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005        20171020120959.0
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245 00 |a Water availability in +2 degrees Celsius and +4 degrees Celsius worlds |h [electronic resource].
260        |a [S.l.] : |b The Royal Society, |c 2011.
490        |a Philosophical Transactions of the Royal Society.
506        |a Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights.
520 3    |a While the parties to the UNFCCC agreed in the December 2009 Copenhagen Accord that a 2◦C global warming over pre-industrial levels should be avoided, current commitments on greenhouse gas emissions reductions from these same parties will lead to a 50 : 50 chance of warming greater than 3.5◦C. Here, we evaluate the differences in impacts and adaptation issues for water resources in worlds corresponding to the policy objective (+2◦C) and possible reality (+4◦C). We simulate the differences in impacts on surface run-off and water resource availability using a global hydrological model driven by ensembles of climate models with global temperature increases of 2◦C and 4◦C. We combine these with UN-based population growth scenarios to explore the relative importance of population change and climate change for water availability. We find that the projected changes in global surface run-off from the ensemble show an increase in spatial coherence and magnitude for a +4◦C world compared with a +2◦C one. In a +2◦C world, population growth in most large river basins tends to override climate change as a driver of water stress, while in a +4◦C world, climate change becomes more dominant, even compensating for population effects where climate change increases runoff. However, in some basins where climate change has positive effects, the seasonality of surface run-off becomes increasingly amplified in a +4◦C climate.
533        |a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software.
650        |a climate change.
650        |a water resources.
650        |a hydrological models.
650        |a greenhouse gases.
720        |a Fai Fung.
720        |a Ana Lopez.
720        |a Mark New.
830    0 |a dpSobek.
830    0 |a Sea Level Rise.
852        |a dpSobek |c Sea Level Rise
856 40 |u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15060346/00001 |y Click here for full text
992 04 |a http://dpanther.fiu.edu/sobek/content/FI/15/06/03/46/00001/FI15060346thm.jpg
997        |a Sea Level Rise


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