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East Asia and Western Pacific METEOROLOGY AND CLIMATE

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mean vertical speed (W^ - K NM ) between 110-120°E at 24 <strong>and</strong> 48<br />

hr integration, respectively. From Pig.4 one can see that up- <strong>and</strong><br />

downdraft of the local Hadley cell shown in ALL are stronger than<br />

in NM, which suggests greater contribution of the vigorous surge to<br />

the excitation of the cell. Further, the cold front lifting is more<br />

intense in the presence of a large-scale orography than without.<br />

4. DISCUSSIONS <strong>AND</strong> CONCLUSIONS<br />

During the cold surge episode the leading edge differs from the<br />

vigorous NE wind center in the southward march as shown in ALL<br />

(see Fig.2). The former moves on average at about 51 m / s ar *d "the<br />

latter at 31 <strong>and</strong> 20 before <strong>and</strong> after arriving at 20 N, respectively,<br />

<strong>and</strong> close to zero when reaching 10 N. Subsequently, the NE wind<br />

center moves westward along the south side of the Plateau* On the<br />

other h<strong>and</strong>, the edge of the surge marches down to the south at approximately<br />

51 m / s when no such orography is available. For this<br />

reason, we think that cold air forced to move down along the east<br />

side of the Plateau may excite two types of waves. One is the fasttravelling<br />

gravity waves that bear no relation to the topography<br />

<strong>and</strong> so is probably excited by the cold front itself. It goes southward<br />

ahead of the front, thus causing the strengthening of the<br />

northerly wind at the leading edge of the surge to be prior to temperature<br />

drop. The other has characteristics of Kelvin waves, travels<br />

at a slow pace, depends on the orography for its existence<br />

<strong>and</strong> becomes non-existent apart from the Plateau. The second type<br />

occurring at the periphery of the topography with the wind direction<br />

nearly parallel to it is identified as the vigorous NE wind<br />

region behind the front.<br />

From the foregoing discussions the following points are summarized<br />

j<br />

(1) The Qinghai-Tibetan Plateau has no significant thermal effect<br />

on the propagation of eastern-<strong>Asia</strong>n cold surges;<br />

(2) The Plateau has, however, very pronounced dynamic effect on<br />

the surge. It steers cold air to move southward along the east side

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