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.Pressure, Winds, Storms,
and Cyclones
8th class science curiosity
Explore the fascinating world of atmospheric forces that shape our weather patterns.
From the basic principles of pressure to the formation of devastating cyclones, this
presentation examines how pressure differences in air and liquids create the natural
phenomena we experience every day.
By : K Sandeep Swamy(M.Sc,B.Ed)
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Key Questions We'll Answer
Why are winds stronger on some days than on
others?
Understanding the relationship between pressure differences and
wind strength
Why are water tanks usually placed at a height?
Exploring how liquid pressure depends on height
Can air pressure really crush us?
Discovering the surprising power of atmospheric pressure
What causes storms and cyclones?
Examining the formation of powerful weather systems
Understanding Pressure
What is Pressure?
Pressure is defined as force per unit area.
Pressure =
Area
Force
The SI unit of pressure is newton/meter² (N/m²), also called a pascal
(Pa).
When the same force acts on a smaller area, it creates higher pressure.
Megha's bag with broad straps distributes weight over a larger area,
creating less pressure on her shoulders compared to Pawan's narrow
straps.
Pressure in Daily Life
Broad straps distribute weight over a larger
area, reducing pressure on shoulders.
Broad handles make it easier to carry water-
filled buckets by reducing pressure on hands.
Knives and nails concentrate force on a small
area, creating high pressure that makes cutting
or penetration easier.
Pressure in Liquids
Key Properties
Liquids exert pressure in all directions - at the bottom and on the
sides of a container
Pressure increases with the height of the liquid column
Pressure depends on the height of the liquid column, not the shape
or width of the container
This is why water tanks are placed at a height - to increase water
pressure in taps below.
Equal heights of water columns produce the same bulge in balloons,
regardless of the pipe diameter.
Liquid Pressure Experiment
Demonstrating Liquid Pressure
Take two transparent pipes of different diameters
1.
Attach balloons to the bottom of each pipe
2.
Fill both pipes with water to the same height
3.
Observe that both balloons bulge equally
4.
This shows that liquid pressure depends on height, not volume or
container shape.
Higher water columns create more pressure, causing larger bulges.
Liquid Pressure on Container Walls
Demonstrating Side Pressure
Take a plastic bottle and make holes at the same height around the
sides
1.
Seal the holes with tape and fill with water
2.
Remove the tape from all holes simultaneously
3.
Observe water flowing out through all side holes
4.
This demonstrates that liquids exert pressure in all directions, not just
downward. Water flowing out from side holes shows that liquids exert pressure on
the walls of containers.
This principle explains why dam bases are broader than their tops - to
withstand the increasing horizontal water pressure near the bottom.
Atmospheric Pressure
The Weight of Air
The envelope of air surrounding Earth (atmosphere) exerts pressure on
everything.
Atmospheric pressure is the force exerted by air per unit area.
At sea level, atmospheric pressure is approximately 101,325 Pa (or
1013.25 hPa).
The force on a 15cm × 15cm area is nearly equal to 2250 N
(equivalent to 225 kg)
We aren't crushed because pressure inside our bodies balances
external pressure
Air exerts pressure in all directions, similar to how water pressure works
in a container.
Demonstrating Atmospheric Pressure
Paper Plate Experiment
Cover an inverted paper plate with unfolded
chart paper and try to lift it. The atmospheric
pressure on the large surface area makes it
difficult to lift.
Rubber Sucker
When pressed against a smooth surface, a
rubber sucker sticks firmly because the air
inside is pushed out, creating lower pressure
inside than outside.
Balloon Inflation
When you blow into a balloon, the air inside
exerts pressure on the walls, causing it to
expand in all directions.
Formation of Wind
Wind Basics
Wind is simply air in motion, caused by differences in air pressure.
Air always moves from high-pressure areas to low-pressure areas
The greater the pressure difference, the faster the air moves
This movement of air is what we experience as wind
Wind strength varies based on the magnitude of pressure differences
between regions.
In this experiment, air moves from the inflated balloon (high pressure) to
the uninflated balloon (low pressure) until pressures equalize.
Land and Sea Breezes
Day: Sea Breeze
Land heats faster than water during the day
Warm air over land rises, creating low pressure
Cool air from sea (high pressure) flows toward land
Night: Land Breeze
Land cools faster than water at night
Warm air over sea rises, creating low pressure
Cool air from land (high pressure) flows toward sea
High-Speed Winds and Pressure
Bernoulli's Principle
High-speed winds create areas of low pressure.
When air moves faster, its pressure decreases - this is known as
Bernoulli's principle.
This explains why:
Roofs can be blown off during storms
Airplane wings generate lift
Two hanging balloons move toward each other when air is blown
between them
When you blow between two hanging balloons, the fast-moving air
creates a low-pressure area, causing the balloons to move toward each
other.
Why Roofs Blow Off During Storms
The Pressure Difference
During storms with high-speed winds:
Fast-moving air above the roof creates low pressure
Higher pressure inside the house pushes upward
This pressure difference can lift and blow away weak roofs
Safety Tip: Keep doors and windows open during storms to equalize
pressure and reduce the risk of roof damage.
Keeping doors and windows open allows air to flow through the house,
reducing the pressure difference between inside and outside.
Thunderstorm Formation
Heating and Rising Air
Land heats up, causing warm and moist air to rise, creating a low-
pressure area.
