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East Asia and Western Pacific METEOROLOGY AND CLIMATE

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126<br />

(a)<br />

OEOPOTEHTIflL FRED<br />

(A]<br />

VEKT1CRL MOTION FIELD AT HlOTKOPOSfHEKE<br />

W..10000 Htt. MT.M.S *C<br />

MtitfOOOO HK. tSUri.K *C<br />

B.w/o.O<br />

ZONAL CURSE<br />

tDECREE)<br />

(b)<br />

ZONRL MIND FIELD<br />

(t) VERTICflL MOTION FILED »1<br />

HL*DOOO KM. SST=«.S *t<br />

W-tlOOOO KR. SSUZS.S *C<br />

£ «<br />

%<br />

I.,<br />

ZONAL fHftSE I DECREE I<br />

ZONAL CMBSE fDECREE I<br />

Fig. 2. Horizontal structure of the<br />

unstable wavenuniber two at SSIM=29.5°C:<br />

(a) geopotential ., (b) zonal wind,<br />

u , (c) meridional wind, v., (d) 0)2><br />

<strong>and</strong> (e) w e . Solid <strong>and</strong> dotted lines<br />

denote positive (or zero) <strong>and</strong> negative<br />

contours, respectively. Contour intervals<br />

for 4>_ <strong>and</strong> u. are 10% of the<br />

maximum value <strong>and</strong> those for v_, o} 2 , <strong>and</strong><br />

o) e are 201 of the maximum value.

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