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regular-article-logo Wednesday, 08 May 2024

Rain forecast for Sunday in south Bengal

In south Bengal, and couple of districts of north Bengal, heat wave conditions are likely to last another 24 to 48 hours

Debraj Mitra Calcutta Published 21.04.23, 05:31 AM
A civic volunteer splashes water on his face for relief from heat at Burdwan

A civic volunteer splashes water on his face for relief from heat at Burdwan Picture by Munshi Muklesur Rahaman 

The prolonged heat wave conditions in Calcutta and the rest of Bengal are set to end with a rainy spell, the Met office said on Thursday.

“In south Bengal, including Calcutta, the showers are most likely on April 23 and 24,” said Sanjib Bandyopadhyay, the deputy director-general of the India Meteorological Department, Calcutta.

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The coastal districts of South 24-Parganas and East Midnapore might get some rain on April 22 as well. The Darjeeling hills, where the rain started on Wednesday, are likely to be wet till April25.

In south Bengal, and a couple of districts of north Bengal, the heat wave conditions are likely to last another 24 to 48 hours.

The Met office had issued a formal heat wave alert for south Bengal on April 12.

On Thursday, the Celsius inched towards the 41-degree mark in Calcutta. Many districts were hotter.

The Met office recorded a maximum temperature of 40.7 degrees in Alipore. Salt Lake and Dum Dum sizzled at 41.5 and 41.7 degrees, respectively. Bankura kept up being the hottest district in Bengal, with a maximum temperature of 44.3 degrees.

The mercury was 43.6 degrees Celsius at Sriniketan and 43.9 at Panagarh. Asansol recorded a temperature of 42.9 degrees Celsius, Jhargram registered a reading of 42.5. In Malda, the temperature was 42.1 degrees Celsius on Thursday.

Not alone

The heat wave in Bengal is not an isolated weather phenomenon. Southeast Asia is enduring an unprecedented heat wave, one that is being billed as the “worst-ever” recorded in April.

Several all-time high-temperature records have been broken, including a 113.7 degrees Fahrenheit (45.4 degrees Celsius) in Thailand last Friday, the nation’s hottest reading on record.

“Vast parts of Southeast Asia are going through an unusually hot spell. A high-pressure area on the Bay of Bengal is moving eastwards from the Indian coast, leading to a rise in temperature in Thailand, the Philippines and parts of China,” said a Met official.

Wind play

The dominance of dry northwesterly winds and the lack of moisture-laden southerly winds from the Bay has been the two main factors behind the prolonged heat wave, according to Met officials.

Usually, dry northwesterly winds are active in Bengal this time of the year, but not throughout the day. As evening approaches, moisture-laden southerly winds from the Bay start entering the coast. Strong southerlies often enter well beyond 100km from the coast.

The heating and the southerly winds together create ideal conditions for thunderstorms.

“But this time, the northwesterly winds are so strong that they are crossing the coast. The southerlies on the sea cannot make their way to the coast, leave alone more inland areas,” said Bandyopadhyay.

Changemaker

An extratropical storm that originates from the Mediterranean region and oftencauses winter rain and snowfall in India is tipped to helptilt the weather scales in Bengal.

“A western disturbanceis passing through eastern India. Darjeeling got hailstorms under its effect on Wednesday. In the coming days, the system is likely to cause rain in south Bengal,” said a Met official.

A western disturbance reaches northwestern India via Iran, Afghanistan and Pakistan. It then keeps moving east through the upper reaches of the country, usually passing over Sikkim and Arunachal Pradesh.

“The system leads to the formation of a trough line that causes rain in Uttar Pradesh, Nepal, Sikkim, Bhutan and Arunachal Pradesh. But when the system is deep, the trough line descends enough to cause rain in Bihar, Jharkhand and Bengal. This is what is likely in the coming days,” said the official.

Lift needed

The mere presence of moisture is not enough for the formation of thunderclouds.

“There has to be a lifting mechanism. A cyclonic circulation or a troughof low pressure helps themoisture-laden winds rise from the surface of the earth. The moist winds need a helping hand for around 5km from the earth’s surface. After that, they can rise on their own. But that initial helping hand is very crucial,” said a weather scientist.

The trough line that is expected to take shape in the coming days will serve that purpose, he said.

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