2010
DOI: 10.1016/j.ecolmodel.2009.12.014
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Simulating property exchange in estuarine ecosystem models at ecologically appropriate scales

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Cited by 20 publications
(14 citation statements)
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“…Smith and Hollibaugh 1993;Gazeau et al 2005a;Testa and Kemp 2008) or from numerical models (e.g. Kremer et al 2010). This approach can be widely applied to different aquatic ecosystems world-wide over multiple seasons and years, thus allowing a uniform standardized methodology for comparative analysis of diverse ecosystems, and represents a powerful approach for analyzing P n responses to changes in climate and nutrient loading and other perturbations.…”
Section: Open Water Methods: Oxygen Isotopesmentioning
confidence: 99%
“…Smith and Hollibaugh 1993;Gazeau et al 2005a;Testa and Kemp 2008) or from numerical models (e.g. Kremer et al 2010). This approach can be widely applied to different aquatic ecosystems world-wide over multiple seasons and years, thus allowing a uniform standardized methodology for comparative analysis of diverse ecosystems, and represents a powerful approach for analyzing P n responses to changes in climate and nutrient loading and other perturbations.…”
Section: Open Water Methods: Oxygen Isotopesmentioning
confidence: 99%
“…Abdelrhman, 2005;Cucco et al, 2009). The ROMS (Regional Oceanic Modelling System (Shchepetkin and McWilliams, 2005)) is a numerical code that has been used successfully in multiple domains and cases (Haidvogel et al, 2008;Ferrer et al, 2009;Grifoll et al, 2009;Kremer et al, 2010;and Warner et al, 2010). ROMS is a free-surface hydrostatic model that solves the three-dimensional Reynolds-Averaged from the Navier-Stokes equations (RANS), in horizontal curvilinear grid and vertical terrain-following coordinates.…”
Section: Numerical Implementation/validation and Scenario Descriptionmentioning
confidence: 99%
“…In fact, even the earliest marine ecosystem modeling studies were able to capture seasonal cycles of phytoplankton and zooplankton dynamics (Riley 1946). In many instances, the underlying formulations represent a daily approximation (Kremer et al 2010), and are based on experiments measured on timescales of a few hours. This raises several important considerations: 1) is it realistic to scale measured rates to such short model time-steps (minutes), 2) are model time-steps limited by past measurements and sampling techniques, and 3) what previous model formulations (e.g., phytoplankton growth rates) may incorrectly predict biomass when applied at short time-steps (Ménesguen et al 2007)?…”
Section: Model Limitations and Their Influence On Simulating Ecologmentioning
confidence: 99%
“…Simulating hydrodynamics and ecology simultaneously would have prohibited annual-scale simulations, and the model showed that inclusion of macroalgae produced water quality results more consistent with field data than with phytoplankton alone. Kremer et al (2010) similarly analyzed hydrodynamic model output to develop a daily exchange mixing matrix for simulating ecology in Narragansett Bay. The approach provided a cost- and time-efficient solution that was appropriate when the spatial and temporal scales needed for the ecology simulation was coarser than the scale used for hydrodynamic simulation.…”
Section: Linking Hydrodynamic and Ecological Modelsmentioning
confidence: 99%