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East Asia and Western Pacific METEOROLOGY AND CLIMATE

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339<br />

100 110 120 130<br />

Fig.3 The synoptic situation over eastern <strong>Asia</strong> at<br />

OOOOGMT 04 February 1979, as analysed<br />

by the Japan Meteorological Agency.<br />

Fig. 4 The synoptic situation over eastern <strong>Asia</strong> at<br />

OOOOGMT 05 February 1979, as analysed<br />

by the Japan Meteorological Agency.<br />

1979/2/04/002 1000 MB TEMP-GRAO-CC/IOOKM] 1979/2/04/QOZ 950 MB PV C*PVU3<br />

Fig.5 The horizontal temperature gradient at 1000<br />

Hpa at OOOOGMT 04 February 1979. The<br />

contour interval is 0.5 C/lOOkm.<br />

Fig.6 The potential vorticity at 950 Hpa at<br />

OOOOGMT 04 February 1979. The contour<br />

interval is 0.5 PV unit.<br />

1979/2/04/002 1000 MB CU,.V3 1979/2/04/OOZ 700 MB CU.J/}<br />

Fig.7 Hie horizontal wind field at 1000 Hpa at<br />

OOOOGMT 04 February 1979. The length<br />

scale of the vectors is such that the longest<br />

vector corresponds to the magnitude of 10<br />

m/sec.<br />

Fig.8 The horizontal wind field at 700 Hpa at<br />

OOOOGMT 04 February 1979, The length<br />

scale of the vectors is such that the longest<br />

vector corresponds to the magnitude of 10<br />

m/sec.

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