ward Hunt Island |
genre_facet |
Arctic Journal of Glaciology polar desert Resolute Bay Tundra Ward Hunt Island |
op_source |
Journal of Glaciology, Vol 68, Pp 457-472 (2022) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143021001052/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2021.105 0022-1430 1727-5652 https://doaj.org/article/a738ca8fa0fb4a3396ccd7d7deb5358e |
op_doi |
https://doi.org/10.1017/jog.2021.105 |
container_title |
Journal of Glaciology |
container_volume |
68 |
container_issue |
269 |
container_start_page |
457 |
op_container_end_page |
472 |
_version_ |
1766329905406017536 |