Biogeophysical controls on soil-atmosphere thermal differences: implications on warming Arctic ecosystems
International audience Soil temperature (ST) has a key role in Arctic ecosystem functioning and global environmental change. However, soil thermal conditions do not necessarily follow synoptic temperature variations. This is because local biogeophysical processes can lead to a pronounced soil-atmosp...
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Online Access: | https://hal.science/hal-02352630 https://doi.org/10.1088/1748-9326/aac83e |
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ftunivpicardie:oai:HAL:hal-02352630v1 2024-02-11T10:00:31+01:00 Biogeophysical controls on soil-atmosphere thermal differences: implications on warming Arctic ecosystems Aalto, Juha Scherrer, Daniel Lenoir, Jonathan, Roger Michel Henri Guisan, Antoine Luoto, Miska Ecologie et Dynamique des Systèmes Anthropisés - UMR CNRS 7058 (EDYSAN) Université de Picardie Jules Verne (UPJV)-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Biologie de la Conservation (LBC) Université de Lausanne = University of Lausanne (UNIL) Thule Institute University of Oulu 2018-06-26 https://hal.science/hal-02352630 https://doi.org/10.1088/1748-9326/aac83e en eng HAL CCSD IOP Publishing info:eu-repo/semantics/altIdentifier/doi/10.1088/1748-9326/aac83e hal-02352630 https://hal.science/hal-02352630 doi:10.1088/1748-9326/aac83e ISSN: 1748-9326 Environmental Research Letters https://hal.science/hal-02352630 Environmental Research Letters, 2018, 13 (7), pp.074003. ⟨10.1088/1748-9326/aac83e⟩ https://iopscience.iop.org/article/10.1088/1748-9326/aac83e/meta [SDV.BID]Life Sciences [q-bio]/Biodiversity [SDV.EE]Life Sciences [q-bio]/Ecology environment [SDE.MCG]Environmental Sciences/Global Changes [SDE.BE]Environmental Sciences/Biodiversity and Ecology info:eu-repo/semantics/article Journal articles 2018 ftunivpicardie https://doi.org/10.1088/1748-9326/aac83e10.1088/1748-9326/aac83e/meta 2024-01-24T17:17:52Z International audience Soil temperature (ST) has a key role in Arctic ecosystem functioning and global environmental change. However, soil thermal conditions do not necessarily follow synoptic temperature variations. This is because local biogeophysical processes can lead to a pronounced soil-atmosphere thermal offset (∆T) while altering the coupling (βT) between ST and ambient air temperature (AAT). Here, we aim to uncover the spatiotemporal variation in these parameters and identify their main environmental drivers. By deploying a unique network of 322 temperature loggers and surveying biogeophysical processes across an Arctic landscape, we found that the spatial variation in ∆T during the AAT≤0 period (mean ∆T = 6.0 °C, standard deviation ± 1.2 °C) was directly and indirectly constrained by local topography controlling snow depth. By contrast, during the AAT>0 period, ∆T was controlled by soil characteristics, vegetation and solar radiation (∆T = −0.6 °C ± 1.0 °C). Importantly, ∆T was not constant throughout the seasons reflecting the influence of βT on the rate of local soil warming being stronger after (mean βT = 0.8 ± 0.1) than before (βT = 0.2 ± 0.2) snowmelt. Our results highlight the need for continuous microclimatic and local environmental monitoring, and suggest a potential for large buffering and non-uniform warming of snow-dominated Arctic ecosystems under projected temperature increase. Article in Journal/Newspaper Arctic Université de Picardie Jules Verne Arctic Environmental Research Letters 13 7 074003 |
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Open Polar |
collection |
Université de Picardie Jules Verne |
op_collection_id |
ftunivpicardie |
language |
English |
topic |
[SDV.BID]Life Sciences [q-bio]/Biodiversity [SDV.EE]Life Sciences [q-bio]/Ecology environment [SDE.MCG]Environmental Sciences/Global Changes [SDE.BE]Environmental Sciences/Biodiversity and Ecology |
