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Adiabatic nonlinear waves with trapped particles: Part III. Wave dynamics
Adiabatic nonlinear waves trapped particles Wave dynamics
2011/8/4
Abstract: The evolution of waves with trapped particles is described within the Lagrangian model developed in Paper I. One-dimensional nonlinear Langmuir waves with deeply trapped electrons are addres...
Edge-Based Compartmental Modeling for Infectious Disease Spread Part III: Disease and Population Structure
Infectious Disease Part III Disease and Population Structure
2011/9/29
We consider the edge-based compartmental models for infectious disease spread introduced in .These models allow us to consider standard SIR diseases spreading in random populations. In this paper we s...
Investigation of the Forecasting Error of a Simple Barotropic Model with the Aid of Empirical Orthogonal Functions. Part III
meteorology Measurement Forecasting Error
2009/6/18
Investigation of the Forecasting Error of a Simple Barotropic Model with the Aid of Empirical Orthogonal Functions. Part III.
The Interaction of the Monthly Mean Flow and Large-Scale Transient Eddies in two Different Circulation Types.Part III
Interaction Monthly Mean Flow Transient Eddies Circulation Types meteorology
2009/6/16
The Interaction of the Monthly Mean Flow and Large-Scale Transient Eddies in two Different Circulation Types. Part III.
A review of biomass burning emissions part III: intensive optical properties of biomass burning particles
biomass burning emissions optical properties biomass burning particles
2009/2/7
Because of its wide coverage over much of the globe, biomass burning has been widely studied in the context of direct radiative forcing. Such study is warranted as smoke particles scatter and at times...
On the Formation of Whitecaps by a Threshold Mechanism. Part III：Field Experiment and Comparison with Theory
Whitecaps Threshold Mechanism Field Experiment
2009/2/6
This paper is the third in a series of papers which seek to evaluate the hypothesis that deep water whitecapping is predictable in terms of a threshold mechanism involving the vertical acceleration. P...
Normal Modes of the World Ocean. Part III：A Procedure for Tidal Synthesis
World Ocean Procedure Tidal Synthesis
2009/1/21
In preceding parts of this study a set of normal modes was constructed as a basis for synthesizing diurnal and semidiurnal solutions of Laplace's tidal equations. The present part describes a procedur...
Circulation on the Continental Shelf of the Southeastern United States. Part III：Modeling the Winter Wind-Driven Flow
South Atlantic Bight Continental Shelf Winter Wind-Driven Flow
2009/1/20
A vertically integrated two-dimensional model has been adapted for the study of the wind-driven flow on the South Atlantic Bight (SAB) shelf during the winter season. Wind data are used as an input to...
A Three-Dimensional Simulation of the Hudson–Raritan Estuary. Part III：Salt Flux Analyses
Three-Dimensional Simulation Hudson–Raritan Estuary Salt Flux Analyses
2009/1/16
Salt fluxes and volume transports in an estuary vary considerably over subtidal time scales of a few days to weeks in response to wind and neap–spring tidal forcings. Results from a numerical simulati...
Columnar modelling of nucleation burst evolution in the convective boundary layer – first results from a feasibility study Part III: Preliminary results on physicochemical model performance using two "clean air mass" reference scenarios
nucleation burst convective boundary layer feasibility study physicochemical model performance
2009/1/15
In Paper I of four papers, a revised columnar high-order model to investigate gas-aerosol-turbulence interactions in the convective boundary layer (CBL) was proposed. In Paper II, the model capability...
A Three-Layer Model for the Wind-Driven Circulation in a Subtropical–Subpolar Basin. Part III：Potential Vorticity Analysis
Three-Layer Model Wind-Driven Circulation Subtropical–Subpolar Basin Potential Vorticity Analysis
2009/1/5
Recent progress in thermocline theory is linked and demonstrated by a wind-driven three-layer numerical model. The dynamic balances of the circulation of the model are studied through examination of p...
The Formation of Labrador Sea Water. Part III：The Evolution of Oxygen and Nutrient Concentration
Labrador Sea Water Oxygen Concentration Nutrient Concentration
2009/1/5
Oxygen, nutrient, and tritium concentrations observed in the western Labrador Sea in March 1976 during deep convective renewal of Labrador Sea water are analyzed to show how a newly formed water mass ...
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...
L’Histoire Physique de la Mer. Part III：On the Motions of Seawater
currents waves tides Seawater movements
2008/12/11
Seawater movements are of three kinds: currents, waves, and tides. Observations were made five times a day for three and one-quarter months in the Strait of Cassis. Mariners' reports of a westward cur...
A New Coastal Wave Model. Part III：Nonlinear Wave–Wave Interaction
Coastal Wave Model Nonlinear Wave–Wave Interaction
2008/11/26
Resonant wave–wave interaction processes are studied with the nonlinear dispersion relationship for shallow water. The formulation was derived based on a Hamiltonian representation first reported by Z...