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<front>
<journal-meta>
<journal-id journal-id-type="publisher">HESSD</journal-id>
<journal-title-group>
<journal-title>Hydrology and Earth System Sciences Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">HESSD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Hydrol. Earth Syst. Sci. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1812-2116</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/hessd-11-9863-2014</article-id>
<title-group>
<article-title>Reducing the basin vulnerability by land management practices under past and future climate: a case study of the Nam Ou River Basin, Lao PDR</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Maharjan</surname>
<given-names>M.</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>Babel</surname>
<given-names>M. 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>Maskey</surname>
<given-names>S.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Water Engineering and Management, Asian Institute of   Technology, P.O. Box 4 Klong Luang, Pathumthani 12120, Thailand</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Department of Water Science and Engineering, UNESCO-IHE Institute for Water Education, P.O. Box 3015, 261DA Delft, the Netherlands</addr-line>
</aff>
<pub-date pub-type="epub">
<day>21</day>
<month>08</month>
<year>2014</year>
</pub-date>
<volume>11</volume>
<issue>8</issue>
<fpage>9863</fpage>
<lpage>9905</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2014 M. Maharjan et al.</copyright-statement>
<copyright-year>2014</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://hess.copernicus.org/preprints/11/9863/2014/hessd-11-9863-2014.html">This article is available from https://hess.copernicus.org/preprints/11/9863/2014/hessd-11-9863-2014.html</self-uri>
<self-uri xlink:href="https://hess.copernicus.org/preprints/11/9863/2014/hessd-11-9863-2014.pdf">The full text article is available as a PDF file from https://hess.copernicus.org/preprints/11/9863/2014/hessd-11-9863-2014.pdf</self-uri>
<abstract>
<p>This research evaluates different land management practices for the
  Nam Ou River Basin in Northern Laos for reducing vulnerability of
  the basin due to erosion and sediment yield under existing and
  future climate conditions. We use climate projection data
  (precipitation and temperature) from three general circulation
  models (GCMs) for three greenhouse gas emission scenarios (GHGES),
  namely B1, A1B and A2 and three future periods, namely 2011–2030,
  2046–2065 and 2080–2099. These large resolution GCM data are
  downscaled using the Long Ashton Research Station-Weather Generator
  (LARS-WG). The Soil and Water Assessment Tool (SWAT), which is
  a process based hydrological model, is used to simulate discharge
  and sediment yield and a threshold value of annual sediment yield is
  applied to identify vulnerable sub-basins. Results show that the
  change in the annual precipitation is expected to be between
  −7.60   to 2.64% in 2011–2030, −8.98 to 11.85% in 2046–2065,
  and −11.04 to 25.84% in 2080–2099. In the meantime, the
  changes in mean monthly temperature vary from 0.3 to
  1.3 &amp;deg;C in the 2011–2030, 1.3 to
  2.9 &amp;deg;C in the 2046–2065 and 1.9 to
  4.9 &amp;deg;C in the 2080–2099. Five sub-basins are
  identified vulnerable (critical) under the current climate. Our
  results show that terracing is the most effective land management
  practice to reduce sediment yield in these sub-basins followed by
  strip-cropping and filter strip. Appropriate land management
  practices applied under future climate scenarios show significant
  reduction in sediment yield (i.e. up to the tolerance limit) except
  for some sub-basins. In these exceptional sub-basins, designing an
  optimum combination of management practices is essential to reduce
  the vulnerability of the basin.</p>
</abstract>
<counts><page-count count="43"/></counts>
<funding-group>
<award-group id="gs1">
<funding-source></funding-source>
<award-id>103807</award-id>
</award-group>
</funding-group>
</article-meta>
</front>
<body/>
<back>
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