CLOUDBURST
1. Context
Following heavy rains in Himachal Pradesh recently, landslides have occurred in the state with at least 22 people dead. Of those who have died, nine people got buried underneath the rubble of a collapsed temple and some houses in Shimla. Uttarakhand has also witnessed high rainfall.
2. Cloudburst
- A cloudburst is a sudden and intense weather phenomenon characterized by a heavy and rapid release of precipitation from a cloud.
- This concentrated burst of rainfall can lead to flash floods, landslides, and other forms of water-related disasters in a very short period of time.
- Cloudbursts typically occur in areas with high humidity and convective activity, such as mountainous regions, coastal areas, and places prone to thunderstorms.
3. How do Cloud bursts Occur?
Cloudbursts typically occur in regions with convective activity, such as areas prone to thunderstorms, mountainous terrain, and coastal regions. They are often associated with towering cumulonimbus clouds, which are large and vertically developed clouds capable of generating intense rainfall and thunderstorms. Here's how a cloudburst happens:
- Formation of Cumulonimbus Clouds: Cloudbursts are most commonly associated with cumulonimbus clouds, which are towering clouds formed through the process of convection. Warm air near the Earth's surface rises, cools, and condenses into water droplets as it encounters cooler air at higher altitudes. This process leads to the formation of these large, vertically oriented clouds.
- Updrafts and Water Vapor: Inside a cumulonimbus cloud, strong updrafts of air carry water vapor from lower altitudes to higher altitudes within the cloud. As the air rises, it cools and the water vapor condenses into tiny water droplets or ice crystals.
- Collision and Coalescence: Within the cloud, water droplets and ice crystals collide and combine, forming larger droplets. As these droplets continue to collide and grow in size, they become too heavy for the updrafts to support, causing them to fall.
- Downdrafts: The larger water droplets and ice crystals begin to descend as downdrafts within the cloud. As they fall through the cloud, they can pick up additional moisture, further increasing their size.
- Precipitation Release: Eventually, the water droplets and ice crystals become large enough that the force of gravity overcomes the upward force of the updrafts, and they start to fall rapidly toward the Earth's surface. This is the point at which the cloudburst occurs. The droplets fall in large quantities over a relatively small area, resulting in intense rainfall within a short timeframe.
- Impact and Consequences: The rapid and concentrated release of precipitation from the cloudburst can overwhelm drainage systems, lead to flash floods, and trigger landslides, especially in areas with steep terrain. The intensity of the rainfall can result in immediate and severe flooding, causing damage to property, and infrastructure, and posing risks to human safety.
4. Causes of Cloud Bursts
- Atmospheric Instability: Cloud bursts often occur in regions with convective instability in the atmosphere. Convective instability refers to the situation where warm and moist air near the Earth's surface rises rapidly due to its lower density compared to the surrounding cooler air. This vertical motion can lead to the formation of towering cumulonimbus clouds that are capable of generating intense rainfall.
- Moisture Availability: The presence of abundant moisture in the atmosphere is essential for the formation of cloud bursts. When warm, moisture-laden air rises and condenses at higher altitudes, it releases latent heat, which further fuels the upward motion of air. This process can lead to the development of strong updrafts within clouds and the rapid accumulation of water droplets.
- Orographic Effects: Cloudbursts are often common in mountainous regions due to orographic lifting. When moist air is forced to rise over a mountain range, it cools and condenses, leading to the formation of clouds and potentially intense rainfall. The combination of orographic lifting and convective instability can enhance the likelihood of cloud bursts in these areas.
- Frontal Boundaries: Cloudbursts can also occur along frontal boundaries, where two air masses of differing temperatures and moisture content meet. The convergence of these air masses can create strong vertical motion and promote the development of thunderstorms and heavy rainfall.
- Cumulonimbus Clouds: Cloud bursts are often associated with cumulonimbus clouds, which are large and vertically developed clouds capable of generating intense weather. These clouds are formed through the process of convection, where warm air rises, cools, and condenses into cloud droplets. The presence of cumulonimbus clouds increases the likelihood of intense rainfall and thunderstorm activity.