ículas aquáticas e nuvens
Cloud Formation
As rising air expands and cools, moisture condenses to form water
droplets and clouds.
Precipitation
Water droplets merge to form heavier drops, which fall as rain, hail, or
snow.
Strong Winds
Strong winds blowing upwards and downwards create the conditions
for a storm.
Lightning Formation
The Electrification Process
Strong winds cause water droplets and ice particles to rub against
each other
1.
This friction creates static electric charges within clouds
2.
Lighter, positively charged ice particles rise to the upper part of
clouds
3.
Heavier, negatively charged water droplets sink to the lower part
4.
The ground below becomes positively charged
5.
When charge buildup becomes too large, electricity flows as
lightning
6.
Lightning can occur within a cloud, between clouds, or between a cloud
and the ground.
Thunder is the sound produced when lightning rapidly heats the air,
causing it to expand.
Lightning Safety
Stay Away from Tall Objects
Avoid trees, poles, and other tall structures that might attract
lightning.
Find Low Ground
Seek a low-lying open area and crouch down with minimal ground
contact. Do not lie flat.
Avoid Metal Objects
Stay away from metal objects, including umbrellas with metal rods.
Get Out of Water
Water conducts electricity, so exit swimming pools, lakes, or other
bodies of water immediately.
Lightning Protection
Lightning Conductors
A lightning conductor is a metallic rod installed on buildings to protect
them from lightning strikes.
The pointed end extends above the highest point of the building
The other end is buried deep in the ground
It provides an easy path for electric charges to flow safely into the
ground
This prevents damage to the building and its occupants Lightning conductors protect buildings by providing a safe path for
lightning to travel to the ground.
Cyclone Formation
This self-reinforcing cycle creates the massive storm systems we know as cyclones, hurricanes, or typhoons.
Warm Ocean Waters
Cyclones form over warm ocean waters
(above 27°C)
Rising Warm Air
Warm, moist air rises, creating a low-
pressure area
Condensation
Water vapor condenses, releasing heat that
further warms the air
Spinning Motion
Earth's rotation causes the moving air to spin
Intensification
The cycle repeats, creating a powerful
spinning storm system
Anatomy of a Cyclone
Structure of a Cyclone
Eye: The calm center with the lowest pressure
Eyewall: Ring of intense thunderstorms with strongest winds
Rain bands: Spiral bands of clouds and precipitation
Outflow: High-level clouds moving away from the center
Wind speeds in severe cyclones can exceed 250 km/h, as in the 2020
Amphan cyclone which reached 270 km/h.
The eye of a cyclone is surprisingly calm, while the surrounding eyewall
contains the most violent winds and heaviest rainfall.
Cyclone Impacts
Storm Surge
Walls of water 3-12 meters high pushed inland, causing severe flooding
Heavy Rainfall
Causes river flooding and landslides, even far inland from the coast
Destructive Winds
Damage buildings, uproot trees, and create dangerous flying debris
Saltwater Intrusion
Contaminates drinking water and damages farmland, reducing soil fertility
Cyclone Preparedness
Stay Informed
Monitor weather reports and alerts from the India Meteorological
Department (IMD)
Prepare Emergency Kit
Include water, non-perishable food, medications, flashlight,
batteries, and important documents
Know Evacuation Routes
Identify nearby cyclone shelters and plan how to reach them
quickly
Secure Property
Reinforce doors and windows, trim trees, and secure loose objects
that could become projectiles
Modern weather monitoring satellites help track cyclones and predict their paths, significantly reducing their impact on life and property.
Local Thunderstorms in India
Regional Thunderstorms
Kalboishakhi: Pre-monsoon thunderstorms in West Bengal, Bihar,
and Jharkhand
Bordoisila: Spring thunderstorms in Assam
Mango Showers: Pre-monsoon thunderstorms in Kerala, Karnataka,
and Tamil Nadu that help ripen mangoes
Coffee Blossoms: Thunderstorms in Karnataka that support coffee
plant growth
These local thunderstorms often occur before the arrival of monsoons
and play an important role in agricultural cycles.
Practical Applications
Water Tanks at Height
Placed high to increase water pressure in taps
below, using the principle that liquid pressure
increases with height.
Dam Design
Dams have broader bases than tops to
withstand the increasing horizontal water
pressure near the bottom.
Holes in Banners
Banners and hoardings have holes to allow
wind to pass through, reducing pressure that
could tear them down.
Key Concepts Review
Pressure
Force per unit area (P = F/A)
SI unit: pascal (Pa) or N/m²
Liquid Pressure
Depends on height of liquid column
Acts in all directions
Atmospheric Pressure
Pressure exerted by air
Approximately 101,325 Pa at sea level
Wind Formation
Air flows from high to low pressure
Greater pressure difference = stronger winds
Storms & Cyclones
Form due to pressure differences, moisture, and Earth's rotation
Monitored by meteorological departments
Explore Further
Activities to Try
Hold a paper strip between your fingers and blow over it. Observe
how it rises due to the pressure difference created by fast-moving
air.
1.
Research major cyclones that have affected India in the last 20
years and the measures taken to reduce their impact.
2.
Collect data on thunderstorm strength across different regions of
India to identify patterns and vulnerable areas.
3.
Questions to Ponder
If the Earth stopped rotating, would cyclones still form? How would
their patterns change?
Why do some regions experience more frequent and severe storms
than others?
How might climate change affect the frequency and intensity of
cyclones in the future?