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Figure 11.23 The characteristic air
circulation over South and East Asia
in summer. Solid lines indicate airflow
at about 6000 m and dashed lines at
about 600 m. Note that the low-level
flow is very uniform between about
600 and 3000 m.
Sources : After Thompson (1951), Flohn
(1968), Frost and Stephenson (1965), and
others.
Figure 11.24 Mean onset date of the summer monsoon over South and East Asia.
Source : After Tao Shi-yan and Chen Longxun. From Domrös and Peng (1988). Reproduced by permission of Professor Tao Shi-yan and the
Chinese Geographical Society, and Springer-Verlag.
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