A cross-scale view of N and P limitation using a Bayesian hierarchical model

dc.contributor.authorCha, Yoonkyung
dc.contributor.authorAlameddine, Ibrahim M.
dc.contributor.authorQian, Song S.
dc.contributor.authorStow, Craig A.
dc.contributor.departmentDepartment of Civil and Environmental Engineering
dc.contributor.facultyMaroun Semaan Faculty of Engineering and Architecture (MSFEA)
dc.contributor.institutionAmerican University of Beirut
dc.date.accessioned2025-01-24T11:26:54Z
dc.date.available2025-01-24T11:26:54Z
dc.date.issued2016
dc.description.abstractWe propose a bivariate Bayesian hierarchical model (BBHM), which adds a perspective on a century-long subject of research, nitrogen (N) and phosphorus (P) dynamics in freshwater and coastal marine ecosystems. The BBHM is differentiated from existing approaches by modeling multiple aspects of N-P relationships―N and P concentration variability, ratio, and correlation―simultaneously, allowing these aspects to vary by seasonal and/or spatial components. The BBHM is applied to three aquatic systems, Finnish Lakes, Saginaw Bay, and the Neuse Estuary, which exhibit differing landscapes and complexity of nutrient dynamics. Our model reveals N and P dynamics that are critical to inferring unknown N and P distributions for the overall system as well as for within system variability. For Finnish lakes, strong positive within- and among-lake N and P correlations indicate that the rates of N and P biogeochemical cycles are closely coupled during summer across the different lake categories. In contrast, seasonal decoupling between N and P cycles in Saginaw Bay is evidenced by the large variability in monthly correlations and the seasonal changes in the N distribution. The results underscore the pivotal role that dreissenids have had on the cycling of nutrients and resurgence of eutrophication. The presence of clear seasonality and a spatial gradient in the distributions and N and P in the Neuse Estuary suggest that riverine N input is an important source in the season-space N dynamics, while summer sediment release is a major process regulating seasonal P distribution. © 2016 Association for the Sciences of Limnology and Oceanography
dc.identifier.doihttps://doi.org/10.1002/lno.10375
dc.identifier.eid2-s2.0-84994663020
dc.identifier.urihttp://hdl.handle.net/10938/26713
dc.language.isoen
dc.publisherWiley Blackwell
dc.relation.ispartofLimnology and Oceanography
dc.sourceScopus
dc.subjectFinland
dc.subjectMichigan
dc.subjectNeuse estuary
dc.subjectNorth carolina
dc.subjectSaginaw bay
dc.subjectUnited states
dc.subjectDreissenidae
dc.subjectBayesian analysis
dc.subjectConcentration (composition)
dc.subjectCorrelation
dc.subjectHierarchical system
dc.subjectNitrogen
dc.subjectNutrient cycling
dc.subjectNutrient limitation
dc.subjectPhosphorus
dc.subjectSeasonal variation
dc.titleA cross-scale view of N and P limitation using a Bayesian hierarchical model
dc.typeArticle

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