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Cotidal Charts for the Pacific Ocean near Hawaii Using f-Plane Solutions
Cotidal Charts f-Plane Solutions Pacific Ocean near Hawaii
2009/3/7
The tidal constituents K1, O1, P1, Q1, M2, S2, N2, K2 derived from sea level records at six sites spanning the Hawaiian Islands show a systematic variation in amplitude and phase from site to site tha...
Eastern Boundary Conditions and Weak Solutions of the Ideal Thermocline Equations
Boundary Conditions Weak Solutions Ideal Thermocline Equations
2009/1/13
It is argued that the ideal fluid thermocline equations have “weak” (i.e., nondifferentiable) solutions that satisfy no mass-flux boundary conditions at the East. This conclusion is based on a local a...
Solutions of the Ideal Fluid Thermocline with Continuous Stratification
Ideal Fluid Thermocline Continuous Stratification
2009/1/10
From an examination of possible ways to satisfy the essential upper boundary conditions, a general way to solve the ideal fluid thermocline is proposed. Through specifying the functional relation betw...
On Intermediate Models for Barotropic Continental Shelf and Slope Flow Fields. Part III：Comparison of Numerical Model Solutions in Periodic Channels
Intermediate Models Slope Flow Fields Barotropic Continental Shelf Numerical Model Solutions
2008/12/30
The study of intermediate models for barotropic continental shelf and slope flow fields initiated in Parts I and II is continued. The objective is to investigate the possible use of intermediate model...
On Intermediate Models for Barotropic Continental Shelf and Slope Flow Fields. Part II：Comparison of Numerical Model Solutions in Doubly Periodic Domains
geostrophic vorticity geostrophic momentum linear balance equations
2008/12/27
As part of a program to improve understanding of the dynamics of the complicated, vigorous eddy and jet flow fields recently observed over the continental shelf and slope, we investigate the potential...
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...
Multiple Equilibria, Periodic, and Aperiodic Solutions in a Wind-Driven, Double-Gyre, Shallow-Water Model
shallow-water western boundary currents quasigeostrophic
2008/12/11
A reduced-gravity shallow-water (SW) model is used to study the nonlinear behavior of western boundary currents (WBCs), with particular emphasis on multiple equilibria and low-frequency variations. Wh...
Tracking Nonlinear Solutions with Simulated Altimetric Data in a Shallow-Water Model
Nonlinear Solutions Simulated Altimetric Data Shallow-Water Model
2008/11/11
Low-frequency variability of western boundary currents (WBCs) is pervasive in both observations and numerical models of the oceans. Because advection is of the essence in WBCs, nonlinearities are thou...
Analytical Solutions for Circular Eddies of the Reduced-Gravity, Shallow-Water Equations
Circular Eddies Shallow-Water Equations Reduced-Gravity
2008/10/29
New analytical, circular eddy solutions of the nonlinear, reduced-gravity, shallow-water equations in a rotating system are presented. While previous analytical solutions were limited to the descripti...
Simple Models of Flow over Deep Ocean Sills: Planetary and Semigeostrophic Solutions
Simple Models Semigeostrophic Solutions Deep Ocean Sills
2008/10/29
Simple inverted reduced-gravity models of flow over deep ocean sills are considered, with emphasis placed on the case for which sills are wide with respect to the abyssal Rossby radius. When the lengt...
Internal Boundary Layer Scaling in “Two Layer” Solutions of the Thermocline Equations
Internal Boundary Layer Scaling Two Layer Thermocline Equations
2008/7/17
The diffusivity dependence of internal boundary layers in solutions of the continuously stratified, diffusive thermocline equations is revisited. If a solution exists that approaches a two-layer solut...
Subsurface maxima of phytoplankton and chlorophyll: Steady-state solutions from a simple model
chlorophyll: Steady-state solutions Subsurface
2014/5/21
In oligotrophic lakes and oceans, the deep chlorophyll maximum may form independently of a maximum of
phytoplankton biomass, because the ratio of chlorophyll to phytoplankton biomass (in units of car...