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East Asia and Western Pacific METEOROLOGY AND CLIMATE

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the equations <strong>and</strong> so on. Then performing coupled or uncoupled model test<br />

with the model are possible.<br />

In the uncoupled model test, SST deviation is stationary, which implies<br />

linear <strong>and</strong> nonlinear response of analogous evolution of monthly averaged<br />

circulation to stationary SST forcing. In the coupled tests, control test is<br />

done at first. On the basis of this, various sensitivity studies are made. The<br />

results not only prove the result of the theoretical analysis, but also provide<br />

a basis for utilizing further this model to do seasonal long—term numerical<br />

forecast.<br />

4. Discussion<br />

It has been shown in the analysis of actual data that there is a temporal<br />

teleconnection in the general circulation, one of which is the analogous<br />

rhythm of monthly averaged circulation. The author believes that it is true.<br />

In spite of this the truth of this phenomenon can still be doubtful because of<br />

the vagueness in this phenomenon <strong>and</strong> the limitation of the statistical methods<br />

<strong>and</strong> sample error appearing in the study.<br />

As to the mechanism of the establishment of rhythm, the current study is<br />

still preliminary. Although the rhythm has been simulated with a numerical<br />

model, the physical mechanism is still ambiguous. To some extent the problems<br />

solved far less than that those produced. Further study should be done<br />

to realize the mechanism of the formation of climate anomalies on a seasonal<br />

scale <strong>and</strong> present a numerical climate forecasting method.<br />

REFERENCES<br />

[I] Chou, J.F., Long-range numerical weather prediction, Meteorological press,<br />

Beijing, PP.329 (1986)(m Chinese).<br />

[2] Dickinson, A,, WMONWP Annual Progress Report for 1987,195-196(1988).<br />

[3] Lau, N.C., Mon. Wea. Rev., 109,2287-311(1981).<br />

[4] Lorenze. E.N., J.Atmos. ScL, 26,636-646(1969).<br />

[5] Madden, R.A., J.Geophys. Res., 86, No.lO(1981).<br />

[6] Marchuk, G.L, World Climate Conference, W.M.O. Geneva, 12-32, February,<br />

1979.<br />

[7] Musealyan, C.A.Meteorology <strong>and</strong> Hydrology, 3,1980 (in Russian).<br />

[8] Namias, J., <strong>and</strong> D.Cayan, Oceamis, 27,40-45(1984).<br />

[9] Owen, J., WMO NWP Annual Progress Report for 1987,195-196(1988).<br />

[10] QhvC.<strong>and</strong> J.Chou, Acta Meteor.Sinica 1,32-42(1987).<br />

II1] Shukla,!, J, Atmos. Sci. 38,2547-72(1981).<br />

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