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East Asia and Western Pacific METEOROLOGY AND CLIMATE

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arc around the Plateau is seen between mid <strong>and</strong> lower latitudes of<br />

the eastern <strong>Asia</strong>n continent, with NW (NE) winds north (south) of<br />

30°N,which is obviously in close relation to the flow-steering role<br />

of the orography. The 36~h integration indicates that NE winds in<br />

the southern part of the Sea keeps on intensifying <strong>and</strong> extending<br />

westward to the northern Indian, with the maximum wind center of 8<br />

m/s displaced southward to the central South-China Sea. At the 48 h<br />

the surge has moved further southward, with the NE wind of 6 m/s<br />

reaching equatorial latitudes <strong>and</strong> a reduced wind region of 8 m/s<br />

travelling westward to the Bay of Bengal. The 60~h result indicates<br />

that the maximum NE wind has dropped to 6 m/s, implying that the<br />

surge is beginning to weaken.<br />

It can be seen in Fig.3a that, north of 5°N, after the starting<br />

of integration,the V - isopleths are getting N - S directed <strong>and</strong> become<br />

closer together,suggest ing that the northerly wind strengthens<br />

rapidly in the first 12 hr, whereas for 5 N <strong>and</strong> south of it the reinforcement<br />

is initiated at the 12th hr. At the 72-h integration<br />

no northerly wind is seen at 25°N, indicating the cutoff of cold<br />

air supply, thus suggesting that the surge moves into the decaying<br />

stage. A salient feature displayed in Fig.Bb is that temperature<br />

drop south of 25°N occurs after the integration of 12 hr.lt follows<br />

that the enforced northerly wind due to the surge is always ahead<br />

of temperature drop caused by it, which may be explained by the<br />

character of cold surges as gravity waves *^.<br />

In the 120°E cross section at the 24-h integration (Fig.4a) the<br />

local Hadley cell intensifies to a considerable degree, with the<br />

ascending leg around the equator <strong>and</strong> in the Southern Hemisphere<br />

<strong>and</strong> descending leg equatorward of 20°N. In the 48-h cross section<br />

(Fig»4b) the surge-caused near-surface northerly flow extends to<br />

equatorial latitudes <strong>and</strong> the ascending leg of the cell ahead of the<br />

surge retreats to 5°S <strong>and</strong> south of it* Fig.4c gives the difference<br />

in vertical speed (fl^gr- w pA^* which shows enhanced legs of the cell.<br />

Hence, in the southward travel of the surge, the Hadley cell retreats<br />

<strong>and</strong> intensifies.

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