{"refrec":{"BRefID":231873,"RR":"<b>Lomax, A.; Michelini, A.</b> (2013). Tsunami early warning within five minutes. <i>Pure Appl. Geophys. 170(9-10)</i>: 1385-1395. <a href=\"https://dx.doi.org/10.1007/s00024-012-0512-6\" target=\"_blank\">https://dx.doi.org/10.1007/s00024-012-0512-6</a>","BEntID":223585,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Pure Appl. Geophys. 170(9-10)</i>: 1385-1395. <a href=\"https://dx.doi.org/10.1007/s00024-012-0512-6\" target=\"_blank\">https://dx.doi.org/10.1007/s00024-012-0512-6</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":1,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Lomax, A.; Michelini, A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Lomax, A.; Michelini, A.","Englishabstract":"Tsunamis are most destructive at near to regional distances, arriving within 20–30 min after a causative earthquake; effective early warning at these distances requires notification within 15 min or less. The size and impact of a tsunami also depend on sea floor displacement, which is related to the length, <em class=\"a-plus-plus\">L</em>, width, <em class=\"a-plus-plus\">W</em>, mean slip, <em class=\"a-plus-plus\">D</em>, and depth, <em class=\"a-plus-plus\">z</em>, of the earthquake rupture. Currently, the primary seismic discriminant for tsunami potential is the centroid-moment tensor magnitude, <em class=\"a-plus-plus\">M</em> <span class=\"a-plus-plus stack\">              <sub class=\"a-plus-plus\">w</sub>                                <sup class=\"a-plus-plus\">CMT</sup>                             </span>, representing the product <em class=\"a-plus-plus\">LWD</em> and estimated via an indirect inversion procedure. However, the obtained <em class=\"a-plus-plus\">M</em>   <span class=\"a-plus-plus stack\">                               <sub class=\"a-plus-plus\">w</sub>                                <sup class=\"a-plus-plus\">CMT</sup>                              </span> and the implied <em class=\"a-plus-plus\">LWD</em> value vary with rupture depth, earth model, and other factors, and are only available 20–30 min or more after an earthquake. The use of more direct discriminants for tsunami potential could avoid these problems and aid in effective early warning, especially for near to regional distances. Previously, we presented a direct procedure for rapid assessment of earthquake tsunami potential using two, simple measurements on <em class=\"a-plus-plus\">P</em>-wave seismograms—the predominant period on velocity records, <em class=\"a-plus-plus\">T</em>               <sub class=\"a-plus-plus\"> <em class=\"a-plus-plus\">d</em>    </sub>, and the likelihood, <em class=\"a-plus-plus\">T</em>        <span class=\"a-plus-plus stack\">                                <sub class=\"a-plus-plus\">50</sub>                                <sup class=\"a-plus-plus\">Ex</sup>                               </span>, that the high-frequency, apparent rupture-duration, <em class=\"a-plus-plus\">T</em> <sub class=\"a-plus-plus\">0</sub>, exceeds 50–55 s. We have shown that <em class=\"a-plus-plus\">T</em> <sub class=\"a-plus-plus\">                      <em class=\"a-plus-plus\">d</em>                              </sub> and <em class=\"a-plus-plus\">T</em> <sub class=\"a-plus-plus\">0</sub> are related to the critical rupture parameters <em class=\"a-plus-plus\">L</em>, <em class=\"a-plus-plus\">W</em>, <em class=\"a-plus-plus\">D</em>, and <em class=\"a-plus-plus\">z</em>, and that either of the period–duration products <em class=\"a-plus-plus\">T</em> <sub class=\"a-plus-plus\"> <em class=\"a-plus-plus\">d</em> </sub>                           <em class=\"a-plus-plus\">T</em> <sub class=\"a-plus-plus\">0</sub> or <em class=\"a-plus-plus\">T</em>                              <sub class=\"a-plus-plus\"> <em class=\"a-plus-plus\">d</em>        </sub> <em class=\"a-plus-plus\">T</em> <span class=\"a-plus-plus stack\"> <sub class=\"a-plus-plus\">50</sub>                        <sup class=\"a-plus-plus\">Ex</sup>                             </span> gives more information on tsunami impact and size than <em class=\"a-plus-plus\">M</em> <span class=\"a-plus-plus stack\">  <sub class=\"a-plus-plus\">w</sub>                              <sup class=\"a-plus-plus\">CMT</sup>                              </span>, <em class=\"a-plus-plus\">M</em>                         <sub class=\"a-plus-plus\">wp</sub>, and other currently used discriminants. These results imply that tsunami potential is not directly related to the product <em class=\"a-plus-plus\">LWD</em> from the “seismic” faulting model, as is assumed with the use of the <em class=\"a-plus-plus\">M</em>                              <span class=\"a-plus-plus stack\">                                 <sub class=\"a-plus-plus\">w</sub>                                <sup class=\"a-plus-plus\">CMT</sup>                               </span> discriminant. Instead, information on rupture length, <em class=\"a-plus-plus\">L</em>, and depth, <em class=\"a- lus-plus\">z</em>, as provided by <em class=\"a-plus-plus\">T</em><sub class=\"a-plus-plus\"> <em class=\"a-plus-plus\">d</em>        </sub> <em class=\"a-plus-plus\">T</em> <sub class=\"a-plus-plus\">0</sub> or <em class=\"a-plus-plus\">T</em>            <sub class=\"a-plus-plus\"> em class=\"a-plus-plus\">d</em>          </sub> <em class=\"a-plus-plus\">T</em> <span class=\"a-plus-plus stack\"> <sub class=\"a-plus-plus\">50</sub>                      <sup class=\"a-plus-plus\">Ex</sup>                            </span>, can constrain well the tsunami potential of an earthquake. We introduce here special treatment of the signal around the <em class=\"a-plus-plus\">S</em> arrival at close stations, a modified, real-time, <em class=\"a-plus-plus\">M</em>   <sub class=\"a-plus-plus\">wpd</sub>(RT) magnitude, and other procedures to enable early estimation of event parameters and tsunami discriminants. We show that with real-time data currently available in most regions of tsunami hazard, event locations, <em class=\"a-plus-plus\">m</em> <sub class=\"a-plus-plus\">              <em class=\"a-plus-plus\">b</em>                              </sub> and <em class=\"a-plus-plus\">M</em>                     <sub class=\"a-plus-plus\">wp</sub> magnitudes, and the direct, period–duration discriminant, <em class=\"a-plus-plus\">T</em> <sub class=\"a-plus-plus\"> <em class=\"a-plus-plus\">d</em>           </sub> <em class=\"a-plus-plus\">T</em> <span class=\"a-plus-plus stack\"> <sub class=\"a-plus-plus\">50</sub> <sup class=\"a-plus-plus\">Ex</sup> </span> can be determined within 5 min after an earthquake occurs, and <em class=\"a-plus-plus\">T</em> <sub class=\"a-plus-plus\">0</sub>, <em class=\"a-plus-plus\">T</em>       <sub class=\"a-plus-plus\"> <em class=\"a-plus-plus\">d</em>          </sub> <em class=\"a-plus-plus\">T</em> sub class=\"a-plus-plus\">0</sub>, and <em class=\"a-plus-plus\">M</em> <sub class=\"a-plus-plus\">wpd</sub>(RT) within approximately 10 min. This processing is implemented and running continuously in real-time within the Early-est earthquake monitor at INGV-Rome (<a href=\"http://early-est.rm.ingv.it\" class=\"a-plus-plus\">http://early-est.rm.ingv.it</a>). We also show that the difference <em class=\"a-plus-plus\">m</em>                   <sub class=\"a-plus-plus\"> <em class=\"a-plus-plus\">b</em>        </sub> - log<sub class=\"a-plus-plus\">10</sub>(<em class=\"a-plus-plus\">T</em> <sub class=\"a-plus-plus\"> <em class=\"a-plus-plus\">d</em> </sub> <em class=\"a-plus-plus\">T</em>         <sub class=\"a-plus-plus\">0</sub>) forms a rapid discriminant for slow, tsunami earthquakes. The rapid availability of these measurements can aid in faster and more reliable tsunami early warning for near to regional distances.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Tsunami early warning within five minutes","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-15 01:32:37.299117","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Early warning; Earthquake location; Real-time seismology","OtherDescriptors":null,"Notes":null,"AnaPub":2013,"MonPub":null,"DateUpdate":"2020-06-29","DateCreate":"2013-12-03","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000323747700003","VABBcode":null,"OpenAcc":0,"DOI":"10.1007/s00024-012-0512-6"},"refs":null,"anarec":{"AnaID":231873,"PubliDate":2013,"Pagination":"1385-1395","XtraPublOfAnaID":null,"ISBN":null,"Volume":"170","Issue":"9-10","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43723,"SerRR":"Pure and Applied Geophysics. 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