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East Asia and Western Pacific METEOROLOGY AND CLIMATE

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238<br />

west of the maximum cloud cover region.<br />

The zonal winds are out of phase at<br />

the upper <strong>and</strong> lower levels.<br />

On the basis of the preceding discussion, it is our view that the 30-50<br />

day oscillation in the equatorial atmosphere is not produced by the Kelvin<br />

wave, but is primarily caused by the cloud wave.<br />

In the present quasidiabatic<br />

geostrophic model, the Kelvin wave is filtered out.<br />

In the present<br />

quasi-dialictic geotrophic model, the Kelvin wave is filtered out.<br />

This is<br />

similar to the case where the gravity wave is removed from the quasi-geostrophic<br />

model in the midlatitudes.<br />

From the traditional viewpoint of the dynamics of the midlatitudes, the<br />

motion systems play the dominant role, whereas the formation of clouds is<br />

subject to the motion systems.<br />

However, from the st<strong>and</strong>point of the cloud wave<br />

for the tropical low frequency motion, the role of cloud systems <strong>and</strong> atmospheric<br />

motions is reversed.<br />

The cloud system plays the leading role, while<br />

the motion systems are secondary <strong>and</strong> are determined by the cloud systems<br />

through the cloud-radiative heating.<br />

References<br />

Anthes, R. A., 1977: A cumulus parameterization scheme utilizing a onedimensional<br />

cloud model. Hon. Wea. Rev., 105, 270-286.<br />

Chang, C. P., <strong>and</strong> H. Lim, 1988: Kelvin wave-CISK: A possible mechanism for<br />

the 30-50 day oscillations. J. 'Atznos. Sci., 45, , 1709-1720.<br />

Charney, J, G., 1963: A note on large scale motions in the tropics, J.<br />

Atmos. Sci., 20, 607-609.<br />

Gill, A. E. , 1980: Some simple solutions for heat induced tropical circulation.<br />

Quart. J. Roy. Meteor. Soc., 106, 447-462.<br />

Gray, W. M., E. Ruprecht, <strong>and</strong> R. Phelps, 1975: Relative humidity in tropical<br />

weather systems. Mon. Wea. Rev. 103, 685-690.

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