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eastern region oil spill disaster contingency plan - Indian Coast Guard

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- 85 -<br />

surface currents over the Bay of Bengal of Bengal remain the same as that of<br />

month of January.<br />

8. Cyclonic Storms and Depressions. The Arabian sea is practically free<br />

from tropical storms in this month. In Bay of Bengal they are very few. They<br />

usually originate between latitude 5 deg to 9 deg North and west of longitude 92<br />

deg East during the winter season. The frequency of formation of Cyclone and<br />

Depression per year is 0.04. These systems initially move NW-Nly direction and<br />

cross the Tamil Nadu or East <strong>Coast</strong> of Srilanka. However, on some occasions<br />

after initial movement they may recurve and move in N-NNEly direction and<br />

strike the Arakkan <strong>Coast</strong>.<br />

March<br />

9. General. The month of March, April and May constitute the premonsoon<br />

season also called as Hot weather period. The main synoptic features<br />

that are generally observed during these months, with a special reference to<br />

coastal areas are given in the succeeding paragraphs.<br />

10. Synoptic Features. During the month of March, a Heat low establishes<br />

itself over the southern peninsula as a result of heating of the interior<br />

landmasses. The heat low is shallow with no well-defined upper air circulation. It<br />

is well marked only during the afternoon / evening hours.<br />

11. Pressure Pattern. The pressure gradient over the entire country is<br />

slack. The pressures are however slightly higher over <strong>Indian</strong> sea areas. The<br />

center of high pressure cells, during the month lies at about 18 Deg North / 60<br />

Deg East in the Arabian sea and 16 Deg North / 90 Deg East in the Bay of<br />

Bengal.<br />

12. Wind Discontinuity: In association with the high pressure cells over<br />

Arabian sea of Bay of Bengal, a North –South wind discontinuity line develops<br />

over the central parts of India with N/NWly winds on one side and S/SEly wind<br />

on the other side. It normally joins with another discontinuity line is potential<br />

area of thunderstorm / thunders activity.<br />

13. Land and Sea Breeze. Since the pressure gradient over the country is<br />

slack during March and sea breezes become pronounce in the coastal areas,<br />

particularly in the late afternoon hours.<br />

14. Thunder Storms. During the Hot Water Period extensive connective<br />

activities occur causing thunderstorms hailstorms and dust storms, on days<br />

having favorable synoptic situation. In general, thunder activity starts by March

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