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Nitrate–nitrite dynamics and phytoplankton growth: Formulation and experimental evaluation of a dynamic model
Nitrate–nitrite dynamics phytoplankton growth Formulation and experimental evaluation dynamic model
2014/4/4
A multi-nutrient quota model was modified to describe the coupled dynamics of nitrate and nitrite utilization for four phytoplankton species, Picochlorum atomus (Butcher) (Chlorophyta), Nannochloropsi...
Nitrate–nitrite dynamics and phytoplankton growth: Formulation and experimental evaluation of a dynamic model
Nitrate–nitrite dynamics phytoplankton growth Formulation experimental evaluation a dynamic model
2014/4/3
A multi-nutrient quota model was modified to describe the coupled dynamics of nitrate and nitrite utilization for four phytoplankton species, Picochlorum atomus(Butcher) (Chlorophyta), Nannochloropsis...
A Multi-Limit Mixed-Layer Entrainment Formulation
turbulence kinetic energy buoyancy flux density-fluctuation
2009/2/5
The second-moment equations for buoyancy flux and density-fluctuation variance in the entrainment zone of a mixed layer are combined to yield an entrainment rate (we dependence having the nature of Tu...
A Three-Layer Model for Wind-Driven Circulation in a Subtropical–Subpolar Basin. Part I：Model Formulation and the Subcritical State
Wind-Driven Circulation Subtropical–Subpolar Basin Subcritical State
2009/1/7
A three-layer model is formulated and run numerically in order to understand the highly nonlinear structure of the wind-driven circulation in a basin including both a subtropical and a subpolar gyre. ...
On Intermediate Models for Barotropic Continental Shelf and Slope Flow Fields. Part I：Formulation and Comparison of Exact Solutions
shallow-water equations geostrophic momentum linear balance equations geostrophic vorticity modified slow equations
2008/12/27
Motivated by the general objective of pursuing oceanographic process and data assimilation studies of the complex, nonlinear eddy and jet current fields observed over the continental shelf and slope o...
Numerical Simulation of Flow around a Tall Isolated Seamount. Part I：Problem Formulation and Model Accuracy
Numerical Simulation Problem Formulation Model Accuracy
2008/12/19
A sigma coordinate ocean circulation model is employed to study flow trapped to a tall seamount in a periodic f-plane channel. In Part I, errors arising from the pressure gradient formulation in the s...
A Bottom Boundary Layer-resolving Three-Dimensional Tidal Model：A Sensitivity Study of Eddy Viscosity Formulation
three-dimensional hydrodynamic model Eddy Viscosity Formulation bottom boundary layer
2008/12/18
A three-dimensional hydrodynamic model of the Irish Sea that resolves the bottom boundary layer, including the logarithmic layer, is developed. A finite-difference grid is employed in the horizontal, ...
The Influence of Eddy Viscosity Formulation, Bottom Topography, and Wind Wave Effects upon the Circulation of a Shallow Bay
Eddy Viscosity Formulation Bottom Topography Wind Wave Effects Shallow Bay
2008/12/12
A three-dimensional hydrodynamic model taking account of enhanced bed stress due to wave-current interaction is used to examine the wind-induced circulation and flushing time of an idealized homogeneo...