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[SDV.BID]Life Sciences [q-bio]/Biodiversity [SDV.EE]Life Sciences [q-bio]/Ecology environment [SDE.MCG]Environmental Sciences/Global Changes [SDE.BE]Environmental Sciences/Biodiversity and Ecology Aalto, Juha Scherrer, Daniel Lenoir, Jonathan, Roger Michel Henri Guisan, Antoine Luoto, Miska Biogeophysical controls on soil-atmosphere thermal differences: implications on warming Arctic ecosystems |
topic_facet |
[SDV.BID]Life Sciences [q-bio]/Biodiversity [SDV.EE]Life Sciences [q-bio]/Ecology environment [SDE.MCG]Environmental Sciences/Global Changes [SDE.BE]Environmental Sciences/Biodiversity and Ecology |
description |
International audience Soil temperature (ST) has a key role in Arctic ecosystem functioning and global environmental change. However, soil thermal conditions do not necessarily follow synoptic temperature variations. This is because local biogeophysical processes can lead to a pronounced soil-atmosphere thermal offset (∆T) while altering the coupling (βT) between ST and ambient air temperature (AAT). Here, we aim to uncover the spatiotemporal variation in these parameters and identify their main environmental drivers. By deploying a unique network of 322 temperature loggers and surveying biogeophysical processes across an Arctic landscape, we found that the spatial variation in ∆T during the AAT≤0 period (mean ∆T = 6.0 °C, standard deviation ± 1.2 °C) was directly and indirectly constrained by local topography controlling snow depth. By contrast, during the AAT>0 period, ∆T was controlled by soil characteristics, vegetation and solar radiation (∆T = −0.6 °C ± 1.0 °C). Importantly, ∆T was not constant throughout the seasons reflecting the influence of βT on the rate of local soil warming being stronger after (mean βT = 0.8 ± 0.1) than before (βT = 0.2 ± 0.2) snowmelt. Our results highlight the need for continuous microclimatic and local environmental monitoring, and suggest a potential for large buffering and non-uniform warming of snow-dominated Arctic ecosystems under projected temperature increase. |
author2 |
Ecologie et Dynamique des Systèmes Anthropisés - UMR CNRS 7058 (EDYSAN) Université de Picardie Jules Verne (UPJV)-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Biologie de la Conservation (LBC) Université de Lausanne = University of Lausanne (UNIL) Thule Institute University of Oulu |
format |
Article in Journal/Newspaper |
author |
Aalto, Juha Scherrer, Daniel Lenoir, Jonathan, Roger Michel Henri Guisan, Antoine Luoto, Miska |
author_facet |
Aalto, Juha Scherrer, Daniel Lenoir, Jonathan, Roger Michel Henri Guisan, Antoine Luoto, Miska |
author_sort |
Aalto, Juha |
title |
Biogeophysical controls on soil-atmosphere thermal differences: implications on warming Arctic ecosystems |
title_short |
Biogeophysical controls on soil-atmosphere thermal differences: implications on warming Arctic ecosystems |
title_full |
Biogeophysical controls on soil-atmosphere thermal differences: implications on warming Arctic ecosystems |
title_fullStr |
Biogeophysical controls on soil-atmosphere thermal differences: implications on warming Arctic ecosystems |
title_full_unstemmed |
Biogeophysical controls on soil-atmosphere thermal differences: implications on warming Arctic ecosystems |
title_sort |
biogeophysical controls on soil-atmosphere thermal differences: implications on warming arctic ecosystems |
publisher |
HAL CCSD |
publishDate |
2018 |
url |
https://hal.science/hal-02352630 https://doi.org/10.1088/1748-9326/aac83e |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
ISSN: 1748-9326 Environmental Research Letters https://hal.science/hal-02352630 Environmental Research Letters, 2018, 13 (7), pp.074003. ⟨10.1088/1748-9326/aac83e⟩ https://iopscience.iop.org/article/10.1088/1748-9326/aac83e/meta |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1088/1748-9326/aac83e hal-02352630 https://hal.science/hal-02352630 doi:10.1088/1748-9326/aac83e |
op_doi |
https://doi.org/10.1088/1748-9326/aac83e10.1088/1748-9326/aac83e/meta |
container_title |
Environmental Research Letters |
container_volume |
13 |
container_issue |
7 |
container_start_page |
074003 |
_version_ |
1790596241950769152 |