Збережено в:
Бібліографічні деталі
Автори: Duan, Jinqiao, Brannan, James R., Ervin, Vincent J.
Формат: Preprint
Опубліковано: 1999
Предмети:
Онлайн доступ:https://arxiv.org/abs/math/9901099
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author Duan, Jinqiao
Brannan, James R.
Ervin, Vincent J.
author_facet Duan, Jinqiao
Brannan, James R.
Ervin, Vincent J.
contents Stochastic dynamical systems arise as models for fluid particle motion in geophysical flows with random velocity fields. Escape probability (from a fluid domain) and mean residence time (in a fluid domain) quantify fluid transport between flow regimes of different characteristic motion. We consider a quasigeostrophic meandering jet model with random perturbations. This jet is parameterized by the parameter $β= (2Ω)/r \cos (θ)$, where $Ω$ is the rotation rate of the earth, $r$ the earth's radius and $θ$ the latitude. Note that $Ω$ and $r$ are fixed, so $β$ is a monotonic decreasing function of the latitude. The unperturbed jet (for $0 < β< 2/3$) consists of a basic flow with attached eddies. With random perturbations, there is fluid exchange between regimes of different characteristic motion. We quantify the exchange by escape probability and mean residence time.
format Preprint
id arxiv_https___arxiv_org_abs_math_9901099
institution arXiv
publishDate 1999
record_format arxiv
spellingShingle Escape Probability, Mean Residence Time and Geophysical Fluid Particle Dynamics
Duan, Jinqiao
Brannan, James R.
Ervin, Vincent J.
Dynamical Systems
Numerical Analysis
Analysis of PDEs
Probability
34F05, 65N30, 86A05
Stochastic dynamical systems arise as models for fluid particle motion in geophysical flows with random velocity fields. Escape probability (from a fluid domain) and mean residence time (in a fluid domain) quantify fluid transport between flow regimes of different characteristic motion. We consider a quasigeostrophic meandering jet model with random perturbations. This jet is parameterized by the parameter $β= (2Ω)/r \cos (θ)$, where $Ω$ is the rotation rate of the earth, $r$ the earth's radius and $θ$ the latitude. Note that $Ω$ and $r$ are fixed, so $β$ is a monotonic decreasing function of the latitude. The unperturbed jet (for $0 < β< 2/3$) consists of a basic flow with attached eddies. With random perturbations, there is fluid exchange between regimes of different characteristic motion. We quantify the exchange by escape probability and mean residence time.
title Escape Probability, Mean Residence Time and Geophysical Fluid Particle Dynamics
topic Dynamical Systems
Numerical Analysis
Analysis of PDEs
Probability
34F05, 65N30, 86A05
url https://arxiv.org/abs/math/9901099