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dc.contributor.authorMoni, Christophe
dc.contributor.authorSilvennoinen, Hanna Marika
dc.contributor.authorKimball, Bruce A.
dc.contributor.authorFjelldal, Erling
dc.contributor.authorBrenden, Marius
dc.contributor.authorBurud, Ingunn
dc.contributor.authorFlø, Andreas Svarstad
dc.contributor.authorRasse, Daniel
dc.coverage.spatialFinnmark, Norwaynb_NO
dc.date.accessioned2019-09-05T11:17:16Z
dc.date.available2019-09-05T11:17:16Z
dc.date.created2019-04-26T10:11:48Z
dc.date.issued2019-01-19
dc.identifier.citationPlant Methods. 2019, 15 1-12.nb_NO
dc.identifier.issn1746-4811
dc.identifier.urihttp://hdl.handle.net/11250/2612645
dc.description.abstractBackground: 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-m2 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.nb_NO
dc.language.isoengnb_NO
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.subjectClimate changenb_NO
dc.subjectWarmingnb_NO
dc.subjectFinnmarknb_NO
dc.subjectArcticnb_NO
dc.subjectInfrared heatersnb_NO
dc.subjectMeadownb_NO
dc.titleControlled infrared heating of an artic meadow: challenge in the vegetation establishment stagenb_NO
dc.typeJournal articlenb_NO
dc.typePeer reviewednb_NO
dc.description.versionpublishedVersionnb_NO
dc.subject.nsiVDP::Landbruks- og Fiskerifag: 900nb_NO
dc.source.pagenumber1-12nb_NO
dc.source.volume15nb_NO
dc.source.journalPlant Methodsnb_NO
dc.identifier.doi10.1186/s13007-019-0387-y
dc.identifier.cristin1694082
dc.relation.projectNorges forskningsråd: 225135nb_NO
cristin.unitcode7677,4,0,0
cristin.unitcode7677,2,0,0
cristin.unitnameDivisjon for miljø og naturressurser
cristin.unitnameDivisjon for skog og utmark
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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