One-dimensional ecosystem model of the equatorial Pacific upwelling system. Part I: model development and silicon and nitrogen cycle

By F. Chai, Richard C. Dugdale, T. Peng, F. Wilkerson, R. Barber. 2002

311 citations recorded by the source corpus.

Subfields: Atmospheric Science, Oceanography

View Paper: https://www.semanticscholar.org/paper/4bd45cf020d94876733186d52b99424cd3cd2e51

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In Atmospheric Science

1. F. Ye
2. S. Grashorn
3. Y. Zhang
4. E. Stanev
5. B. Fry
6. B. Popp

In Oceanography

1. B. Popp
2. C. Hannides
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Citations in the corpus

• Predicting potentially toxigenic Pseudo-nitzschia blooms in the Chesapeake Bay (2010, methodology): “Present research involves diagnostic coupling of alternative ecosystem models to ChesROMS that include Si(OH)4 in their formulation (e.g. Moore et al., 2002; Chai et al., 2002).”
• Bridging the gap from ocean models to population dynamics of large marine predators: A model of mid-trophic functional groups (2010, methodology): “, 1998, 2003; Lehodey, 2001) with predicted fields from two different coupled physical–biogeochemical models: the carbon-based biogeochemical model used in the present study, and a nitrogen-based model (Chai et al., 2002; Dugdale et al., 2002).”
• Planktonic ecosystem models: perplexing parameterizations and a failure to fail (2009, unknown): “…uptake from 10 recent ecosystem models Model NO3 Ks (mmol N L21) NH4 Ks (mmol N L21) Besiktepe et al. (2003) 0.5 0.2 Chai et al. (2002) 0.5 0.05 Christian et al. (2002) 0.25 0.05 Denman and Peña (1999) 0.1 Fujii et al. (2002) 3.0 0.3 Hood et al. (2001) 0.5 Kishi et al. (2007)…”
• Insight into the Trophic Ecology of Yellowfin Tuna, Thunnus albacares, from Compound‐Specific Nitrogen Isotope Analysis of Proteinaceous Amino Acids (2007, methodology): “Collectively, we define these taxa as components of the mesozooplankton guild, after Chai et al. (2002) and Olson and Watters (2003).”
• Pelagic functional group modeling: Progress, challenges and prospects (2006, unknown): “Several models have yielded realistic distributions and time courses of [Si(OH)4], SiObio and the contribution of diatoms to primary productivity using this assumption (Chai et al., 2002; Fujii et al., 2002; Aumont et al., 2003).”
• Co-limitation of diatoms by iron and silicic acid in the equatorial Pacific (2011, background): “Our results help resolve whether phytoplankton growth rates and new production in the EEP are regulated by Si (Dugdale and Wilkerson, 1998; Chai et al., 2002) or Fe (Coale et al., 1996a; Martin et al., 1994; de Baar et al., 2005; Boyd et al., 2007).”
• Seamless cross-scale modeling with SCHISM (2016, methodology): “At the moment the SCHISM modeling sys- S em includes: a wind-wave model ( Roland et al 2012 ), 3 sediment ransport models (Community Sediment Transport Model ( Pinto et l. 2012 ), SED2D ( Dodet 2013 ), and TIMOR ( Zanke 2003 )), 2 biologcal/ecological models (EcoSIM ( Rodrigues et al. 2009 ) and CoS”