quasi-geostrophic motions in the equatorial areas matsuno (1966) todd barron eas 8802 2 oct 2007
TRANSCRIPT
Quasi-Geostrophic Motions in the Equatorial Areas
Matsuno (1966)
Todd Barron
EAS 8802
2 Oct 2007
Purpose of what Matsuno attempted to accomplish
• Discuss the behaviors of the Rossby and gravity waves in the equatorial area (more precise than previous studies) and to answer the following questions:
1. Can we get 2 waves of different types in the tropics?
2. Is there quasi-geostrophic motion even at the equator?
3. Is it possible to eliminate the gravity oscillations by use of the filtering procedures?
Background
• In tropical regions, there are 2 types of waves can be obtained: Rossby and gravity.
• What separates these waves are the difference in frequencies and their relationship to pressure and velocity fields.
• As we will see, waves confined near the equator exhibit both gravity and Rossby characteristics.
The Model
• Matsunso used the “divergent barotropic model” (a layer of incompressible fluid of homogenous density w/ a free surface under hydrostatic balance).
• Foundation of most of the derived equations:
The Model
• Matsuno converted the basic equations into non-dimensional form:
Taking units of T and l as:
We can now transform to non- dimensional form:
Frequency Equation
• Derived to consider E-W propagating waves.• Matsuno started with the basic eqs. and assumed a factor of e so now we
have:
iωt+ikx
Eliminating u and φ gives us:
with boundary conditions of: v0 when y-+∞
Boundary conditions are only satisfied when the
constant, is equal to an odd integer now written as:
Frequency Equation
• The previous equation gives a relation b/t the frequency and the longitudinal wave number for some meridional mode.
• The equation is a cubic root to ω. Therefore we have 3 roots when the wave number and frequency is given. Two roots are expected to gravity waves (one E and W propagating) and the other being a Rossby wave.
Frequency Equation
• By solving the cubic equation with arbitrary k values, Matsuno was able to graphically show frequencies:
Frequency Equation
• What if n=0?• 3 roots will be obtained from ω
• Plugging n=0 into the equation and factoring yields:
• Matsuno was able to classify the 3 roots as:
When he consider a continuous parameter of:
Frequency Equation
• So, for n=0, the frequency of the E propagating gravity wave is NOT separated from that of the Rossby wave… they coincide at k=1/√2
• Matsuno suggested that one of the roots should be rejected since the boundary conditions are not satisfied when we solve for φ in the following relation:
Frequency Equation
• So what does all that boil down to?• The westward propagating gravity wave and Kelvin
wave do NOT exist in the lowest mode (close to Equator).
• What we have is a combo of the two.
Equatorial Waves• Matsuno’s eigenvalues obtained can be graphically shown:
Equatorial Waves
Summing up Matsuno’s diagrams
• No marked difference b/t the Rossby and gravity waves confined near the Equator. Cannot apply mathematical filtering to equatorial motions since there are no physical reason to distinguish the two.
Wave Trapping
• Matsuno investigated this topic more thoroughly than previously studies.
• Found that propagation velocity is larger for higher latitudes, which means the wave generated near the equator will be reflected and reflected toward the equator.
• Not the case for Rossby waves• Suggested more studies needed to be done
concerning what way the wave is refracted or trapped.
Forced Stationary Motion
• Matsuno considered a stationary state resulting from some external causes.
Transformed to non-dimensional terms
w/ boundary conditions of:
Forced Stationary Motion
Conclusion
• At the lowest mode, the westward propagating wave exhibits features found in both Rossby and gravity waves.
• At lower modes, Rossby and gravity waves are confined near the equator
Conclusions
• For stationary motions, high and low pressure cells are split along the equator.
• Caused by deviations of the sfc elevations being less that that in higher latitudes in magnitude.
• Because of this, strong zonal flow is noticed along the equator.