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<front>
<journal-meta>
<journal-id journal-id-type="publisher">NHESS</journal-id>
<journal-title-group>
<journal-title>Natural Hazards and Earth System Sciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">NHESS</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Nat. Hazards Earth Syst. Sci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1684-9981</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/nhess-13-187-2013</article-id>
<title-group>
<article-title>On the multi-fractal characteristics of the ULF geomagnetic field before the 1993 Guam earthquake</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Masci</surname>
<given-names>F.</given-names>
<ext-link>https://orcid.org/0000-0003-2314-3023</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Istituto Nazionale di Geofisica e Vulcanologia, L&apos;Aquila, Italy</addr-line>
</aff>
<pub-date pub-type="epub">
<day>29</day>
<month>01</month>
<year>2013</year>
</pub-date>
<volume>13</volume>
<issue>1</issue>
<fpage>187</fpage>
<lpage>191</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 F. Masci</copyright-statement>
<copyright-year>2013</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://nhess.copernicus.org/articles/13/187/2013/nhess-13-187-2013.html">This article is available from https://nhess.copernicus.org/articles/13/187/2013/nhess-13-187-2013.html</self-uri>
<self-uri xlink:href="https://nhess.copernicus.org/articles/13/187/2013/nhess-13-187-2013.pdf">The full text article is available as a PDF file from https://nhess.copernicus.org/articles/13/187/2013/nhess-13-187-2013.pdf</self-uri>
<abstract>
<p>Ida et al. (2005) document significant changes in the multi-fractal
parameters of the ULF geomagnetic field &lt;i&gt;H&lt;/i&gt; component starting about one month
before the 1993 Guam earthquake. According to the authors, these
multi-fractal signatures can be considered as precursory signals of the Guam
earthquake. As a consequence, they conclude that the multi-fractal analysis
may have an important role in the development of short-term earthquake
prediction capabilities. Since this and other similar reports have motivated
the idea that earthquake prediction based on electromagnetic precursory
signals may one day become a routine technique, the presumed precursors need
to be validated through independent datasets. In this review the seismogenic
origin of the multi-fractal magnetic signatures documented by Ida et al. (2005)
 before the 8 August 1993 Guam earthquake is seriously put into
question. By means of the geomagnetic &amp;Sigma;&lt;i&gt;K&lt;/i&gt;&lt;sub&gt;p&lt;/sub&gt; index, it is demonstrated
that these multi-fractal parameter changes are normal signals induced by
the variation of the global geomagnetic activity level.</p>
</abstract>
<counts><page-count count="5"/></counts>
</article-meta>
</front>
<body/>
<back>
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