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An Overview of Surface Conditions in Numerical Simulations of Dust Devils and the Consequent Near-surface Air Flow Fields
Dust devil Convection Large eddy simulation (LES) Vortices Surface friction
2016/3/29
Dust devils are generally attributed to the near-surface conditions, usually the composite actions of the surface
parameters, such as heat flux, wind shear and surface friction. Dust devil scale (DD-...
A Simple Model for Stratified Shelf Flow Fields with Bottom Friction
Flow Fields Bottom Friction stratified shelf flow
2009/1/20
The effect of bottom friction on the subinertial frequency motion of stratified shelf flow fields is studied in a two-layer f-plane model with idealized shelf and slope bottom topography. Coastal-trap...
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...