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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ADGEO</journal-id>
<journal-title-group>
<journal-title>Advances in Geosciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">ADGEO</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Adv. Geosci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7359</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/adgeo-10-51-2007</article-id>
<title-group>
<article-title>Mapping monthly rainfall data in Galicia (NW Spain) using inverse distances and geostatistical methods</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Mirás-Avalos</surname>
<given-names>J. 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>Paz-González</surname>
<given-names>A.</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>Vidal-Vázquez</surname>
<given-names>E.</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>Sande-Fouz</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Faculty of Sciences, University of Coru&amp;ntilde;a, 15071 Coru&amp;ntilde;a, Spain</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>EPS Lugo, University of Santiago de Compostela, 27002 Lugo, Spain</addr-line>
</aff>
<pub-date pub-type="epub">
<day>26</day>
<month>04</month>
<year>2007</year>
</pub-date>
<volume>10</volume>
<fpage>51</fpage>
<lpage>57</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2007 J. M. Mirás-Avalos et al.</copyright-statement>
<copyright-year>2007</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://adgeo.copernicus.org/articles/10/51/2007/adgeo-10-51-2007.html">This article is available from https://adgeo.copernicus.org/articles/10/51/2007/adgeo-10-51-2007.html</self-uri>
<self-uri xlink:href="https://adgeo.copernicus.org/articles/10/51/2007/adgeo-10-51-2007.pdf">The full text article is available as a PDF file from https://adgeo.copernicus.org/articles/10/51/2007/adgeo-10-51-2007.pdf</self-uri>
<abstract>
<p>In this paper, results from three different interpolation techniques based
on Geostatistics (ordinary kriging, kriging with external drift and
conditional simulation) and one deterministic method (inverse distances) for
mapping total monthly rainfall are compared. The study data set comprised
total monthly rainfall from 1998 till 2001 corresponding to a maximum of 121
meteorological stations irregularly distributed in the region of Galicia (NW
Spain). Furthermore, a raster Geographic Information System (GIS) was used
for spatial interpolation with a 500&amp;times;500 m grid digital elevation model.
Inverse distance technique was appropriate for a rapid estimation of the
rainfall at the studied scale. In order to apply geostatistical
interpolation techniques, a spatial dependence analysis was performed;
rainfall spatial dependence was observed in 33 out of 48 months analysed,
the rest of the rainfall data sets presented a random behaviour. Different
values of the semivariogram parameters caused the smoothing in the maps
obtained by ordinary kriging. Kriging with external drift results were
according to former studies which showed the influence of topography.
Conditional simulation is considered to give more realistic results;
however, this consideration must be confirmed with new data.</p>
</abstract>
<counts><page-count count="7"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>