5. Consequences of Cloud Bursts
The consequences of a cloud burst, which is a sudden and intense release of precipitation from a cloud, can be significant and often lead to a range of water-related hazards and disruptions. Here are some of the key consequences of a cloud burst:
- Flash Floods: One of the most immediate and dangerous consequences of a cloud burst is the occurrence of flash floods. The intense and concentrated rainfall from the cloud burst can overwhelm drainage systems, rivers, and streams, leading to rapid and widespread flooding. Flash floods can occur within minutes of the onset of heavy rainfall and pose a serious threat to lives, property, and infrastructure.
- Landslides and Mudslides: In hilly or mountainous regions, a cloud burst can saturate the soil, making it more susceptible to landslides and mudslides. The additional water weight, coupled with the steep terrain, can trigger the sudden movement of soil and rock, leading to dangerous landslides that can bury homes, roads, and communities.
- Property Damage: The rapid and intense nature of a cloud burst's rainfall can result in significant damage to homes, buildings, and infrastructure. Floodwaters can enter structures, causing structural damage, waterlogging, and destruction of personal belongings. Infrastructure such as roads, bridges, and utility systems can also be severely affected.
- Disruption of Services: Cloud bursts can disrupt essential services, including transportation, communication, and utilities. Flooded roads and bridges can make travel difficult or impossible, hampering emergency response and evacuation efforts. Power outages can occur if the electrical infrastructure is damaged by flooding or landslides.
- Health and Safety Risks: The flooding and contamination of water sources during a cloud burst can pose health risks to the affected population. Contaminated water can lead to the spread of waterborne diseases, and individuals may be at risk of injuries, drowning, or exposure to hazardous materials in floodwaters.
6. Mitigating Measures for Cloud Bursts
Mitigating the impacts of cloud bursts requires a combination of proactive planning, infrastructure improvements, and community preparedness. Here are some key measures that can be taken to mitigate the effects of cloud bursts:
- Early Warning Systems: Implement effective early warning systems that can provide timely alerts about impending cloud bursts and heavy rainfall. These systems should be capable of reaching a wide audience through various communication channels, including mobile phones, sirens, and local media.
- Floodplain Zoning and Land Use Planning: Designate floodplain areas where development is restricted or regulated. Proper land use planning can help prevent construction in high-risk flood areas, reducing potential damage to property and infrastructure.
- Improved Drainage Infrastructure: Enhance drainage systems in urban and rural areas to handle sudden and intense rainfall. Well-designed drainage systems can help prevent water accumulation on roads and prevent flash floods.
- Erosion Control Measures: Implement erosion control measures, such as building retaining walls, stabilizing slopes, and using vegetation to prevent soil erosion in hilly and mountainous regions.
- Reservoirs and Dams: Construct reservoirs and dams to store excess water during heavy rainfall and release it gradually to prevent downstream flooding. Proper maintenance of these structures is essential to ensure their effectiveness.
- Green Infrastructure: Incorporate green infrastructure solutions such as permeable pavements, rain gardens, and rooftop gardens in urban planning. These measures can help absorb and manage excess rainwater, reducing the risk of flooding.
7. Conclusion
A cloudburst is a result of the complex interplay between atmospheric conditions, convective processes, and the physical properties of water droplets and ice crystals within a cloud. These intense weather events can have significant impacts on the affected areas and highlight the importance of preparedness, early warning systems, and proper urban planning to mitigate their effects.
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For Prelims: Cloudbursts, flash floods, landslides, Cumulonimbus Clouds, Water Vapour, Floodplain Zoning, Green Infrastructure.
For Mains: 1. What is a cloudburst, and how does it differ from regular rainfall? Explain the causes and meteorological factors that contribute to the occurrence of a cloudburst.
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Previous year Questions1. Which of the following statements with regard to Cloudburst is/are correct? (UPSC CDS 2017)
1. It is defined as sudden localized very heavy downpour with cloud thunder and lightning.
2. It mostly occurs in the hilly areas.
3. It results in a very high intensity of rainfall, i.e., 250 mm-300 mm in a couple of hours.
4. It occurs only during the daytime.
Select the correct answer using the code given below.
A. 1, 2 and 3
B. 1, 3 and 4
C. 2 and 3 only
D. 2 only
Answer: A
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Source: The Indian Express
