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Coupled flow accumulation and atmospheric blocking govern flood duration

dc.contributor.authorNajibi, Nasser
dc.contributor.authorDevineni, Naresh
dc.contributor.authorLu, Mengqian
dc.contributor.authorPerdigão, Rui A. P.
dc.date.accessioned2023-10-13T17:26:09Z
dc.date.available2023-10-13T17:26:09Z
dc.date.issued2019-06
dc.description.abstractWe present a physically based Bayesian network model for inference and prediction of flood duration that allows for a deeper understanding of the nexus of antecedent flow regime, atmospheric blocking, and moisture transport/release mechanisms. Distinct scaling factors at the land surface and regional atmospheric levels are unraveled using this Bayesian network model. Land surface scaling explains the variability in flood duration as a function of cumulative exceedance index, a new measure that represents the evolution of the flood in the basin. Dynamic atmospheric scaling explains the cumulative exceedance index using the interaction between atmospheric blocking system and the synergistic model of wind divergence and atmospheric water vapor. Our findings underline that the synergy between a large persistent low-pressure blocking system and a higher rate of divergent wind often triggers a long-duration flood, even in the presence of moderate moisture supply in the atmosphere. This condition in turn causes an extremely long-duration flood if the basin-wide cumulative flow prior to the flood event was already high. Thus, this new land-atmospheric interaction framework integrates regional flood duration scaling and dynamic atmospheric scaling to enable the coupling of ‘horizontal’ (for example, streamflow accumulation inside the basin) and ‘vertical’ flow of information (for example, interrelated land and ocean-atmosphere interactions), providing an improved understanding of the critical forcing of regional hydroclimatic systems. This Bayesian model approach is applied to the Missouri River Basin, which has the largest system of reservoirs in the United States. Our predictive model can aid in decision support systems for the protection of national infrastructure against long-duration flood events.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationNajibi, N., Devineni, N., Lu, M. et al. Coupled flow accumulation and atmospheric blocking govern flood duration. npj Clim Atmos Sci 2, 19 (2019). https://doi.org/10.1038/s41612-019-0076-6pt_PT
dc.identifier.doi10.1038/s41612-019-0076-6pt_PT
dc.identifier.urihttp://hdl.handle.net/10451/59763
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherNaturept_PT
dc.relationFCT UID/BIA/00329/2019pt_PT
dc.relationFCT UID/EEA/50008/2019pt_PT
dc.relationMeteoceanics research project MR-220617 “Mathematical Physics and Predictability of Complex Coevolutionary Systemspt_PT
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/pt_PT
dc.titleCoupled flow accumulation and atmospheric blocking govern flood durationpt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.issue1pt_PT
oaire.citation.titlenpj Climate and Atmospheric Sciencept_PT
oaire.citation.volume2pt_PT
person.familyNamePerdigão
person.givenNameRui A. P.
person.identifier.ciencia-id9817-6C5B-1956
person.identifier.orcid0000-0001-5543-1754
person.identifier.ridK-9896-2015
person.identifier.scopus-author-id16025322100
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublication1d0aaa34-2a0b-4161-95a2-ac966a4a3b68
relation.isAuthorOfPublication.latestForDiscovery1d0aaa34-2a0b-4161-95a2-ac966a4a3b68

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