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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ESD</journal-id>
<journal-title-group>
<journal-title>Earth System Dynamics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ESD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Earth Syst. Dynam.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">2190-4987</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/esd-4-129-2013</article-id>
<title-group>
<article-title>Climate change impact on available water resources obtained using multiple global climate and hydrology models</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hagemann</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Chen</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Clark</surname>
<given-names>D. B.</given-names>
<ext-link>https://orcid.org/0000-0003-1348-7922</ext-link>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Folwell</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gosling</surname>
<given-names>S. N.</given-names>
<ext-link>https://orcid.org/0000-0001-5973-6862</ext-link>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Haddeland</surname>
<given-names>I.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hanasaki</surname>
<given-names>N.</given-names>
<ext-link>https://orcid.org/0000-0002-5092-7563</ext-link>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Heinke</surname>
<given-names>J.</given-names>
<ext-link>https://orcid.org/0000-0001-5256-0024</ext-link>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ludwig</surname>
<given-names>F.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Voss</surname>
<given-names>F.</given-names>
</name>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Wiltshire</surname>
<given-names>A. J.</given-names>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Max Planck Institute for Meteorology, Bundesstr. 53, 20146 Hamburg, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Centre for Ecology and Hydrology, Wallingford, UK</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>School of Geography, University of Nottingham, Nottingham, UK</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Norwegian Water Resources and Energy Directorate, Oslo, Norway</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>National Institute for Environmental Studies, Tsukuba, Japan</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Potsdam Institute for Climate Impact Research, Potsdam, Germany</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>Wageningen University and Research Centre, Wageningen, the Netherlands</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>Center for Environmental Systems Research, University of Kassel, Kassel, Germany</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>Met Office Hadley Centre, Exeter, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>07</day>
<month>05</month>
<year>2013</year>
</pub-date>
<volume>4</volume>
<issue>1</issue>
<fpage>129</fpage>
<lpage>144</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 S. Hagemann et al.</copyright-statement>
<copyright-year>2013</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://esd.copernicus.org/articles/4/129/2013/esd-4-129-2013.html">This article is available from https://esd.copernicus.org/articles/4/129/2013/esd-4-129-2013.html</self-uri>
<self-uri xlink:href="https://esd.copernicus.org/articles/4/129/2013/esd-4-129-2013.pdf">The full text article is available as a PDF file from https://esd.copernicus.org/articles/4/129/2013/esd-4-129-2013.pdf</self-uri>
<abstract>
<p>Climate change is expected to alter the hydrological cycle resulting in
large-scale impacts on water availability. However, future climate change
impact assessments are highly uncertain. For the first time, multiple global
climate (three) and hydrological models (eight) were used to systematically
assess the hydrological response to climate change and project the future
state of global water resources. This multi-model ensemble allows us to
investigate how the hydrology models contribute to the uncertainty in
projected hydrological changes compared to the climate models. Due to their
systematic biases, GCM outputs cannot be used directly in hydrological impact
studies, so a statistical bias correction has been applied. The results show
a large spread in projected changes in water resources within the
climate–hydrology modelling chain for some regions. They clearly
demonstrate that climate models are not the only source of uncertainty for
hydrological change, and that the spread resulting from the choice of the
hydrology model is larger than the spread originating from the climate
models over many areas. But there are also areas showing a robust change
signal, such as at high latitudes and in some midlatitude regions, where
the models agree on the sign of projected hydrological changes, indicative
of higher confidence in this ensemble mean signal. In many catchments an
increase of available water resources is expected but there are some severe
decreases in Central and Southern Europe, the Middle East, the Mississippi
River basin, southern Africa, southern China and south-eastern Australia.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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