1 / 12

Section 5 Atmospheric Waves: Introduction

Section 5 Atmospheric Waves: Introduction. Clouds: why are they regularly spaced?. Vertical Velocity ( w ) Field During a Model Initial Adjustment Periods. 200 hPa Geopotential Height Composite during El Nino Events : The Pacific-North American (PNA) Pattern.

luna
Télécharger la présentation

Section 5 Atmospheric Waves: Introduction

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Section 5 Atmospheric Waves:Introduction

  2. Clouds: why are they regularly spaced?

  3. Vertical Velocity (w) Field During a Model Initial Adjustment Periods

  4. 200 hPaGeopotential Height Composite during El Nino Events: The Pacific-North American (PNA) Pattern How does a tropical forcing induce a stationary wave train pattern extending to the extratropics? Years: Nino 3.4 
1958: 1.607 
1966: 1.308 
1973: 1.639 
1983: 2.548 
1987: 1.254 
1992: 1.820 
1995: 1.013 
1998: 2.396 
2003: 1.162

  5. What are waves? What if you throw a rock into the lake? Waves are oscillations (in field variables, such as velocity or pressure) that propagate in space.

  6. One-dimensional wave:

  7. Two-dimensional wave:

  8. What are we going to do? • Linearize the governing equations using the perturbation method • Derive the analytic wave solution • What is the dynamic mechanism of the wave? • What determines the wave propagation speed? • Group velocity and wave dispersion

More Related