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...
Published in: | The Cryosphere |
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Language: | English |
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Copernicus Publications
2022
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Online Access: | https://doi.org/10.5194/tc-16-3357-2022 https://doaj.org/article/8a3c44a330034d16869a74da08fd85a2 |
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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 |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English |
topic |
Environmental sciences GE1-350 Geology QE1-996.5 |
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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 |
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16 |
container_issue |
8 |
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3357 |
op_container_end_page |
3373 |
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1766341722455932928 |