Zonation des conditions d'enneigement en toundra forestière, Baie d'Hudson, Nouveau-Québec

Data on snow depth and snow density of various forest–tundra coniferous stands are presented in this paper. A latitudinal pattern in snow conditions is observed in the forest–tundra environment, as predicted from the facts that are obtained when this phytogeographical region is subdivided, firstly,...

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Published in:Canadian Journal of Botany
Main Authors: Payette, Serge, Ouzilleau, Jacques, Filion, Louise
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1975
Subjects:
Online Access:http://dx.doi.org/10.1139/b75-120
http://www.nrcresearchpress.com/doi/pdf/10.1139/b75-120
id crcansciencepubl:10.1139/b75-120
record_format openpolar
spelling crcansciencepubl:10.1139/b75-120 2023-12-17T10:27:37+01:00 Zonation des conditions d'enneigement en toundra forestière, Baie d'Hudson, Nouveau-Québec Payette, Serge Ouzilleau, Jacques Filion, Louise 1975 http://dx.doi.org/10.1139/b75-120 http://www.nrcresearchpress.com/doi/pdf/10.1139/b75-120 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Botany volume 53, issue 10, page 1021-1030 ISSN 0008-4026 Plant Science journal-article 1975 crcansciencepubl https://doi.org/10.1139/b75-120 2023-11-19T13:38:21Z Data on snow depth and snow density of various forest–tundra coniferous stands are presented in this paper. A latitudinal pattern in snow conditions is observed in the forest–tundra environment, as predicted from the facts that are obtained when this phytogeographical region is subdivided, firstly, into a forested subzone in the southern part and a shrub subzone (or krummholz) in the northern part and, secondly, into a maritime ecoclimatic area near Hudson Bay and a continental ecoclimatic area inland. The most snowy coniferous stands are located in the shrub subzone; snow density rises gradually from the taiga to the tundra. The highest values in snow properties are found in the maritime ecoclimatic area. These data suggest the following observations: (1) maximum snow depth measured in the northern part of the forest–tundra is explained by an increase of barren ground cover and by the presence of more open coniferous stands, which favor snow drifting and snow trapping; (2) the gradual increase in snow density is related to more rigorous climatic conditions; wind exposure is rather important since these sites are getting more open; and (3) the differences in snow conditions between the ecoclimatic areas show that the maritime environment is more windy; the presence of scattered and erected white spruce (Picea glauca (Moench) Voss) in various krummholz formations in that area favors more efficient snow traps than those of krummholz formations located in the continental area. The latter is dominated by prostrate and erect black spruce (Picea mariana (Mill.) BSP.) always densely agglomerated. The latitudinal pattern in snow conditions reflects the climatic conditions of the forest–tundra, and this determines the specific ecological distribution of coniferous stands. Article in Journal/Newspaper Baie d'Hudson Hudson Bay taiga toundra Tundra Canadian Science Publishing (via Crossref) Hudson Bay Hudson Baie d'Hudson ENVELOPE(-78.666,-78.666,58.417,58.417) Baie-d'Hudson ENVELOPE(-74.999,-74.999,58.500,58.500) Canadian Journal of Botany 53 10 1021 1030
institution Open Polar
collection Canadian Science Publishing (via Crossref)
op_collection_id crcansciencepubl
language English
topic Plant Science
spellingShingle Plant Science
Payette, Serge
Ouzilleau, Jacques
Filion, Louise
Zonation des conditions d'enneigement en toundra forestière, Baie d'Hudson, Nouveau-Québec
topic_facet Plant Science
description Data on snow depth and snow density of various forest–tundra coniferous stands are presented in this paper. A latitudinal pattern in snow conditions is observed in the forest–tundra environment, as predicted from the facts that are obtained when this phytogeographical region is subdivided, firstly, into a forested subzone in the southern part and a shrub subzone (or krummholz) in the northern part and, secondly, into a maritime ecoclimatic area near Hudson Bay and a continental ecoclimatic area inland. The most snowy coniferous stands are located in the shrub subzone; snow density rises gradually from the taiga to the tundra. The highest values in snow properties are found in the maritime ecoclimatic area. These data suggest the following observations: (1) maximum snow depth measured in the northern part of the forest–tundra is explained by an increase of barren ground cover and by the presence of more open coniferous stands, which favor snow drifting and snow trapping; (2) the gradual increase in snow density is related to more rigorous climatic conditions; wind exposure is rather important since these sites are getting more open; and (3) the differences in snow conditions between the ecoclimatic areas show that the maritime environment is more windy; the presence of scattered and erected white spruce (Picea glauca (Moench) Voss) in various krummholz formations in that area favors more efficient snow traps than those of krummholz formations located in the continental area. The latter is dominated by prostrate and erect black spruce (Picea mariana (Mill.) BSP.) always densely agglomerated. The latitudinal pattern in snow conditions reflects the climatic conditions of the forest–tundra, and this determines the specific ecological distribution of coniferous stands.
format Article in Journal/Newspaper
author Payette, Serge
Ouzilleau, Jacques
Filion, Louise
author_facet Payette, Serge
Ouzilleau, Jacques
Filion, Louise
author_sort Payette, Serge
title Zonation des conditions d'enneigement en toundra forestière, Baie d'Hudson, Nouveau-Québec
title_short Zonation des conditions d'enneigement en toundra forestière, Baie d'Hudson, Nouveau-Québec
title_full Zonation des conditions d'enneigement en toundra forestière, Baie d'Hudson, Nouveau-Québec
title_fullStr Zonation des conditions d'enneigement en toundra forestière, Baie d'Hudson, Nouveau-Québec
title_full_unstemmed Zonation des conditions d'enneigement en toundra forestière, Baie d'Hudson, Nouveau-Québec
title_sort zonation des conditions d'enneigement en toundra forestière, baie d'hudson, nouveau-québec
publisher Canadian Science Publishing
publishDate 1975
url http://dx.doi.org/10.1139/b75-120
http://www.nrcresearchpress.com/doi/pdf/10.1139/b75-120
long_lat ENVELOPE(-78.666,-78.666,58.417,58.417)
ENVELOPE(-74.999,-74.999,58.500,58.500)
geographic Hudson Bay
Hudson
Baie d'Hudson
Baie-d'Hudson
geographic_facet Hudson Bay
Hudson
Baie d'Hudson
Baie-d'Hudson
genre Baie d'Hudson
Hudson Bay
taiga
toundra
Tundra
genre_facet Baie d'Hudson
Hudson Bay
taiga
toundra
Tundra
op_source Canadian Journal of Botany
volume 53, issue 10, page 1021-1030
ISSN 0008-4026
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/b75-120
container_title Canadian Journal of Botany
container_volume 53
container_issue 10
container_start_page 1021
op_container_end_page 1030
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