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LiDAR-based quantification of lava flow susceptibility in the City of Auckland (New Zealand)
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Lava flows represent one of the most significant volcanic hazards from basaltic monogenetic volcanoes, such as spatter cones, scoria cones, maars, and tuff rings. They are common features emanating from parasitic vents on the flanks of polygenetic volcanoes and in dominantly 'flat-lying' intraplate volcanic fields. The Auckland Volcanic Field (AVF) is a volcanic field that has been active for the last ca. 250ka, hosting at least 50 monogenetic volcanoes. Morphometric parameters of lava flows, such as volume, length, thickness and area, were used to quantify the potential lava-flow inundation susceptibility to New Zealand's most densely populated area, the City of Auckland based on an airborne Light Detection and Ranging (LiDAR) Digital Surface Model (DSM). The morphometric parameters of fifteen studied flows included: average length of 2.5km (range 0.7-6.5km), overall average thickness of 14.8m (range 3.4-43.8m), average of maximum thicknesses of 48.2m (range 18.3-180.5m), average area occupied of 5.1km 2 (range 0.4-25.1km 2) and average volume of 0.12km 3 (range 0.005-1km 3). Based on these parameters and a LiDAR-derived DSM, the present topography was classified into: sea, topographic depressions; low-lying areas prone to inundation by an average lava flow; buffer zones prone to inundation only by extremely thick lava flows; and peaks or ridges, which are unlikely to be overtopped. In monogenetic fields, each new vent occurs in a new location, creating uncertainty around the spatial location of the volcanic hazard. Thus, this research provides a general vent location-independent approach to describe the lava flow susceptibility for a potentially active monogenetic volcanic field. What this analysis reveals is that the City of Auckland can be divided into two distinct areas with strongly different susceptibility to lava flow inundation. The southern part of the City is predominantly flat, without hindrance to lava flow, whereas the hilly northern and central part has many ridges that can limit or channelise lavas. These contrasting properties must be accounted for in scenario-based or probabilistic hazard and risk models developed for the AVF. © 2012 Elsevier Inc.
2012
(Németh Károly (Vulkanológia, szediment...); 2012.10.05. 04:11:31)
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<div class="JournalArticle Publication short-list"> <div class="authors"> <span class="author-name" > Kereszturi, G </span> <span class="author-type"> </span> ; <span class="author-name" > Procter, J </span> <span class="author-type"> </span> ; <span class="author-name" > Cronin, SJ </span> <span class="author-type"> </span> ; <span class="author-name" mtid="10015050"> <a href="/gui2/?type=authors&mode=browse&sel=10015050" target="_blank">Németh, K</a> </span> <span class="author-type"> </span> ; <span class="author-name" > Bebbington, M </span> <span class="author-type"> </span> ; <span class="author-name" > Lindsay, J </span> <span class="author-type"> </span> </div ><div class="title"><a href="/gui2/?mode=browse¶ms=publication;2083403" mtid="2083403" target="_blank">LiDAR-based quantification of lava flow susceptibility in the City of Auckland (New Zealand)</a></div> <div class="pub-info"> <span class="journal-title">REMOTE SENSING OF ENVIRONMENT</span> <span class="journal-volume">125</span> <span class="page"> pp. 198-213. , 16 p. </span> <span class="year">(2012)</span> </div> <div class="pub-end"><div class="identifier-list"> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1016/j.rse.2012.07.015" target="_blank" href="https://doi.org/10.1016/j.rse.2012.07.015"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="S0034425712002891" target="_blank" href="http://www.sciencedirect.com/science/article/pii/S0034425712002891"> ScienceDirect </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000309331100017" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000309331100017"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="84865054143" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-84865054143"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:black" title="http://dx.doi.org/10.1016/j.rse.2012.07.015" target="_blank" href="http://dx.doi.org/10.1016/j.rse.2012.07.015"> Teljes dokumentum </a> </span> </span> </div> <div class="short-pub-prop-list"> <span class="deleted-record">Zárolt</span> <span class="short-pub-mtid"> Közlemény:2083403 </span> <span class="status-holder"><span class="status-data status-ADMIN_APPROVED"> Admin láttamozott </span></span> <span class="pub-core">Forrás Idéző </span> <span class="pub-type">Folyóiratcikk (Szakcikk ) </span> <!