an analytical study of filtered tropical flows using an improvement of the longwave model
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An Analytical Study of Filtered Tropical Flows Using an Improvement of the Longwave Model. Alex O. Gonzalez. Acknowledgements Wayne Schubert, Matt Masarik, Levi Silvers, Jonathan Vigh, CMMAP, and SOARS Program. Overview. - PowerPoint PPT PresentationTRANSCRIPT
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
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
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-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
OLR Observations
-Filter out inertia-gravity waves
-OLR shows relative importance of wave types for MJO
Dispersion Diagram-Filters out inertia-gravity wave while retaining Kelvin waves
-Provides a better approximation of Rossby waves of all wavelengths
Rossby Dispersion Approximation
-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
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-Gill model neglects , we use
Gill Model vs. Filtered Model
Gill model equations Filtered model equations
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Gill Model vs. Filtered Model
-Using Ripa (1994) method of separating and h into Kelvin and non-Kelvin parts
Gill using Ripa method Filtered using Ripa method
-Can do this because v=0 for Kelvin waves
,,vu
-Need to solve a master equation for potential function,
-1st order dispersion relation, instead of cubic
-Gill model dispersion relation does not contain
Potential Function
-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
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-balanceddynamics 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
Horizontal structure