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Controlled infrared heating of an artic meadow: challenge in the vegetation establishment stage

BACKGROUND: Global warming is going to affect both agricultural production and carbon storage in soil worldwide. Given the complexity of the soil-plant-atmosphere continuum, in situ experiments of climate warming are necessary to predict responses of plants and emissions of greenhouse gases (GHG) fr...

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Autores principales: Moni, Christophe, Silvennoinen, Hanna, Kimball, Bruce A., Fjelldal, Erling, Brenden, Marius, Burud, Ingunn, Flø, Andreas, Rasse, Daniel P.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: BioMed Central 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6339320/
https://www.ncbi.nlm.nih.gov/pubmed/30675175
http://dx.doi.org/10.1186/s13007-019-0387-y
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author Moni, Christophe
Silvennoinen, Hanna
Kimball, Bruce A.
Fjelldal, Erling
Brenden, Marius
Burud, Ingunn
Flø, Andreas
Rasse, Daniel P.
author_facet Moni, Christophe
Silvennoinen, Hanna
Kimball, Bruce A.
Fjelldal, Erling
Brenden, Marius
Burud, Ingunn
Flø, Andreas
Rasse, Daniel P.
author_sort Moni, Christophe
collection PubMed
description BACKGROUND: Global warming is going to affect both agricultural production and carbon storage in soil worldwide. Given the complexity of the soil-plant-atmosphere continuum, in situ experiments of climate warming are necessary to predict responses of plants and emissions of greenhouse gases (GHG) from soils. Arrays of infrared (IR) heaters have been successfully applied in temperate and tropical agro-ecosystems to produce uniform and large increases in canopy surface temperature across research plots. Because this method had not yet been tested in the Arctic where consequences of global warming on GHG emission are expected to be largest, the objective of this work was to test hexagonal arrays of IR heaters to simulate a homogenous 3 °C warming of the surface, i.e. canopy and visible bare soil, of five 10.5-m(2) plots in an Arctic meadow of northern Norway. RESULTS: Our results show that the IR warming setup was able to simulate quite accurately the target + 3 °C, thereby enabling us to simulate the extension of the growing season. Meadow yield increased under warming but only through the lengthening of the growing season. Our research also suggests that, when investigating agricultural systems on the Arctic, it is important to start the warming after the vegetation is established,. Indeed, differential emergence of meadow plants impaired the homogeneity of the warming with patches of bare soil being up to 9.5 °C warmer than patches of vegetation. This created a pattern of soil crusting, which further induced spatial heterogeneity of the vegetation. However, in the Arctic these conditions are rather rare as the soil exposed by snow melt is often covered by a layer of senescent vegetation which shelters the soil from direct radiation. CONCLUSIONS: Consistent continuous warming can be obtained on average with IR systems in an Arctic meadow, but homogenous spatial distribution requires that the warming must start after canopy closure. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (10.1186/s13007-019-0387-y) contains supplementary material, which is available to authorized users.
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spelling pubmed-63393202019-01-23 Controlled infrared heating of an artic meadow: challenge in the vegetation establishment stage Moni, Christophe Silvennoinen, Hanna Kimball, Bruce A. Fjelldal, Erling Brenden, Marius Burud, Ingunn Flø, Andreas Rasse, Daniel P. Plant Methods Methodology BACKGROUND: Global warming is going to affect both agricultural production and carbon storage in soil worldwide. Given the complexity of the soil-plant-atmosphere continuum, in situ experiments of climate warming are necessary to predict responses of plants and emissions of greenhouse gases (GHG) from soils. Arrays of infrared (IR) heaters have been successfully applied in temperate and tropical agro-ecosystems to produce uniform and large increases in canopy surface temperature across research plots. Because this method had not yet been tested in the Arctic where consequences of global warming on GHG emission are expected to be largest, the objective of this work was to test hexagonal arrays of IR heaters to simulate a homogenous 3 °C warming of the surface, i.e. canopy and visible bare soil, of five 10.5-m(2) plots in an Arctic meadow of northern Norway. RESULTS: Our results show that the IR warming setup was able to simulate quite accurately the target + 3 °C, thereby enabling us to simulate the extension of the growing season. Meadow yield increased under warming but only through the lengthening of the growing season. Our research also suggests that, when investigating agricultural systems on the Arctic, it is important to start the warming after the vegetation is established,. Indeed, differential emergence of meadow plants impaired the homogeneity of the warming with patches of bare soil being up to 9.5 °C warmer than patches of vegetation. This created a pattern of soil crusting, which further induced spatial heterogeneity of the vegetation. However, in the Arctic these conditions are rather rare as the soil exposed by snow melt is often covered by a layer of senescent vegetation which shelters the soil from direct radiation. CONCLUSIONS: Consistent continuous warming can be obtained on average with IR systems in an Arctic meadow, but homogenous spatial distribution requires that the warming must start after canopy closure. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (10.1186/s13007-019-0387-y) contains supplementary material, which is available to authorized users. BioMed Central 2019-01-19 /pmc/articles/PMC6339320/ /pubmed/30675175 http://dx.doi.org/10.1186/s13007-019-0387-y Text en © The Author(s) 2019 Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated.
spellingShingle Methodology
Moni, Christophe
Silvennoinen, Hanna
Kimball, Bruce A.
Fjelldal, Erling
Brenden, Marius
Burud, Ingunn
Flø, Andreas
Rasse, Daniel P.
Controlled infrared heating of an artic meadow: challenge in the vegetation establishment stage
title Controlled infrared heating of an artic meadow: challenge in the vegetation establishment stage
title_full Controlled infrared heating of an artic meadow: challenge in the vegetation establishment stage
title_fullStr Controlled infrared heating of an artic meadow: challenge in the vegetation establishment stage
title_full_unstemmed Controlled infrared heating of an artic meadow: challenge in the vegetation establishment stage
title_short Controlled infrared heating of an artic meadow: challenge in the vegetation establishment stage
title_sort controlled infrared heating of an artic meadow: challenge in the vegetation establishment stage
topic Methodology
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6339320/
https://www.ncbi.nlm.nih.gov/pubmed/30675175
http://dx.doi.org/10.1186/s13007-019-0387-y
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