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An Analytical Study of Filtered Tropical Flows Using an Improvement of the Longwave Model Acknowledgements Wayne Schubert, Matt Masarik, Levi Silvers,

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Presentation on theme: "An Analytical Study of Filtered Tropical Flows Using an Improvement of the Longwave Model Acknowledgements Wayne Schubert, Matt Masarik, Levi Silvers,"— Presentation transcript:

1 An Analytical Study of Filtered Tropical Flows Using an Improvement of the Longwave Model Acknowledgements Wayne Schubert, Matt Masarik, Levi Silvers, Jonathan Vigh, CMMAP, and SOARS Program Alex O. Gonzalez

2 Overview -Theoretical studies vital because lack of numerical data in tropics -Analytical model using different filtering techniques -Use equatorial wave theory (on beta-plane) to gain insight on atmospheric phenomena such as MJO

3 -4 types of atmospheric waves in equatorial region: -Inertia gravity, Mixed-Rossby gravity, Rossby, and Kelvin waves -Most concerned with Rossby and Kelvin waves for MJO Wave Types

4 OLR Observations -Filter out inertia-gravity waves -OLR shows relative importance of wave types for MJO

5 Dispersion Diagram -Filters out inertia-gravity wave while retaining Kelvin waves

6 -Provides a better approximation of Rossby waves of all wavelengths Rossby Dispersion Approximation

7 -Two important models: Matsuno and Gill -Want to improve Gill model because it distorts short Rossby waves Analytical Models Matsuno Primitive Model Filtered Model Gill Longwave Model -Shallow-water primitive equations without forcings

8 -Gill model neglects, we use Gill Model vs. Filtered Model Gill model equationsFiltered model equations

9 Gill Model vs. Filtered Model -Using Ripa (1994) method of separating and h into Kelvin and non-Kelvin parts Gill using Ripa methodFiltered using Ripa method -Can do this because v=0 for Kelvin waves

10 -Need to solve a master equation for potential function, -1 st order dispersion relation, instead of cubic -Gill model dispersion relation does not contain Potential Function 

11 -Not easy to solve shallow-water equations with convective coupling, need to make assumptions -Follow framework of Ripa (1994) -Use arguments of PV, Geostrophic Flow, and Divergence -Learn more about importance of Rossby and Kelvin modes in MJO Forced Model

12 Gill, A. E. 1980. Some simple solutions for heat-induced tropical circulation. Quart. J. Roy. Meteor. Soc., 447-462. Matsuno, T. 1966: Quasi-Geostrophic Motions in the Equatorial Area. J. Meteor. Soc. Japan, 14, 25-42. Ripa, P. 1994: Horizontal wave propagation in the equatorial waveguide. J. Fluid Mech., 271, 267-284 Schubert, W. H., M. T. Masarik, L. G. Silvers, and A. O. Gonzalez 2008: A Filtered Model of Tropical Wave Motions. Q. J. R. Meteorol. Soc. (2008), 134, pp. 1-10. In Progress. Stevens, P. L., H.-C. Kuo, W. H. Schubert, and P. Ciesielski, 1990: Quasi-balanced dynamics in the tropics. J. Atmos. Sci., 47, 2262-2273. Wheeler, M.C., 2002: Tropical Meteorology: Equatorial Waves. In: J. Holton, J. Curry, and J. Pyle (eds), Encyclopedia of Atmospheric Sciences. Academic Press, 2313-2325. References

13 Horizontal structure


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