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DOI10.1038/s41612-019-0076-6
Coupled flow accumulation and atmospheric blocking govern flood duration
Najibi N.; Devineni N.; Lu M.; Perdigão R.A.P.
发表日期2019
ISSN23973722
卷号2期号:1
英文摘要We 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. © 2019, The Author(s).
语种英语
scopus关键词atmospheric blocking; Bayesian analysis; flooding; hydrological regime; moisture transfer; wind; Missouri Basin; United States
来源期刊npj Climate and Atmospheric Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/178115
作者单位Department of Civil Engineering, City University of New York (City College), New York, NY 10031, United States; Center for Water Resources and Environmental Research (City Water Center), City University of New York, New York, NY 10031, United States; NOAA/Cooperative Science Center for Earth System Sciences and Remote Sensing Technologies (CREST), City University of New York, New York, NY 10031, United States; Department of Civil and Environmental Engineering, The Hong Kong University of Science and Technology, Clear Water Bay, Kowloon, Hong Kong; Institute of Telecommunications, Physics of Information and Quantum Technologies Group, Lisbon, Portugal; Centre for Ecology, Evolution and Environmental Changes, Faculty of Sciences, University of Lisbon, Lisbon, Portugal; Meteoceanics Interdisciplinary Centre for Complex System Science & Technische Universtät Wien (TU Wien), Vienna, Austria
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Najibi N.,Devineni N.,Lu M.,et al. Coupled flow accumulation and atmospheric blocking govern flood duration[J],2019,2(1).
APA Najibi N.,Devineni N.,Lu M.,&Perdigão R.A.P..(2019).Coupled flow accumulation and atmospheric blocking govern flood duration.npj Climate and Atmospheric Science,2(1).
MLA Najibi N.,et al."Coupled flow accumulation and atmospheric blocking govern flood duration".npj Climate and Atmospheric Science 2.1(2019).
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