Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/163860
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dc.contributor.authorTailpied, Dorianneen_US
dc.contributor.authorLe Pichon, Alexisen_US
dc.contributor.authorTaisne, Benoiten_US
dc.date.accessioned2022-12-20T06:47:32Z-
dc.date.available2022-12-20T06:47:32Z-
dc.date.issued2022-
dc.identifier.citationTailpied, D., Le Pichon, A. & Taisne, B. (2022). Assessing uncertainties in infrasound network performance modelling: application to the Euro-Mediterranean and Southeast Asian region. Geophysical Journal International, 228(2), 1324-1345. https://dx.doi.org/10.1093/gji/ggab399en_US
dc.identifier.issn0956-540Xen_US
dc.identifier.urihttps://hdl.handle.net/10356/163860-
dc.description.abstractWe propose a modelling technique to confidently estimate and optimize the performance of any infrasound network to remotely monitor sources of interest such as volcanic eruptions, while considering realistic atmospheric specifications along the propagation path, source frequency and noise levels at the station. To provide a more realistic picture of the network performance, we define a confidence level accounting for propagation and atmospheric uncertainties. Therefore, we consider 'numerical' uncertainties linked to the approximations made in the used propagation model, errors of the developed mathematical model and atmospheric uncertainties derived from measurement campaigns. In parallel, we perform a sensitivity analysis to determine how each input parameter contributes to the developed mathematical model output as well as to the attenuation model output. Such study is helpful for model simplification and uncertainty reduction by identifying, and thus paying more attention to the most influential model inputs. Below 1 Hz, the effect of 'numerical' errors on network performance modelling dominates. The same situation is observed during strong and stable downwind stratospheric winds along propagation paths. Conversely, when propagation occurs upwind, atmospheric uncertainties become predominant as the frequency increases. This method is then applied to assess the performance of the International Monitoring System (IMS) infrasound network in the Euro-Mediterranean and the Southeast Asian regions. We highlight a frequency, seasonal and spatial dependence of uncertainties in the modelling. Below 1 Hz, large errors are predicted in the shadow zone but the overall error is less than 20 dB. Above 1 Hz, errors with same order of magnitude are also observed, when strong stratospheric jets prevail. But during weak stratospheric duct, uncertainties associated to the modelled attenuation may exceed 30 dB. Such studies lead to significant improvement in assessing detection capability of infrasound network, which is of great interest for monitoring artificial or natural explosive sources like volcanic eruption. In particular this work will contribute into designing and prioritizing maintenance of any given infrasound network, in order to provide even better and more accurate predictions.en_US
dc.description.sponsorshipMinistry of Education (MOE)en_US
dc.description.sponsorshipNational Research Foundation (NRF)en_US
dc.language.isoenen_US
dc.relation.ispartofGeophysical Journal Internationalen_US
dc.rights© The Author(s) 2021. Published by Oxford University Press on behalf of The Royal Astronomical Society. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited.en_US
dc.subjectScience::Geologyen_US
dc.titleAssessing uncertainties in infrasound network performance modelling: application to the Euro-Mediterranean and Southeast Asian regionen_US
dc.typeJournal Articleen
dc.contributor.schoolAsian School of the Environmenten_US
dc.contributor.researchEarth Observatory of Singaporeen_US
dc.identifier.doi10.1093/gji/ggab399-
dc.description.versionPublished versionen_US
dc.identifier.scopus2-s2.0-85121130204-
dc.identifier.issue2en_US
dc.identifier.volume228en_US
dc.identifier.spage1324en_US
dc.identifier.epage1345en_US
dc.subject.keywordsNumerical Modellingen_US
dc.subject.keywordsRemote Sensing Of Volcanoesen_US
dc.description.acknowledgementThis research was supported by the Earth Observatory of Singapore via its funding from the National Research Foundation Singapore and the Singapore Ministry of Education under the Research Centres of Excellence initiative. This work comprises EOS contribution number 405.en_US
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