Why are there so many cloud bursts in Uttarakhand?

Amid heavy rainfall in the region, a cloud burst occurred over Jamri and Tarkot hamlets in Jumma village area around 02:00 am on August 30. The excessive rainfall caused a huge landslide uphill leading to debris, muck deluge that buried about seven houses.

How does cloud burst happen?

Where does cloudburst happen? It usually occurs in high-altitude areas due to the formation of a low-pressure area on the top of a mountain. The low-pressure zone attracts clouds to the top of the mountain with great force. When they hit the peak, the moisture content is released in the form of rain.

How did Uttarakhand glacier burst happen?

A glacier burst took place on Sunday in Chamoli district of Uttarakhand after a chunk of Nanda Devi glacier broke off. It triggered an avalanche and a deluge crushing two hydroelectric power stations and washing away scores of homes.

What are the causes of flood in Uttarakhand?

A confluence of cyclonic storms forming in the Bay of Bengal and the Arabian Sea is among the biggest reasons behind heavy rains in different parts of the country over the past few days that have claimed dozens of lives in Uttarakhand, Kerala and other states, experts said on Tuesday.

Why cloud burst occurs in hilly areas?

Why did cloud burst in hilly areas? According to scientists, clouds filled with water get trapped in the mountainous regions. Due to the height of the mountains, the clouds are unable to move and then suddenly it starts raining at the same place.

Is cloud bursting real?

However, cloudbursts are infrequent as they occur only via orographic lift or occasionally when a warm air parcel mixes with cooler air, resulting in sudden condensation. The term “cloudburst” arose from the notion that clouds were akin to water balloons and could burst, resulting in rapid precipitation.

What is cloud burst explain with example?

cloudburst, a sudden, very heavy rainfall, usually local in nature and of brief duration. Most so-called cloudbursts occur in connection with thunderstorms. In these storms there are violent uprushes of air, which at times prevent the condensing raindrops from falling to the ground.

When did Uttarakhand glacier burst happen?

Disaster struck Uttarakhand’s Chamoli district on February 7, 2021 in the form of an avalanche and deluge, after a portion of the Nanda Devi glacier broke off.

Where did the glacier burst in Uttarakhand?

Chamoli district
The glacier burst took place near the India-China border in Chamoli district of Uttarakhand.

Which disaster usually occur in Uttarakhand?

Cloudburst is a natural and common phenomenon in the Himalaya, especially in Garhwal and Kumaon region of uttarakhand. Cloudburst and associated disaster affect thousands of people every year and cause loss of life, property, livelihood, infrastructure and environment.

How often do cloudbursts occur in Uttarakhand Himalaya?

Almost every year several parts of Uttarakhand Himalaya experience cloudburst and associated hazards.

What are cloud bursts in India?

With the beginning of south west monsoon season 2019, many Himalayan states started witnessing exceptional rainfall events known as Cloud Bursts. The extreme weather event – like previous years- caused large scale destruction in ecologically sensitive and remotely located vulnerable hilly areas.

What is the most destructive cloud burst incident In Uttarakashi?

The most destructive cloud burst incident in the state happened on Aug. 18 in which 17 people were killed and several went missing in Mori Block of Uttarakashi district. The unprecedented flash floods in Tons river wreaked havoc in Arakot, Sanel, Makudi and Tikochi villages, flattening number of houses and uprooting trees.

What caused Uttarakhand floods and landslides?

Torrential rains triggered by cloud bursts caused landslides and heavy floods that poured down hills in Uttarakhand, killing at least 9 people by Friday and destroying dozens of homes, officials said. Many people were trapped under toppled houses and debris unleashed by the landslides.