Critical impacts of global warming on land ecosystems

dc.bibliographicCitation.firstPage347eng
dc.bibliographicCitation.issue2eng
dc.bibliographicCitation.lastPage357eng
dc.bibliographicCitation.volume4
dc.contributor.authorOstberg, S.
dc.contributor.authorLucht, W.
dc.contributor.authorSchaphoff, S.
dc.contributor.authorGerten, D.
dc.date.accessioned2018-09-08T12:07:46Z
dc.date.available2019-06-28T10:34:42Z
dc.date.issued2013
dc.description.abstractGlobally increasing temperatures are likely to have impacts on terrestrial, aquatic and marine ecosystems that are difficult to manage. Quantifying impacts worldwide and systematically as a function of global warming is fundamental to substantiating the discussion on climate mitigation targets and adaptation planning. Here we present a macro-scale analysis of climate change impacts on terrestrial ecosystems based on newly developed sets of climate scenarios featuring a step-wise sampling of global mean temperature increase between 1.5 and 5 K by 2100. These are processed by a biogeochemical model (LPJmL) to derive an aggregated metric of simultaneous biogeochemical and structural shifts in land surface properties which we interpret as a proxy for the risk of shifts and possibly disruptions in ecosystems. Our results show a substantial risk of climate change to transform terrestrial ecosystems profoundly. Nearly no area of the world is free from such risk, unless strong mitigation limits global warming to around 2 degrees above preindustrial level. Even then, our simulations for most climate models agree that up to one-fifth of the land surface may experience at least moderate ecosystem change, primarily at high latitudes and high altitudes. If countries fulfil their current emissions reduction pledges, resulting in roughly 3.5 K of warming, this area expands to cover half the land surface, including the majority of tropical forests and savannas and the boreal zone. Due to differences in regional patterns of climate change, the area potentially at risk of major ecosystem change considering all climate models is up to 2.5 times as large as for a single model.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/234
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/3772
dc.language.isoengeng
dc.publisherMünchen : European Geopyhsical Unioneng
dc.relation.doihttps://doi.org/10.5194/esd-4-347-2013
dc.relation.ispartofseriesEarth System Dynamics, Volume 4, Issue 2, Page 347-357eng
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subjectBiogeochemical modelingeng
dc.subjectClimate change impacteng
dc.subjectClimate mitigationseng
dc.subjectGlobal-mean temperatureeng
dc.subjectIncreasing temperatureseng
dc.subjectLand surface propertieseng
dc.subjectPre-industrial levelseng
dc.subjectTerrestrial ecosystemseng
dc.subject.ddc500eng
dc.titleCritical impacts of global warming on land ecosystemseng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleEarth System Dynamicseng
tib.accessRightsopenAccesseng
wgl.contributorPIKeng
wgl.subjectUmweltwissenschafteneng
wgl.typeZeitschriftenartikeleng
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