-- && !record.category.scientific --> <span class="pub-category">Tudományos</span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 25</span> | Független: 14 | Függő: 11 | Nem jelölt: 0 | WoS jelölt: 22 | Scopus jelölt: 15 | WoS/Scopus jelölt: 24 | DOI jelölt: 25 </div> </div> </div> </div><div class="JournalArticle Publication long-list"> <div class="authors"> <img title="Forrásközlemény" style="float: left" src="/frontend/resources/grid/publication-core-icon.png"> <img title="Idézőközlemény" style="float: left" src="/frontend/resources/grid/publication-citation-icon.png"> <div class="autype autype0"> <span class="author-name" >Kereszturi G </span> ; <span class="author-name" >Procter J </span> ; <span class="author-name" >Cronin SJ </span> ; <span class="author-name" mtid="10015050"><a href="/gui2/?type=authors&mode=browse&sel=10015050" target="_blank">Németh K (<span class="authorship-author-name">Németh Károly</span> <span class="authorAux-mtmt"> Vulkanológia, szedimentológia</span>) </a> </span> ; <span class="author-name" >Bebbington M </span> ; <span class="author-name" >Lindsay J </span> </div> </div> <div class="title"><a href="/gui2/?mode=browse¶ms=publication;2083403" target="_blank">LiDAR-based quantification of lava flow susceptibility in the City of Auckland (New Zealand)</a></div> <div> <span class="journal-title">REMOTE SENSING OF ENVIRONMENT</span> <span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0034-4257">0034-4257</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1879-0704">1879-0704</a>)</span>: <span class="journal-volume">125</span> <span class="page"> pp 198-213 </span> <span class="year">(2012)</span> </div> <div class="pub-footer"> <span class="language" xmlns="http://www.w3.org/1999/html">Nyelv: Angol | </span> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1016/j.rse.2012.07.015" target="_blank" href="https://doi.org/10.1016/j.rse.2012.07.015"> DOI </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="S0034425712002891" target="_blank" href="http://www.sciencedirect.com/science/article/pii/S0034425712002891"> ScienceDirect </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000309331100017" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000309331100017"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="84865054143" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-84865054143"> Scopus </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:black" title="http://dx.doi.org/10.1016/j.rse.2012.07.015" target="_blank" href="http://dx.doi.org/10.1016/j.rse.2012.07.015"> Teljes dokumentum </a> </span> </span> <div class="publication-citation" style="margin-left: 0.5cm;"> <span title="Nyilvános idézőközlemények összesen, említések nélkül" class="citingPub-count">Nyilvános idéző összesen: 25</span> | Független: 14 | Függő: 11 | Nem jelölt: 0 | WoS jelölt: 22 | Scopus jelölt: 15 | WoS/Scopus jelölt: 24 | DOI jelölt: 25 </div> <div class="publication-citation"> <a target="_blank" href="/api/publication?cond=citations.related;eq;2083403&sort=publishedYear,desc&sort=title"> Idézett közlemények száma: 9 </a> </div> <div class="mtid"><span class="long-pub-mtid">Közlemény: 2083403</span> | <span class="status-data status-ADMIN_APPROVED"> Admin láttamozott </span> <span class="oldId">Régi azonosító: 2083403</span> | Forrás Idéző | <span class="type-subtype">Folyóiratcikk ( Szakcikk ) </span> | <span class="pub-category">Tudományos</span> | <span class="publication-sourceOfData">Scopus</span> </div> <div class="lastModified">Utolsó módosítás: 2020.12.22. 12:39 Szuper Admin (admin) </div> <div class="lockedBy">Ideiglenesen zárolva 2022.03.22. 19:24 Boros Annamária (MTMT Központi admin) </div> </div></div>