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<front>
<journal-meta>
<journal-id journal-id-type="publisher">PIAHS</journal-id>
<journal-title-group>
<journal-title>Proceedings of the International Association of Hydrological Sciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">PIAHS</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Proc. IAHS</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">2199-899X</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/piahs-366-86-2015</article-id>
<title-group>
<article-title>What part of natural flow can be considered a &quot;water resource&quot;?</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Andréassian</surname>
<given-names>V.</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>Margat</surname>
<given-names>J.</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>Thirel</surname>
<given-names>G.</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>Hubert</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Irstea, Hydrosystems and Bioprocesses Research Unit (HBAN), Antony, France</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>BRGM, Orléans, France</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Sorbonne Universités, UPMC Univ. Paris 06, UMR 7619 METIS,  75005, Paris, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>10</day>
<month>04</month>
<year>2015</year>
</pub-date>
<volume>366</volume>
<fpage>86</fpage>
<lpage>92</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2015 V. Andréassian et al.</copyright-statement>
<copyright-year>2015</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://piahs.copernicus.org/articles/366/86/2015/piahs-366-86-2015.html">This article is available from https://piahs.copernicus.org/articles/366/86/2015/piahs-366-86-2015.html</self-uri>
<self-uri xlink:href="https://piahs.copernicus.org/articles/366/86/2015/piahs-366-86-2015.pdf">The full text article is available as a PDF file from https://piahs.copernicus.org/articles/366/86/2015/piahs-366-86-2015.pdf</self-uri>
<abstract>
<p>In this paper, we discuss an unfortunate semantic shortcut – the use of the expression &quot;water resources&quot; as a synonym for &quot;river/groundwater flow&quot; – which causes great confusion in all Water Security-related discussions. We show that only a part of the flow can be considered a resource, and that the efficiency of the flow-to-resource conversion is a complex function of: (i) the hydrologic regime, (ii) environmental constraints (in-stream reserved flows), (iii) the type of water demand, and (iv) the existence of artificial reservoirs. Last, we illustrate how the flow-to-resource conversion can be affected by future climatic changes. Hydrologic data and climate change simulations for three French rivers (the rivers Vilaine, Durance and Garonne) are used to illustrate this discussion.</p>
</abstract>
<counts><page-count count="7"/></counts>
</article-meta>
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