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Pouches in the sky: Mammatus clouds spark global interest

Explainer on clouds, with recent relevance due to Mammatus clouds spotted over Russia

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In news: Mammatus clouds over Russia

Unusual Mammatus clouds — pouch-like bulges hanging underneath the base of clouds — were seen over Russia, catching global attention. Typically associated with severe thunderstorms, these clouds form on the underside of cumulonimbus clouds and are indicative of strong atmospheric turbulence, making them a useful visual cue for aviation and meteorology.
What are clouds?
Clouds are suspended masses of minute water droplets or ice crystals in the atmosphere, formed when air becomes saturated and water vapour condenses around aerosols.
How are clouds formed?
Clouds form through the following steps:
  1. Uplift of air (due to heating, mountains, fronts or convergence)
  2. Adiabatic cooling (temperature drops as air rises and pressure decreases)
  3. Condensation when the air reaches the dew point (requires condensation nuclei)
  4. Aggregation of condensed water droplets to form visible cloud masses
Factors that define the shape of clouds
Several physical factors govern cloud shapes:
Factor
Influence
Altitude
High clouds are thin; low clouds are denser and layered
Temperature
Affects ice or water droplet formation
Humidity
Determines size and density of the cloud
Wind patterns
Horizontal vs vertical growth
Atmospheric Stability
Unstable air leads to vertical (cumulus) clouds; stable air leads to horizontal (stratus) clouds
Topography
Mountains can induce specific types like lenticular clouds
Rain-bearing vs non-rain-bearing clouds
Type
Description
Examples
Rain-bearing clouds
Dense, thick clouds capable of precipitation
Nimbostratus, Cumulonimbus
Non-rain-bearing clouds
Thin, wispy or layered clouds with minimal water content
Cirrus, Altostratus, Stratocumulus
Classification of clouds
Based on altitude
Level
Cloud types
High (Above 6,000 m)
Cirrus (Ci), Cirrostratus (Cs), Cirrocumulus (Cc)
Middle (2,000-6,000 m)
Altostratus (As), Altocumulus (Ac)
Low (Surface to 2,000 m)
Stratus (St), Stratocumulus (Sc), Nimbostratus (Ns)
Vertical Development
Cumulus (Cu), Cumulonimbus (Cb)
Based on shape
Shape
Cloud type
Layered
Stratus-type (flat, sheet-like)
Heap/Convectional
Cumulus-type (puffy, rising)
Wispy
Cirrus-type (feathery, high-altitude ice clouds)
Towering
Cumulonimbus (storm clouds, vertical extent)
Summary of key cloud types
Cloud
Appearance
Altitude
Precipitation
Note
Cirrus
Wispy, thin
High
No
Made of ice crystals
Cumulus
Puffy, cotton-like
Low to mid
No/light rain
Fair-weather cloud
Stratus
Flat, uniform layer
Low
Light drizzle
Fog-like when near surface
Nimbostratus
Thick, dark
Low to mid
Continuous rain
Covers large area
Cumulonimbus
Towering, anvil-top
Vertical
Heavy rain, thunder
Severe weather cloud
Mammatus
Pouch-like bulges under base
Below thunderclouds
No direct rain
Associated with turbulence

UPSC mains relevance – GS Paper I & III
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(geography, disaster management)

Sample UPSC questions
Short questions (prelims & basics)
  1. Which type of cloud is associated with thunderstorms and severe weather?
  2. Name any two high-level clouds.
  3. Define “Mammatus clouds”.
Long questions (mains)
  1. Explain the mechanism of cloud formation and the role of condensation nuclei.
  2. Differentiate between rain-bearing and non-rain-bearing clouds with examples.
  3. Discuss how different factors influence the shape and type of clouds in various atmospheric layers.
Analytical questions
  1. “Clouds are indicators of climate and weather conditions.” Explain with reference to classification based on height and shape.
  2. How can observation of specific cloud types (like cumulonimbus or mammatus) help in disaster forecasting?
  3. With recent examples, analyse how cloud types are linked with extreme weather events globally.
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