Q. What is the phenomenon of ‘cloudbursts’? Explain. (10 Marks)
Core
Demand of the Question ●
Discuss the phenomenon of cloudbursts. ●
Shed light on the characteristics of the cloudbursts. |
Answer
A cloudburst is
an extreme weather event characterised by sudden, intense rainfall over
a localised area, often within an hour, leading to flash
floods. For instance, in 2013, a cloudburst in Uttarakhand, India,
triggered devastating floods and landslides, illustrating the destructive
potential of such events, especially in mountainous regions.
Phenomenon
of Cloudburst:
- Rapid Upward Movement and
Orographic Lifting: Cloudbursts occur when warm, moisture-laden air
rapidly rises, cools, and condenses into dense clouds.
For example: In the Himalayas, steep terrain accelerates orographic lifting, causing heavy rainfall, as seen in the 2013 Kedarnath tragedy. - Localised Low-Pressure
Zones: The development of low-pressure areas in high-altitude regions
attracts moisture-laden winds, leading to heavy cloud formation and
eventual cloudbursts.
For example: The 2020 cloudburst in Himachal Pradesh can be linked to such low-pressure zones in the atmosphere. - Saturation of Air: When air
holds more moisture than it can sustain, any sudden atmospheric
disturbance can lead to excessive rainfall.
- Atmospheric Instability: Collisions
between warm, moist air and cooler air pockets create unstable atmospheric
conditions, triggering cloudbursts.
For example: The 2014 cloudburst in Jammu and Kashmir, which led to widespread destruction, was a result of such instability. - Global Warming and Climate
Change: Rising global temperatures have led to an increase in
atmospheric moisture levels, making cloudbursts more frequent and
intense..
Characteristics
of Cloudbursts:
- High-Intensity Rainfall: Cloudbursts
are defined by rainfall exceeding 100 mm in an hour, leading
to significant flooding.
For example: The Leh cloudburst of 2010 dumped an immense amount of rain in a very short period, overwhelming local drainage systems. - Localised Nature: Cloudbursts
typically affect small areas, less than 20-30 square kilometres.
For example: In 2022 Amarnath Yatra cloudburst, where a specific zone experienced extreme rainfall, causing rapid flooding. - Short Duration: Though
cloudbursts last only a few minutes to an hour, the intensity of rainfall
causes immense damage.
For example: The 2021 Uttarakhand cloudburst lasted for about 30 minutes, causing flash floods in several areas. - Sudden River Surge and Dam
Breach: Cloudbursts often cause a rapid and uncontrolled surge in
river water levels, putting immense pressure on dams, sometimes causing
breaches that result in catastrophic flash floods.
- Occurrence in Hilly
Regions: Cloudbursts are most common in mountainous regions like the
Himalayas, due to the orographic effect.
- Lack of Predictability: Cloudbursts
are difficult to forecast due to their sudden and localised nature.
As
climate patterns shift, the frequency and intensity of cloudbursts are expected
to rise, particularly in vulnerable areas. Enhanced weather
forecasting and disaster preparedness will be essential to
mitigate their impacts and help communities adapt to these unpredictable events
in the future.
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