Global Response Patterns of Major Rainfed Crops to Adaptation by Maintaining Current Growing Periods and Irrigation

dc.bibliographicCitation.firstPage1464eng
dc.bibliographicCitation.issue12eng
dc.bibliographicCitation.journalTitleEarth's futureeng
dc.bibliographicCitation.lastPage1480eng
dc.bibliographicCitation.volume7eng
dc.contributor.authorMinoli, Sara
dc.contributor.authorMüller, Christoph
dc.contributor.authorElliott, Joshua
dc.contributor.authorRuane, Alex C.
dc.contributor.authorJägermeyr, Jonas
dc.contributor.authorZabel, Florian
dc.contributor.authorDury, Marie
dc.contributor.authorFolberth, Christian
dc.contributor.authorFrançois, Louis
dc.contributor.authorHank, Tobias
dc.contributor.authorJacquemin, Ingrid
dc.contributor.authorLiu, Wenfeng
dc.contributor.authorOlin, Stefan
dc.contributor.authorPugh, Thomas A.M.
dc.date.accessioned2021-09-30T05:47:50Z
dc.date.available2021-09-30T05:47:50Z
dc.date.issued2019
dc.description.abstractIncreasing temperature trends are expected to impact yields of major field crops by affecting various plant processes, such as phenology, growth, and evapotranspiration. However, future projections typically do not consider the effects of agronomic adaptation in farming practices. We use an ensemble of seven Global Gridded Crop Models to quantify the impacts and adaptation potential of field crops under increasing temperature up to 6 K, accounting for model uncertainty. We find that without adaptation, the dominant effect of temperature increase is to shorten the growing period and to reduce grain yields and production. We then test the potential of two agronomic measures to combat warming-induced yield reduction: (i) use of cultivars with adjusted phenology to regain the reference growing period duration and (ii) conversion of rainfed systems to irrigated ones in order to alleviate the negative temperature effects that are mediated by crop evapotranspiration. We find that cultivar adaptation can fully compensate global production losses up to 2 K of temperature increase, with larger potentials in continental and temperate regions. Irrigation could also compensate production losses, but its potential is highest in arid regions, where irrigation expansion would be constrained by water scarcity. Moreover, we discuss that irrigation is not a true adaptation measure but rather an intensification strategy, as it equally increases production under any temperature level. In the tropics, even when introducing both adapted cultivars and irrigation, crop production declines already at moderate warming, making adaptation particularly challenging in these areas. ©2019. The Authors.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/6945
dc.identifier.urihttps://doi.org/10.34657/5992
dc.language.isoengeng
dc.publisherHoboken, NJ : Wiley-Blackwelleng
dc.relation.doihttps://doi.org/10.1029/2018EF001130
dc.relation.essn2328-4277
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subject.ddc550eng
dc.subject.otheradaptationeng
dc.subject.otheragricultural modelingeng
dc.subject.othercrop productioneng
dc.subject.othercultivareng
dc.subject.othergrowing seasoneng
dc.subject.otherhigh temperatureeng
dc.subject.otherirrigation systemeng
dc.subject.otherrainfed agricultureeng
dc.titleGlobal Response Patterns of Major Rainfed Crops to Adaptation by Maintaining Current Growing Periods and Irrigationeng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorPIKeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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