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dc.contributor.authorKnox, Ryan G.
dc.contributor.authorKoven, Charles D.
dc.contributor.authorRiley, William J.
dc.contributor.authorWalker, Anthony P.
dc.contributor.authorWright, S. Joseph
dc.contributor.authorHolm, Jennifer A.
dc.contributor.authorWei, Xinyuan
dc.contributor.authorFisher, Rosie
dc.contributor.authorZhu, Qing
dc.contributor.authorTang, Jinyun
dc.contributor.authorRicciuto, Daniel M.
dc.contributor.authorShuman, Jacquelyn K.
dc.contributor.authorYang, Xiaojuan
dc.contributor.authorKueppers, Lara M.
dc.contributor.authorChambers, Jeffrey Q.
dc.date.accessioned2024-09-23T08:46:37Z
dc.date.available2024-09-23T08:46:37Z
dc.date.created2024-03-19T10:34:58Z
dc.date.issued2024
dc.identifier.citationJournal of Advances in Modeling Earth Systems. 2024, 16 (3), .en_US
dc.identifier.issn1942-2466
dc.identifier.urihttps://hdl.handle.net/11250/3153675
dc.description.abstractWe present a representation of nitrogen and phosphorus cycling in the Functionally Assembled Terrestrial Ecosystem Simulator, a demographic vegetation model within the Energy Exascale Earth System land model. This representation is modular, and designed to allow testing of multiple hypothetical approaches for carbon-nutrient coupling in plants. Novel model hypotheses introduced in this work include, (a) the controls on plant acquisition of aqueous mineralized nutrients in the soil and (b) fairly straight forward methods of allocating nutrients to specific plant organs and their losses through live plant turnover as well as litter fluxes generated through plant mortality. This combines the new with pre-existing hypotheses (such as nitrogen fixation and soil decomposition) into a system that can accommodate plant-soil dynamics for a large number of size- and functional-type-resolved plant cohorts within a time-since-disturbance-resolved ecosystem. Root uptake of nutrients is governed by fine root biomass, and plants vary in their fine root biomass allocation in order to balance carbon and nutrient limitations to growth. We test the sensitivity of the model to a wide range of parameter variations and structural representations, and in the context of observations at Barro Colorado Island, Panama. A key model prediction is that plants in the high-light-availability canopy positions allocate more carbon to fine roots than plants in low-light understory environments, given the widely different carbon versus nutrient constraints of these two niches within a given ecosystem. This model provides a basis for exploring carbon-nutrient coupling with vegetation demography within Earth system models.en_US
dc.language.isoengen_US
dc.publisherJohn Wiley & Sonsen_US
dc.rightsNavngivelse-Ikkekommersiell 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by-nc/4.0/deed.no*
dc.titleNutrient Dynamics in a Coupled Terrestrial Biosphere and Land Model (ELM-FATES-CNP)en_US
dc.title.alternativeNutrient Dynamics in a Coupled Terrestrial Biosphere and Land Model (ELM-FATES-CNP)en_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber0en_US
dc.source.volume16en_US
dc.source.journalJournal of Advances in Modeling Earth Systemsen_US
dc.source.issue3en_US
dc.identifier.doi10.1029/2023MS003689
dc.identifier.cristin2255658
dc.relation.projectEU – Horisont Europa (EC/HEU): 101003536en_US
dc.relation.projectEU – Horisont Europa (EC/HEU): 821003en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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Navngivelse-Ikkekommersiell 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse-Ikkekommersiell 4.0 Internasjonal