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dc.contributor.authorRichter, G.M.
dc.contributor.authorQi, Aiming
dc.contributor.authorSemenov, M.A.
dc.contributor.authorJaggard, K. W.
dc.date.accessioned2013-12-18T13:00:11Z
dc.date.available2013-12-18T13:00:11Z
dc.date.issued2006-03
dc.identifier.citationRichter , G M , Qi , A , Semenov , M A & Jaggard , K W 2006 , ' Modelling the variability of UK sugar beet yields under climate change and husbandry adaptations ' , Soil Use and Management , vol. 22 , no. 1 , pp. 39-47 . https://doi.org/10.1111/j.1475-2743.2006.00018.x
dc.identifier.issn0266-0032
dc.identifier.otherPURE: 1996090
dc.identifier.otherPURE UUID: 8d005263-8e4a-466c-ad42-45bdb519763a
dc.identifier.otherWOS: 000236414300005
dc.identifier.otherScopus: 33644771182
dc.identifier.urihttp://hdl.handle.net/2299/12406
dc.description.abstractIn the future, UK summers are likely to be warmer and drier. Modelling differential water redistribution and uptake, we assessed the impact of future drier climates on sugar beet yields. Weather was generated for 1961-1990 (BASE) and predictions based on low- and high-emission scenarios (LO, HI) described in the most recent global climate simulations by the Hadley Centre, UK. Distributions and variability of relative soil moisture deficit (rSMD) and yield gap (drought-related yield loss, YG(dr) = 1-actual yield/potential yield), and sugar yield were calculated for different time-lines using regional weather, soil texture and management inputs. The rSMD is estimated to exceed the senescence threshold with a probability of 75% (2050sLO) to 95% (2080sHI) compared with 65% (BASE). The potential yield loss, YG(dr), is likely to increase from 17% (BASE) to 22% (2050sLO) to 35% (2080sHI). However, increasing potential growth rates (CO2 x temperature) cause average sugar yields to rise by between 1.4 and 2 t ha(-1) (2050sLO and 2050sHI respectively). Yield variation (CV%) may increase from 15-18% (BASE) to 18-23% (2050s) and 19-25% (2080s). Differences are small between regions but large within regions because of soil variability. In future, sugar yields on sands (8 t ha(-1)) are likely to increase by little (0.5-1.5 t ha(-1)), but on loams yields are likely to increase from 11 to 13 t ha(-1) (2050sHI) and 15 t ha(-1) (2080sHI). Earlier sowing and later harvest are potential tools to compensate for drought-related losses on sandy soils.en
dc.format.extent9
dc.language.isoeng
dc.relation.ispartofSoil Use and Management
dc.subjectSYSTEMS
dc.subjectHadRM3
dc.subjectCHANGE SCENARIOS
dc.subjectvariation
dc.subjectNITROGEN
dc.subjectINTERCEPTION
dc.subjectclimate change
dc.subjectENGLAND
dc.subjectIRRIGATION
dc.subjectdrought
dc.subjectWATER
dc.subjectsugar beet
dc.subjectGROWTH
dc.subjectPRODUCTIVITY
dc.subjectDROUGHT
dc.subjectyield gap
dc.subjectsoil available water
dc.titleModelling the variability of UK sugar beet yields under climate change and husbandry adaptationsen
dc.contributor.institutionDepartment of Human and Environmental Sciences
dc.contributor.institutionAgriculture, Food and Veterinary Sciences
dc.contributor.institutionGeography, Environment and Agriculture
dc.contributor.institutionCrop Protection and Climate Change
dc.contributor.institutionSchool of Life and Medical Sciences
dc.contributor.institutionHealth & Human Sciences Research Institute
dc.description.statusPeer reviewed
rioxxterms.versionofrecordhttps://doi.org/10.1111/j.1475-2743.2006.00018.x
rioxxterms.typeJournal Article/Review
herts.preservation.rarelyaccessedtrue


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