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<front>
<journal-meta>
<journal-id journal-id-type="publisher">HESS</journal-id>
<journal-title-group>
<journal-title>Hydrology and Earth System Sciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">HESS</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Hydrol. Earth Syst. Sci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1607-7938</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/hess-7-245-2003</article-id>
<title-group>
<article-title>TECHNICAL NOTE: &lt;br&gt;First evidence of a structured and dynamic spatial pattern of rainfall within a small humid tropical catchment</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bidin</surname>
<given-names>K.</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>Chappell</surname>
<given-names>N. A.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>School of Science and Technology, University Malaysia Sabah, 88999 Kota Kinabalu, Sabah, Malaysia</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute of Environmental and Natural Sciences, Lancaster University, Lancaster LA1 4YQ, UK</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Email for corresponding author: n.chappell@lancaster.ac.uk</addr-line>
</aff>
<pub-date pub-type="epub">
<day>30</day>
<month>04</month>
<year>2003</year>
</pub-date>
<volume>7</volume>
<issue>2</issue>
<fpage>245</fpage>
<lpage>253</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2003 K. Bidin</copyright-statement>
<copyright-year>2003</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Generic License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by-nc-sa/2.5/">https://creativecommons.org/licenses/by-nc-sa/2.5/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://hess.copernicus.org/articles/7/245/2003/hess-7-245-2003.html">This article is available from https://hess.copernicus.org/articles/7/245/2003/hess-7-245-2003.html</self-uri>
<self-uri xlink:href="https://hess.copernicus.org/articles/7/245/2003/hess-7-245-2003.pdf">The full text article is available as a PDF file from https://hess.copernicus.org/articles/7/245/2003/hess-7-245-2003.pdf</self-uri>
<abstract>
<p>In a study of the spatial variability of rainfall across a network of 46 
        raingauges in a 4 km&lt;sup&gt;2&lt;/sup&gt; rainforest catchment in the interior of northeastern 
        Borneo, seasonal rainfall totals were correlated with raingauge separation distance, 
        aspect and relief. A very high degree of spatial variability in seasonal totals across 
        a very small area was found, even in comparison with other regions experiencing convective 
        rainfall. Moreover, it shows systematic, stochastic structure in rainfall is present over 
        scales of 10s to 100s metres; these patterns change from the southwest monsoon (May-October) 
        to the northeast monsoon (November-April). Local associations with aspect and relief are 
        present but the seasonal changes in rainfall pattern over the whole 4 km&lt;sup&gt;2&lt;/sup&gt; 
        catchment must relate to more complex local topographic effects on the regional windfield.&lt;/p&gt;

&lt;p style=&quot;line-height: 20px;&quot;&gt;&lt;b&gt;Keywords: &lt;/b&gt;catchment, Malaysia,monsoon, rainfall, spatial variability</p>
</abstract>
<counts><page-count count="9"/></counts>
</article-meta>
</front>
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