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   <subfield code="a">10.1007/s10950-006-9044-9</subfield>
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   <subfield code="u">AWE Blacknest, Brimpton, RG7 4RS, Reading, UK</subfield>
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   <subfield code="a">Source bias in epicentre determinations revisited</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[A. Douglas]</subfield>
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   <subfield code="a">Most estimates of the epicentre of the Long Shot explosion (29 October 1965, Aleutian Islands) are biased to the north of the true epicentre, this bias being much larger than formal uncertainty estimates. The bias is interpreted by some as evidence that the P-wave speeds in the upper mantle in the source region are higher to the north than to the south; that is, the difference between estimated and true epicentre is a source bias. Others argue that much of the bias can be explained by station anomalies, i.e. differences in the wave speeds in the upper mantle at stations to the north relative to those to the south. Bias may also be introduced by measurement error if signal-to-noise ratio (SNR) is lower on average at stations to the south compared to those to the north and times are read late at the low SNR stations. Here I locate Long Shot and the other two Aleutian Island explosions (Milrow and Cannikin) using P times from small networks of stations all on continents. The results support the view that a large component of the bias in the epicentres of the three explosions is due to station anomalies and not source bias, but that for the Long Shot explosion (the lowest magnitude of the three explosions), measurement error due to systematic variations in the SNR between stations to the north and south also contributes to the bias.</subfield>
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   <subfield code="a">Springer Science+Business Media, Inc., 2007</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">P waves</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">epicentre bias</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">nuclear explosions</subfield>
   <subfield code="2">nationallicence</subfield>
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  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">Journal of Seismology</subfield>
   <subfield code="d">Kluwer Academic Publishers</subfield>
   <subfield code="g">11/2(2007-04-01), 171-176</subfield>
   <subfield code="x">1383-4649</subfield>
   <subfield code="q">11:2&lt;171</subfield>
   <subfield code="1">2007</subfield>
   <subfield code="2">11</subfield>
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   <subfield code="B">NATIONALLICENCE</subfield>
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   <subfield code="E">0-</subfield>
   <subfield code="t">Journal of Seismology</subfield>
   <subfield code="d">Kluwer Academic Publishers</subfield>
   <subfield code="g">11/2(2007-04-01), 171-176</subfield>
   <subfield code="x">1383-4649</subfield>
   <subfield code="q">11:2&lt;171</subfield>
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   <subfield code="o">10950</subfield>
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  <datafield tag="900" ind1=" " ind2="7">
   <subfield code="a">Metadata rights reserved</subfield>
   <subfield code="b">Springer special CC-BY-NC licence</subfield>
   <subfield code="2">nationallicence</subfield>
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