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<div class="section" id="mb-bb">
<span id="global-mb-bb"></span><h1>mB_BB<a class="headerlink" href="#mb-bb" title="Permalink to this headline"></a></h1>
<p>Body wave magnitude at teleseismic distances similar to mb</p>
<div class="section" id="description">
<h2>Description<a class="headerlink" href="#description" title="Permalink to this headline"></a></h2>
<p>The name <strong>mB</strong> is used in <cite>SeisComP</cite> as a synonym for <strong>mB_BB</strong> which is recommended
by the IASPEI commission (<span id="id1">IASPEI [<a class="reference internal" href="../base/references.html#id40" title="IASPEI. Summary of magnitude working group recommendations on standard procedures for determining earthquake magnitudes from digital data. IASPEI Website, 2013. URL: http://www.iaspei.org/commissions/commission-on-seismological-observation-and-interpretation/Summary_WG_recommendations_20130327.pdf.">43</a>]</span>).</p>
<p>mB is a magnitude based on body waves like <a class="reference internal" href="global_mb.html#global-mb"><span class="std std-ref">mb</span></a>, but with the amplitude
measured in a broad
frequency range and longer time windows. Instead of amplitude measurements on displacement
data together with the dominant period, the maximum velocity amplitude Vmax is taken
directly from velocity-proportional records with <img class="math" src="../_images/math/3e38ca2d603956fc616a5148453d32f873cfdbd0.png" alt="V = 2 \pi A/T"/>. The time
window for the
measurement can be determined by the duration of the high-frequency (1-3 Hz) radiation
(<span id="id2">Bormann and Saul [<a class="reference internal" href="../base/references.html#id18" title="P. Bormann and J. Saul. The new iaspei standard broadband magnitude mb. Seismol. Res. Lett., 5:698 - 705, 2008. doi:10.1785/gssrl.79.5.698.">35</a>]</span>). This time window usually contains the phases P, pP, sP, PcP, but
not PP. According to the long time window and broad frequency range used for amplitude
measurements mB saturates not like mb.</p>
<div class="section" id="amplitude">
<h3>Amplitude<a class="headerlink" href="#amplitude" title="Permalink to this headline"></a></h3>
<p>The mB amplitudes are calculated on vertical-component displacement seismograms
in accordance with <span id="id3">Bormann and Saul [<a class="reference internal" href="../base/references.html#id18" title="P. Bormann and J. Saul. The new iaspei standard broadband magnitude mb. Seismol. Res. Lett., 5:698 - 705, 2008. doi:10.1785/gssrl.79.5.698.">35</a>]</span> and similar to <a class="reference internal" href="global_mb.html#global-mb"><span class="std std-ref">mb</span></a>.
A default time window of 60 s is considered for amplitude measurements
at stations in the distance range of 5° to 105°.
If the epicentral is known, the length of the time window after the P wave onset is</p>
<div class="math">
<p><img src="../_images/math/b79194c277468cc762f2a083243771fd575b5613.png" alt="t = min(11.5 \Delta, 60)"/></p>
</div><p>where <img class="math" src="../_images/math/6450616b75212cb568e905db49efd0c3dd584648.png" alt="\Delta"/> is the epicentral distance. The methods for measuring
amplitudes are configurable in the global bindings.</p>
</div>
<div class="section" id="station-magnitude">
<h3>Station Magnitude<a class="headerlink" href="#station-magnitude" title="Permalink to this headline"></a></h3>
<p>The mB station magntiudes are calculated in accordance with <span id="id4">Bormann and Saul [<a class="reference internal" href="../base/references.html#id18" title="P. Bormann and J. Saul. The new iaspei standard broadband magnitude mb. Seismol. Res. Lett., 5:698 - 705, 2008. doi:10.1785/gssrl.79.5.698.">35</a>]</span>.</p>
<div class="math">
<p><img src="../_images/math/c4e29d7f89b54eff7de102b648e87d8c0f96afd6.png" alt="mB = \log \left(\frac{A}{2\Pi}\right) + Q(h,\Delta) - 3.0"/></p>
</div><p>with A as the displacement amplitude in micrometers, T as the dominant period of
the signal in seconds, Q as a correction term for depth and distance.</p>
<ul class="simple">
