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50<br />
area) than in the surface isobaric analysis. In this section an instance of this<br />
type of aynoptic situation will be discussed.<br />
18.2 From 23rd October 1971 onwards, the seasonal trough was well-marked<br />
over south Arabian Sea, south Peninsula and south Bay of Bengal. A low pressure<br />
area (clearly seen in the upper air) moved westwards across the south Peninsula<br />
between 23 and 25 and reached Laccadives area on 25th. On this day,<br />
line also ran roughly along 9°N on the surface (Fig. 18.1) and in the lower troposphere,<br />
from Laccadives to extreme south Vietnam coast<br />
Extended<br />
charts showed that the trough extended as far east as southwest Pacific with a<br />
number of embedded lows in it (Fig. 18.3). The trough was seen upto 3.6 km<br />
(Fig.18.3)<br />
without any noticeable tilt with height./ Both the easterlies and westerlies (on<br />
either side of the trough line) were moderate to strong, the strength being on<br />
an average about 15/20 kts. Even though the low pressure area had moved to<br />
laccadives, still an elongated closed isobar could be drawn over south Bay and<br />
south Andaman Sea. The rainfall on this day was fairly widespread over the<br />
Peninsula south of Lat. 13°N. The significant amounts were close to the trough<br />
line and they were moderate to rather heavy. Monsoon was active in Tamil Nadu.<br />
This increased activity was partly due to the low pressure area moving westwards;<br />
across the area in the<br />
24 hrs.<br />
18.3 Cloudiness and light precipitation extended in the north upto about<br />
Lat. 20°N. The upper air charts showed that air was considerably dry at all<br />
levels to the north of Lat. 20°N. To the south of Lat. 20°N, the easterlies we::e<br />
more or less uniformly moist., This was also reflected in the surface dew point<br />
distribution. Thus,there was a pronounced moisture discontinuity across the<br />
country along Lat. 20°N, which was also the northern limit of weather and cloud<br />
belts.<br />
<strong>18.4</strong> On the 26th also the situation was nearly similar except that the<br />
trough extended upto 6.0 km. On this day also significant rainfall amounts were