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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-18-981-2014</article-id>
<title-group>
<article-title>A spatial bootstrap technique for parameter estimation of rainfall  annual maxima distribution</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Uboldi</surname>
<given-names>F.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sulis</surname>
<given-names>A. N.</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>Lussana</surname>
<given-names>C.</given-names>
<ext-link>https://orcid.org/0000-0003-3159-4895</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>Cislaghi</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>Russo</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>ARPA Lombardia, Regional Hydrographic Service, Milano, Italy</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Norwegian Meteorological Institute, Climatology Division, Oslo, Norway</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Independent researcher, Milano, Italy</addr-line>
</aff>
<pub-date pub-type="epub">
<day>11</day>
<month>03</month>
<year>2014</year>
</pub-date>
<volume>18</volume>
<issue>3</issue>
<fpage>981</fpage>
<lpage>995</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2014 F. Uboldi 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/articles/18/981/2014/hess-18-981-2014.html">This article is available from https://hess.copernicus.org/articles/18/981/2014/hess-18-981-2014.html</self-uri>
<self-uri xlink:href="https://hess.copernicus.org/articles/18/981/2014/hess-18-981-2014.pdf">The full text article is available as a PDF file from https://hess.copernicus.org/articles/18/981/2014/hess-18-981-2014.pdf</self-uri>
<abstract>
<p>Estimation of extreme event distributions and depth-duration-frequency
(DDF) curves is achieved at any target site by repeated sampling among
all available raingauge data in the surrounding area. The estimate
is computed over a gridded domain in Northern Italy, using precipitation
time series from 1929 to 2011, including data from historical analog
stations and from the present-day automatic observational network.
The presented local regionalisation naturally overcomes
traditional station-point methods, with their demand
of long historical series and their sensitivity to very rare events occurring
at very few stations, possibly causing unrealistic spatial gradients
in DDF relations. At the same time, the presented approach allows
for spatial dependence, necessary in a geographical domain such as
Lombardy, complex for both its topography and its climatology.
The bootstrap technique enables evaluating uncertainty maps for all
estimated parameters and for rainfall depths at assigned return periods.</p>
</abstract>
<counts><page-count count="15"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>