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• W2102552059 endingPage "374" @default.
• W2102552059 startingPage "359" @default.
• W2102552059 abstract "Abstract. Future changes in runoff can have important implications for water resources and flooding. In this study, runoff projections from ISI-MIP (Inter-sectoral Impact Model Intercomparison Project) simulations forced with HadGEM2-ES bias-corrected climate data under the Representative Concentration Pathway 8.5 have been analysed for differences between impact models. Projections of change from a baseline period (1981–2010) to the future (2070–2099) from 12 impacts models which contributed to the hydrological and biomes sectors of ISI-MIP were studied. The biome models differed from the hydrological models by the inclusion of CO2 impacts and most also included a dynamic vegetation distribution. The biome and hydrological models agreed on the sign of runoff change for most regions of the world. However, in West Africa, the hydrological models projected drying, and the biome models a moistening. The biome models tended to produce larger increases and smaller decreases in regionally averaged runoff than the hydrological models, although there is large inter-model spread. The timing of runoff change was similar, but there were differences in magnitude, particularly at peak runoff. The impact of vegetation distribution change was much smaller than the projected change over time, while elevated CO2 had an effect as large as the magnitude of change over time projected by some models in some regions. The effect of CO2 on runoff was not consistent across the models, with two models showing increases and two decreases. There was also more spread in projections from the runs with elevated CO2 than with constant CO2. The biome models which gave increased runoff from elevated CO2 were also those which differed most from the hydrological models. Spatially, regions with most difference between model types tended to be projected to have most effect from elevated CO2, and seasonal differences were also similar, so elevated CO2 can partly explain the differences between hydrological and biome model runoff change projections. Therefore, this shows that a range of impact models should be considered to give the full range of uncertainty in impacts studies." @default.
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• W2102552059 date "2013-10-10" @default.
• W2102552059 modified "2023-10-09" @default.
• W2102552059 title "Comparing projections of future changes in runoff from hydrological and biome models in ISI-MIP" @default.
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• W2102552059 cites W1724334760 @default.
• W2102552059 cites W1975503965 @default.
• W2102552059 cites W1976095361 @default.
• W2102552059 cites W1976357734 @default.
• W2102552059 cites W1982646121 @default.
• W2102552059 cites W1985945138 @default.
• W2102552059 cites W1994917366 @default.
• W2102552059 cites W1995168765 @default.
• W2102552059 cites W1999243260 @default.
• W2102552059 cites W2015609649 @default.
• W2102552059 cites W2016714376 @default.
• W2102552059 cites W2017513998 @default.
• W2102552059 cites W2024695780 @default.
• W2102552059 cites W2027219405 @default.
• W2102552059 cites W2028714471 @default.
• W2102552059 cites W2033581884 @default.
• W2102552059 cites W2037513366 @default.
• W2102552059 cites W2043602343 @default.
• W2102552059 cites W2048476205 @default.
• W2102552059 cites W2052969156 @default.
• W2102552059 cites W2054653365 @default.
• W2102552059 cites W2063154108 @default.
• W2102552059 cites W2069079992 @default.
• W2102552059 cites W2074568577 @default.
• W2102552059 cites W2082776805 @default.
• W2102552059 cites W2085858708 @default.
• W2102552059 cites W2089855656 @default.
• W2102552059 cites W2091101199 @default.
• W2102552059 cites W2094915443 @default.
• W2102552059 cites W2097896815 @default.
• W2102552059 cites W2098445064 @default.
• W2102552059 cites W2105808960 @default.
• W2102552059 cites W2108443408 @default.
• W2102552059 cites W2110534701 @default.
• W2102552059 cites W2113442858 @default.
• W2102552059 cites W2118487689 @default.
• W2102552059 cites W2119442345 @default.
• W2102552059 cites W2122389133 @default.
• W2102552059 cites W2129095959 @default.
• W2102552059 cites W2131013362 @default.
• W2102552059 cites W2135774910 @default.
• W2102552059 cites W2140155467 @default.
• W2102552059 cites W2140193139 @default.
• W2102552059 cites W2141849518 @default.
• W2102552059 cites W2145814228 @default.
• W2102552059 cites W2147760191 @default.
• W2102552059 cites W2148345493 @default.
• W2102552059 cites W2151162783 @default.
• W2102552059 cites W2151329188 @default.
• W2102552059 cites W2159078401 @default.
• W2102552059 cites W2162323974 @default.
• W2102552059 cites W2163352988 @default.
• W2102552059 cites W2163673508 @default.
• W2102552059 cites W2168945034 @default.
• W2102552059 cites W2168945835 @default.
• W2102552059 cites W2171648606 @default.
• W2102552059 cites W2334507649 @default.
• W2102552059 cites W2761027408 @default.
• W2102552059 cites W2784510511 @default.
• W2102552059 cites W4232083844 @default.
• W2102552059 cites W4238537122 @default.
• W2102552059 cites W4246358509 @default.
• W2102552059 cites W4252317510 @default.
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• W2102552059 doi "https://doi.org/10.5194/esd-4-359-2013" @default.
• W2102552059 hasPublicationYear "2013" @default.
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