Biogeophysical controls on soil-atmosphere thermal differences: implications on warming Arctic ecosystems
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 ( ∆...
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ftdoajarticles:oai:doaj.org/article:f7dd1fbaec5a4d0e91e2539b200a81f4 2023-09-05T13:16:51+02:00 Biogeophysical controls on soil-atmosphere thermal differences: implications on warming Arctic ecosystems J Aalto D Scherrer J Lenoir A Guisan M Luoto 2018-01-01T00:00:00Z https://doi.org/10.1088/1748-9326/aac83e https://doaj.org/article/f7dd1fbaec5a4d0e91e2539b200a81f4 EN eng IOP Publishing https://doi.org/10.1088/1748-9326/aac83e https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/aac83e 1748-9326 https://doaj.org/article/f7dd1fbaec5a4d0e91e2539b200a81f4 Environmental Research Letters, Vol 13, Iss 7, p 074003 (2018) thermal variability microclimate soil-atmosphere decoupling soil temperature structural equation model snow cover Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 article 2018 ftdoajarticles https://doi.org/10.1088/1748-9326/aac83e 2023-08-13T00:37:37Z 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 (β T ) 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 β T on the rate of local soil warming being stronger after (mean β T = 0.8 ± 0.1) than before (β T = 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 Directory of Open Access Journals: DOAJ Articles Arctic Environmental Research Letters 13 7 074003 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
thermal variability microclimate soil-atmosphere decoupling soil temperature structural equation model snow cover Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 |
spellingShingle |
thermal variability microclimate soil-atmosphere decoupling soil temperature structural equation model snow cover Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 J Aalto D Scherrer J Lenoir A Guisan M Luoto Biogeophysical controls on soil-atmosphere thermal differences: implications on warming Arctic ecosystems |
topic_facet |
thermal variability microclimate soil-atmosphere decoupling soil temperature structural equation model snow cover Environmental technology. Sanitary engineering TD1-1066 Environmental sciences GE1-350 Science Q Physics QC1-999 |
description |
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 (β T ) 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 β T on the rate of local soil warming being stronger after (mean β T = 0.8 ± 0.1) than before (β T = 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. |
format |
Article in Journal/Newspaper |
author |
J Aalto D Scherrer J Lenoir A Guisan M Luoto |
author_facet |
J Aalto D Scherrer J Lenoir A Guisan M Luoto |
author_sort |
J Aalto |
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 |
IOP Publishing |
publishDate |
2018 |
url |
https://doi.org/10.1088/1748-9326/aac83e https://doaj.org/article/f7dd1fbaec5a4d0e91e2539b200a81f4 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
Environmental Research Letters, Vol 13, Iss 7, p 074003 (2018) |
op_relation |
https://doi.org/10.1088/1748-9326/aac83e https://doaj.org/toc/1748-9326 doi:10.1088/1748-9326/aac83e 1748-9326 https://doaj.org/article/f7dd1fbaec5a4d0e91e2539b200a81f4 |
op_doi |
https://doi.org/10.1088/1748-9326/aac83e |
container_title |
Environmental Research Letters |
container_volume |
13 |
container_issue |
7 |
container_start_page |
074003 |
_version_ |
1776198289656381440 |