A cross-scale view of N and P limitation using a Bayesian hierarchical model
| dc.contributor.author | Cha, Yoonkyung | |
| dc.contributor.author | Alameddine, Ibrahim M. | |
| dc.contributor.author | Qian, Song S. | |
| dc.contributor.author | Stow, Craig A. | |
| dc.contributor.department | Department of Civil and Environmental Engineering | |
| dc.contributor.faculty | Maroun Semaan Faculty of Engineering and Architecture (MSFEA) | |
| dc.contributor.institution | American University of Beirut | |
| dc.date.accessioned | 2025-01-24T11:26:54Z | |
| dc.date.available | 2025-01-24T11:26:54Z | |
| dc.date.issued | 2016 | |
| dc.description.abstract | We 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.doi | https://doi.org/10.1002/lno.10375 | |
| dc.identifier.eid | 2-s2.0-84994663020 | |
| dc.identifier.uri | http://hdl.handle.net/10938/26713 | |
| dc.language.iso | en | |
| dc.publisher | Wiley Blackwell | |
| dc.relation.ispartof | Limnology and Oceanography | |
| dc.source | Scopus | |
| dc.subject | Finland | |
| dc.subject | Michigan | |
| dc.subject | Neuse estuary | |
| dc.subject | North carolina | |
| dc.subject | Saginaw bay | |
| dc.subject | United states | |
| dc.subject | Dreissenidae | |
| dc.subject | Bayesian analysis | |
| dc.subject | Concentration (composition) | |
| dc.subject | Correlation | |
| dc.subject | Hierarchical system | |
| dc.subject | Nitrogen | |
| dc.subject | Nutrient cycling | |
| dc.subject | Nutrient limitation | |
| dc.subject | Phosphorus | |
| dc.subject | Seasonal variation | |
| dc.title | A cross-scale view of N and P limitation using a Bayesian hierarchical model | |
| dc.type | Article |
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