Snow properties at the forest–tundra ecotone: predominance of water vapor fluxes even in deep, moderately cold snowpacks

The forest–tundra ecotone is a large circumpolar transition zone between the Arctic tundra and the boreal forest, where snow properties are spatially variable due to changing vegetation. The extent of this biome through all circumpolar regions influences the climate. In the forest–tundra ecotone nea...

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Published in:The Cryosphere
Main Authors: G. Lackner, F. Domine, D. F. Nadeau, M. Lafaysse, M. Dumont
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
Online Access:https://doi.org/10.5194/tc-16-3357-2022
https://doaj.org/article/8a3c44a330034d16869a74da08fd85a2
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spelling ftdoajarticles:oai:doaj.org/article:8a3c44a330034d16869a74da08fd85a2 2023-05-15T15:10:46+02:00 Snow properties at the forest–tundra ecotone: predominance of water vapor fluxes even in deep, moderately cold snowpacks G. Lackner F. Domine D. F. Nadeau M. Lafaysse M. Dumont 2022-08-01T00:00:00Z https://doi.org/10.5194/tc-16-3357-2022 https://doaj.org/article/8a3c44a330034d16869a74da08fd85a2 EN eng Copernicus Publications https://tc.copernicus.org/articles/16/3357/2022/tc-16-3357-2022.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-16-3357-2022 1994-0416 1994-0424 https://doaj.org/article/8a3c44a330034d16869a74da08fd85a2 The Cryosphere, Vol 16, Pp 3357-3373 (2022) Environmental sciences GE1-350 Geology QE1-996.5 article 2022 ftdoajarticles https://doi.org/10.5194/tc-16-3357-2022 2022-12-30T23:42:44Z The forest–tundra ecotone is a large circumpolar transition zone between the Arctic tundra and the boreal forest, where snow properties are spatially variable due to changing vegetation. The extent of this biome through all circumpolar regions influences the climate. In the forest–tundra ecotone near Umiujaq in northeastern Canada ( <math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">56</mn><msup><mi/><mo>∘</mo></msup><msup><mn mathvariant="normal">33</mn><mo>′</mo></msup><msup><mn mathvariant="normal">31</mn><mrow><mo>′′</mo></mrow></msup></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="51pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="f1db1439419f1c115d33170bc9fc3b0e"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-3357-2022-ie00001.svg" width="51pt" height="11pt" src="tc-16-3357-2022-ie00001.png"/></svg:svg> N, <math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">76</mn><msup><mi/><mo>∘</mo></msup><msup><mn mathvariant="normal">28</mn><mo>′</mo></msup><msup><mn mathvariant="normal">56</mn><mrow><mo>′′</mo></mrow></msup></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="51pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="5933117e795b4e341763bad4c5c10a2e"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-3357-2022-ie00002.svg" width="51pt" height="11pt" src="tc-16-3357-2022-ie00002.png"/></svg:svg> W), we contrast the snow properties between two sites, TUNDRA (located in a low-shrub tundra) and ... Article in Journal/Newspaper Arctic The Cryosphere Tundra Umiujaq Directory of Open Access Journals: DOAJ Articles Arctic Canada Umiujaq ENVELOPE(-76.549,-76.549,56.553,56.553) The Cryosphere 16 8 3357 3373
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
G. Lackner
F. Domine
D. F. Nadeau
M. Lafaysse
M. Dumont
Snow properties at the forest–tundra ecotone: predominance of water vapor fluxes even in deep, moderately cold snowpacks
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description The forest–tundra ecotone is a large circumpolar transition zone between the Arctic tundra and the boreal forest, where snow properties are spatially variable due to changing vegetation. The extent of this biome through all circumpolar regions influences the climate. In the forest–tundra ecotone near Umiujaq in northeastern Canada ( <math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">56</mn><msup><mi/><mo>∘</mo></msup><msup><mn mathvariant="normal">33</mn><mo>′</mo></msup><msup><mn mathvariant="normal">31</mn><mrow><mo>′′</mo></mrow></msup></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="51pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="f1db1439419f1c115d33170bc9fc3b0e"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-3357-2022-ie00001.svg" width="51pt" height="11pt" src="tc-16-3357-2022-ie00001.png"/></svg:svg> N, <math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">76</mn><msup><mi/><mo>∘</mo></msup><msup><mn mathvariant="normal">28</mn><mo>′</mo></msup><msup><mn mathvariant="normal">56</mn><mrow><mo>′′</mo></mrow></msup></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="51pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="5933117e795b4e341763bad4c5c10a2e"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-3357-2022-ie00002.svg" width="51pt" height="11pt" src="tc-16-3357-2022-ie00002.png"/></svg:svg> W), we contrast the snow properties between two sites, TUNDRA (located in a low-shrub tundra) and ...
format Article in Journal/Newspaper
author G. Lackner
F. Domine
D. F. Nadeau
M. Lafaysse
M. Dumont
author_facet G. Lackner
F. Domine
D. F. Nadeau
M. Lafaysse
M. Dumont
author_sort G. Lackner
title Snow properties at the forest–tundra ecotone: predominance of water vapor fluxes even in deep, moderately cold snowpacks
title_short Snow properties at the forest–tundra ecotone: predominance of water vapor fluxes even in deep, moderately cold snowpacks
title_full Snow properties at the forest–tundra ecotone: predominance of water vapor fluxes even in deep, moderately cold snowpacks
title_fullStr Snow properties at the forest–tundra ecotone: predominance of water vapor fluxes even in deep, moderately cold snowpacks
title_full_unstemmed Snow properties at the forest–tundra ecotone: predominance of water vapor fluxes even in deep, moderately cold snowpacks
title_sort snow properties at the forest–tundra ecotone: predominance of water vapor fluxes even in deep, moderately cold snowpacks
publisher Copernicus Publications
publishDate 2022
url https://doi.org/10.5194/tc-16-3357-2022
https://doaj.org/article/8a3c44a330034d16869a74da08fd85a2
long_lat ENVELOPE(-76.549,-76.549,56.553,56.553)
geographic Arctic
Canada
Umiujaq
geographic_facet Arctic
Canada
Umiujaq
genre Arctic
The Cryosphere
Tundra
Umiujaq
genre_facet Arctic
The Cryosphere
Tundra
Umiujaq
op_source The Cryosphere, Vol 16, Pp 3357-3373 (2022)
op_relation https://tc.copernicus.org/articles/16/3357/2022/tc-16-3357-2022.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-16-3357-2022
1994-0416
1994-0424
https://doaj.org/article/8a3c44a330034d16869a74da08fd85a2
op_doi https://doi.org/10.5194/tc-16-3357-2022
container_title The Cryosphere
container_volume 16
container_issue 8
container_start_page 3357
op_container_end_page 3373
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