Met. Dept warns of proper water management
The onset of the Southwest Monsoon to Sri Lanka usually takes place
during the third week of May each year. However in 2005, the monsoon
established over Sri Lanka only around 29th of May. Under normal
circumstances, during the first few weeks of its establishment, the
monsoon is fairly active and results in heavy rain and strong winds over
the southwestern part of the island. These adverse weather conditions
usually result in disasters such as floods, earthslips and wind damage
to parts of Galle, Matara, Colombo, Kalutara, Ratnapura, Kegalle and
Nuwara Eliya districts during the months of May and June.
In 2005, however, there were only a very limited number of such
events: minor floods in Galle and Kalutara during 28-29 May, strong
winds at Ambalangoda on May 29 and minor earthslips during June 8-9 at
Nawalapitiya. Hence the beginning of the Southwest Monsoon to Sri Lanka
this year was gentle with no serious damages.
Although the early part of the monsoon causes damages, rain which
occurs during this period particularly in the hydro-catchment areas is
extremely important. Major hydroreservoirs situated in the western
slopes of the central hills depend very heavily on these rains.
The total rainfall receive during the month of June is near average
only in the districts of Colombo and Kalutara. In all the other
districts, the values are below normal. The total rainfall received in
the hydro-catchment areas during the period lies between 60-70% of the
average.
During July and August, the monsoon is very likely to be
comparatively less active in terms of rainfall. Furthermore, it is more
likely to confine more to the southwestern parts of the country. Global
forecast models too do not predict significantly heavy rainfall over Sri
Lanka area during the next few months. Therefore, it is extremely
necessary at this moment to properly manage water in order to minimize
the consequences associated with water shortages, states a press release
issued by the Department of Meteorology. |