Cyclones
Atmospheric Science · Part 4
180 KB9 sections3 key equationsLaTeX typeset
Table of Contents
- 1.Norwegian Cyclone Model
- 2.Vorticity and Cyclone Development
- 3.QG Omega Equation & Vertical Motion
- 4.Cyclone Structure
- 5.Baroclinic Instability & Growth Rates
- 6.Stage 1: Initial Perturbation
- 7.Stage 2: Development
- 8.Stage 3: Mature
- 9.Stage 4: Occlusion & Decay
Key Equations
$$\left(\nabla^2 + \frac{f_0^2}{\sigma}\frac{\partial^2}{\partial p^2}\right)\omega = \frac{f_0}{\sigma}\frac{\partial}{\partial p}\left[\mathbf{V}_g \cdot \nabla(\zeta_g + f)\right] + \frac{R}{\sigma p}\nabla^2\left[\mathbf{V}_g \cdot \nabla T\right]$$
$$\sigma_{\max} = 0.31 \frac{f}{N}\left|\frac{\partial u}{\partial z}\right| = 0.31 \frac{f}{N}\frac{\Lambda}{H}$$
$$\frac{\partial p_s}{\partial t} \propto -f_0\left[\mathbf{V}_g \cdot \nabla(\zeta_g + f)\right]_{500} - \frac{R}{p}\left[\nabla^2(\mathbf{V}_g \cdot \nabla T)\right]_{1000\text{--}500}$$
Equations are rendered with MathJax in the PDF with professional LaTeX typesetting.
Course Context
This PDF is part of the Atmospheric Science course on CoursesHub.World. Study the physics of weather and climate from atmospheric thermodynamics to planetary atmospheres. Covers atmospheric dynamics, synoptic meteorology, clouds and precipitation, radiation budgets, clima...