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No. IV-18.4 - (IMD), Pune

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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

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