<li><p>Amplitude unit in <cite>SeisComP</cite>: <strong>nanometers/s</strong> (nm/s),</p></li>
<li><p>Time window: 60 s if set by <a class="reference internal" href="scautopick.html#scautopick"><span class="std std-ref">scautopick</span></a>, otherwise 0 s - 11.5 * distance
(deg) with 60 s minimum</p></li>
<li><p>Default distance range: 5 - 105 deg, configurable: <a class="reference internal" href="global.html#confval-magnitudes.mB.minDist"><code class="xref std std-confval docutils literal notranslate"><span class="pre">magnitudes.mB.minDist</span></code></a>,
<a class="reference internal" href="global.html#confval-magnitudes.mB.maxDist"><code class="xref std std-confval docutils literal notranslate"><span class="pre">magnitudes.mB.maxDist</span></code></a>,</p></li>
<li><p>Depth range: no limitation.</p></li>
</ul>
<div class="admonition note">
<p class="admonition-title">Note</p>
<p>In 2013 the IASPEI commission (<span id="id5">IASPEI [<a class="reference internal" href="../base/references.html#id40" title="IASPEI. Summary of magnitude working group recommendations on standard procedures for determining earthquake magnitudes from digital data. IASPEI Website, 2013. URL: http://www.iaspei.org/commissions/commission-on-seismological-observation-and-interpretation/Summary_WG_recommendations_20130327.pdf.">43</a>]</span>) recommended a minimum
distance of
20 deg. However, the calibration formula (<span id="id6">Bormann and Saul [<a class="reference internal" href="../base/references.html#id18" title="P. Bormann and J. Saul. The new iaspei standard broadband magnitude mb. Seismol. Res. Lett., 5:698 - 705, 2008. doi:10.1785/gssrl.79.5.698.">35</a>]</span>) which is
integrated in
<cite>SeisComP</cite> allows the extension down to 5 deg while maintaining consistent magnitudes
at 20 deg and beyond. Therefore, 5 deg is used as the default in
<a class="reference internal" href="global.html#confval-magnitudes.mB.minDist"><code class="xref std std-confval docutils literal notranslate"><span class="pre">magnitudes.mB.minDist</span></code></a>.</p>
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<div class="section" id="network-magnitude">
<h3>Network magnitude<a class="headerlink" href="#network-magnitude" title="Permalink to this headline"></a></h3>
<p>By default, the trimmed mean is calculated from the station magnitudes to form
the <a class="reference internal" href="../base/glossary.html#term-network-magnitude"><span class="xref std std-term">network magnitude</span></a>. Outliers beyond the outer 12.5% percentiles are
removed before forming the mean.</p>
</div>
<div class="section" id="configuration">
<h3>Configuration<a class="headerlink" href="#configuration" title="Permalink to this headline"></a></h3>
<p>Adjust the configurable parameters in global bindings in the mB section or use
<code class="file docutils literal notranslate"><span class="pre">global.cfg</span></code>
as <a class="reference internal" href="global_mlv.html#global-mlv"><span class="std std-ref">MLv</span></a>. Add mB to the list of computed amplitudes and magnitudes
in the configuration of
<a class="reference internal" href="scamp.html#scamp"><span class="std std-ref">scamp</span></a> and <a class="reference internal" href="scmag.html#scmag"><span class="std std-ref">scmag</span></a> and in <a class="reference internal" href="scesv.html#scesv"><span class="std std-ref">scesv</span></a> or <a class="reference internal" href="scolv.html#scolv"><span class="std std-ref">scolv</span></a> for visibility.</p>
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<h3><a href="../index.html">Table of Contents</a></h3>
<ul>
<li><a class="reference internal" href="#">mB_BB</a><ul>
<li><a class="reference internal" href="#description">Description</a><ul>
<li><a class="reference internal" href="#amplitude">Amplitude</a></li>
<li><a class="reference internal" href="#station-magnitude">Station Magnitude</a></li>
<li><a class="reference internal" href="#network-magnitude">Network magnitude</a></li>
<li><a class="reference internal" href="#configuration">Configuration</a></li>
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