On Friday, a lifeguard passes through the abandoned beach Kovallam when tourists are forbidden because of bad weather and harsh sea.
Since the southwestern monsoon slipped into the crank phase of two rounds of intense spells above Keraral since the beginning of May 24, in June there is now no main charm with rainfall limited to some pockets, although light to medium showers will continue.
The state cumulatively accepted over 800 mm rains since the monsoon began his journey north of Keralay.
With regard to the average monthly Kerala rainfall in June, which is 648 mm, the state received excessive rain in the first four weeks of monsoon. However, Monsoon is still normal in Kerala according to the monsoon chart of the Indian meteorological department (IMD), because it considers 440.5 mm received in the opening magic of the monsoon between May 24 and 31, as before Monsoon rain.
Without any main weather systems in Bengal and the Arab Sea for Keral and weakening Westerlies, Monsoon rain will be suppressed for the next two weeks.
“We expect a revival or other intense charm only until the end of July,” says Neetha K. Gopal, director of IMD, Thiruvananthapuram. The specialty of the monsoon this year was the high depth of western wind influenced by a large atmospheric element.
According to the scientists, this time was a strong Somali stream, the cross -equity system of the wind. The monsoon wind enters the Indian subcontinent as a Somali beam with a wind from the Mascarene Islands high -pressure cell on Madagascar entering the African country and emerges back to the Indian Ocean and then to the Arab Sea as Somali stream.
Low -pressure cells existed in the Arab Sea, and then depression formed above the Bengal Gulf of the last week of May, helping the monsoon to move quickly to the ground.
Although Monsoon covered Karnataka very quickly and in the last week of May gave some intense magic of rain for Keral, his progress to the north has been slow since then, especially on June 1, which increases the suspicion of false onset.
Permanent and semi -hot features such as offshore Crough have not developed from today and the monsoon trough is not yet clear, as it is merged with the existing low -pressure system in the north.
The boreholes at the sea associated with the coastal trough launched torrential rain in July last year and caused catastrophic landslides in Kerala.
The delay in the formation of offshore trough and associated vortex along the west coast is likely to give Keraral in July, as traditionally July represents the highest precipitation in the four -month southwest monsoon season in Kerala. Similarly, although the state received some intense charms, extreme rains categories have been limited to several stations several times.
Published – June 20, 2025 20:51 is
