How do climate and topography influence the greening of the forest‐tundra ecotone in northern Québec? A dendrochronological analysis of Betula glandulosa

Summary NDVI analysis and repeated aerial photographs have revealed significant shrub expansion in many subarctic regions. While the recent increase in temperature is usually considered to be the main driver of this phenomenon at regional scales, very little is known about the local heterogeneity of...

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Published in:Journal of Ecology
Main Authors: Ropars, Pascale, Lévesque, Esther, Boudreau, Stéphane
Other Authors: Bardgett, Richard, Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2015
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Online Access:http://dx.doi.org/10.1111/1365-2745.12394
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spelling crwiley:10.1111/1365-2745.12394 2024-06-23T07:52:25+00:00 How do climate and topography influence the greening of the forest‐tundra ecotone in northern Québec? A dendrochronological analysis of Betula glandulosa Ropars, Pascale Lévesque, Esther Boudreau, Stéphane Bardgett, Richard Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada 2015 http://dx.doi.org/10.1111/1365-2745.12394 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2F1365-2745.12394 https://besjournals.onlinelibrary.wiley.com/doi/pdf/10.1111/1365-2745.12394 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Ecology volume 103, issue 3, page 679-690 ISSN 0022-0477 1365-2745 journal-article 2015 crwiley https://doi.org/10.1111/1365-2745.12394 2024-06-13T04:22:53Z Summary NDVI analysis and repeated aerial photographs have revealed significant shrub expansion in many subarctic regions. While the recent increase in temperature is usually considered to be the main driver of this phenomenon at regional scales, very little is known about the local heterogeneity of shrub responses across the landscape. In this study, we aim to identify the climatic factors controlling the growth of the largely distributed shrub species B etula glandulosa in three types of environments (terrace, hilltop and snowbed). We also aim to evaluate the relationship between B . glandulosa growth and the NDVI data for the Boniface River region, in north‐western Québec, where the study took place. In the field, we harvested 180 B . glandulosa individuals (20 per site, 3 sites per type of environment). We constructed specific growth‐ring width chronologies and mean axial growth rate chronologies for each site and used them for dendroclimatic analysis (response functions). We also used linear regressions to evaluate the relative influence of dwarf birch growth on the NDVI trend. We found a sharp increase in B . glandulosa radial growth in the 1990s followed by a sharp decreasing trend from 2002 on terraces and hilltops, while growth remained high in snowbeds. B etula glandulosa growth was positively correlated with summer temperatures on terraces and hilltops, whereas winter precipitation promoted growth on snowbeds. The NDVI trend was largely correlated to B . glandulosa growth on terraces and hilltops for the period between 1986 and 2002 (71–80% explained variance). Synthesis . Our results suggest that topography plays a major role in B . glandulosa growth and therefore in shrub community dynamics. Because terraces and hilltops represent 70% of the land surface, the sharp B . glandulosa growth increase at these sites promoted an important overall expansion of the shrub community in the region. However, the decline in B . glandulosa growth observed after 2002 suggests that the expansion could be slowed down ... Article in Journal/Newspaper Dwarf birch Subarctic Tundra Wiley Online Library Journal of Ecology 103 3 679 690
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Summary NDVI analysis and repeated aerial photographs have revealed significant shrub expansion in many subarctic regions. While the recent increase in temperature is usually considered to be the main driver of this phenomenon at regional scales, very little is known about the local heterogeneity of shrub responses across the landscape. In this study, we aim to identify the climatic factors controlling the growth of the largely distributed shrub species B etula glandulosa in three types of environments (terrace, hilltop and snowbed). We also aim to evaluate the relationship between B . glandulosa growth and the NDVI data for the Boniface River region, in north‐western Québec, where the study took place. In the field, we harvested 180 B . glandulosa individuals (20 per site, 3 sites per type of environment). We constructed specific growth‐ring width chronologies and mean axial growth rate chronologies for each site and used them for dendroclimatic analysis (response functions). We also used linear regressions to evaluate the relative influence of dwarf birch growth on the NDVI trend. We found a sharp increase in B . glandulosa radial growth in the 1990s followed by a sharp decreasing trend from 2002 on terraces and hilltops, while growth remained high in snowbeds. B etula glandulosa growth was positively correlated with summer temperatures on terraces and hilltops, whereas winter precipitation promoted growth on snowbeds. The NDVI trend was largely correlated to B . glandulosa growth on terraces and hilltops for the period between 1986 and 2002 (71–80% explained variance). Synthesis . Our results suggest that topography plays a major role in B . glandulosa growth and therefore in shrub community dynamics. Because terraces and hilltops represent 70% of the land surface, the sharp B . glandulosa growth increase at these sites promoted an important overall expansion of the shrub community in the region. However, the decline in B . glandulosa growth observed after 2002 suggests that the expansion could be slowed down ...
author2 Bardgett, Richard
Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada
format Article in Journal/Newspaper
author Ropars, Pascale
Lévesque, Esther
Boudreau, Stéphane
spellingShingle Ropars, Pascale
Lévesque, Esther
Boudreau, Stéphane
How do climate and topography influence the greening of the forest‐tundra ecotone in northern Québec? A dendrochronological analysis of Betula glandulosa
author_facet Ropars, Pascale
Lévesque, Esther
Boudreau, Stéphane
author_sort Ropars, Pascale
title How do climate and topography influence the greening of the forest‐tundra ecotone in northern Québec? A dendrochronological analysis of Betula glandulosa
title_short How do climate and topography influence the greening of the forest‐tundra ecotone in northern Québec? A dendrochronological analysis of Betula glandulosa
title_full How do climate and topography influence the greening of the forest‐tundra ecotone in northern Québec? A dendrochronological analysis of Betula glandulosa
title_fullStr How do climate and topography influence the greening of the forest‐tundra ecotone in northern Québec? A dendrochronological analysis of Betula glandulosa
title_full_unstemmed How do climate and topography influence the greening of the forest‐tundra ecotone in northern Québec? A dendrochronological analysis of Betula glandulosa
title_sort how do climate and topography influence the greening of the forest‐tundra ecotone in northern québec? a dendrochronological analysis of betula glandulosa
publisher Wiley
publishDate 2015
url http://dx.doi.org/10.1111/1365-2745.12394
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2F1365-2745.12394
https://besjournals.onlinelibrary.wiley.com/doi/pdf/10.1111/1365-2745.12394
genre Dwarf birch
Subarctic
Tundra
genre_facet Dwarf birch
Subarctic
Tundra
op_source Journal of Ecology
volume 103, issue 3, page 679-690
ISSN 0022-0477 1365-2745
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1111/1365-2745.12394
container_title Journal of Ecology
container_volume 103
container_issue 3
container_start_page 679
op_container_end_page 690
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