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www.pmfias.com https://www.youtube.com/c/PoorMansFriend www.pmfias.com WWW.PMFIAS.COM Thunderstorms Thunderstorms and tornadoes are severe local storms. They are of short duration, occurring over a small area but are violent. Thunderstorm is a storm with thunder and lightning and typically also heavy rain or hail. Thunderstorms mostly occur on ground where the temperature is high. Thunderstorms are less frequent on water bodies due to low temperature. How does a thunderstorm form? Cumulus stage Intense convection of moist hot air building up a cumulonimbus cloud. Mature stage Characterised by intense updraft of rising warm air, which causes the clouds to grow bigger and rise to greater height. Later, downdraft brings down to earth the cool air and the rain.

Climatology.12.Thunderstorms

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Thunderstorms

Thunderstorms and tornadoes are severe local storms. They are of short duration,

occurring over a small area but are violent.

Thunderstorm is a storm with thunder and lightning and typically also heavy rain or

hail.

Thunderstorms mostly occur on ground where the temperature is high. Thunderstorms

are less frequent on water bodies due to low temperature.

How does a thunderstorm form?

Cumulus stage

Intense convection of moist hot air building up a cumulonimbus cloud.

Mature stage

Characterised by intense updraft of rising warm air, which causes the clouds to grow

bigger and rise to greater height. Later, downdraft brings down to earth the cool air and

the rain.

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Dissipating stage

When the clouds extend to heights where sub-zero temperature prevails, hails are

formed and they come down as hailstorm. Intense precipitation occurs.

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Motion of a thunderstorm

Path of a thunderstorm is irratic. Motion is primarily due to interactions of its updrafts

and downdrafts.

The speed of isolated storms is typically about 20 km (12 miles) per hour, but some

storms move much faster.

In extreme circumstances, a supercell storm may move 65 to 80 km (about 40 to 50

miles) per hour.

Types of Thunderstorms

Convectional, Frontal, Orographic Thunderstorms.

Isolated Thunderstorms, Multiple-Cell Thunderstorms, Supercell thunderstorms.

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Downbursts

Downdrafts are referred to as macrobursts or microbursts.

Macroburst is more than 4 km in diameter and can produce winds as high as 60 metres

per second, or 215 km per hour.

A microburst is smaller in dimension but produces winds as high as 75 metres per

second, or 270 km per hour

They are seriously hazardous to aircrafts, especially during takeoffs and landings.

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Lightning and thunder

Thunder clouds in different geographic locations tend to produce an excess negative

charge [−5 and −15 °C].

Positive charge accumulates at both higher and lower altitudes.

Larger and heavier cloud particles charge with a negative polarity.

Smaller and lighter particles acquire a positive polarity.

This creates a high electric field.

Lightning discharges take place between opposite charge regions, between charged

regions and the ground.

Roughly two-thirds of all discharges occur within the cloud; The rest are between the

cloud and ground.

Lightning can be triggered by a mountain or a tall structure.

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Thunder

Lightning creates plasma [30,000 °C].

The channel pressure greatly exceeds the ambient (surrounding) pressure, and the

channel expands at a supersonic rate (speed of sound).

The resultant shock wave decays rapidly with distance and is eventually heard as

thunder once it slows to the speed of sound.

How many thunderstorms occur?

Worldwide, there are an estimated 16 million thunderstorms each year, and at any

given moment, there are roughly 2,000 thunderstorms in progress.

What kinds of damage can thunderstorms cause?

Many hazardous weather events are associated with thunderstorms.

Under the right conditions, rainfall from thunderstorms causes flash flooding, killing

more people each year than hurricanes, tornadoes or lightning.

Lightning is responsible for many fires around the world each year, and causes

fatalities.

Hail up to the size of softballs damages cars and windows, and kills livestock caught

out in the open.

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Strong (up to more than 120 mph) straight-line winds associated with thunderstorms

knock down trees, power lines and mobile homes.

Tornadoes (with winds up to about 300 mph) can destroy all but the best-built man-

made structures.

Thunderstorm Types

Thermal storm

• Caused due to intense heating of ground during summer.

Orographic storm

Forceful upliftment of warm moist air parcel when it passes over a mountain barrier

creates cumulonimbus cloud causing heavy precipitation on the windward side.

Orographic ‘Cloud bursts’ are common in Jammu and Kashmir, Cherrapunji and

Mawsynram.

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Frontal strom

Thunderstroms occurring along fronts.

Single-cell strom

Single-cell thunderstorms are small, brief, weak storms that grow and die within an

hour or so. They are typically driven by heating on a summer afternoon. Single-cell

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storms may produce brief heavy rain and lightning (Very common in India during

summers, mostly April, May. In Kerala they are called ‘Mango Showers’ and in

Karnataka ‘Blossom showers’).

A multi-cell storm

A multi-cell storm is a thunderstorm in which new updrafts form along the leading edge

of rain-cooled air (the gust front).

Individual cells usually last 30 to 60 minutes, while the system as a whole may last for

many hours.

Multicell storms may produce hail, strong winds, brief tornadoes, and/or flooding.

A supercell storm

A supercell is a long-lived (greater than 1 hour) and highly organized storm feeding off

an updraft (a rising current of air) that is tilted and rotating.

Most large and violent tornadoes come from supercells.

Tornado

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From severe thunderstorms sometimes spiralling wind descends like a trunk of an

elephant with great force, with very low pressure at the centre, causing massive

destruction on its way. Such a phenomenon is called a tornado.

Tornadoes generally occur in middle latitudes. The tornado over the sea is called water

sprouts.

These violent storms are the manifestation of the atmosphere’s adjustments to varying

energy distribution. The potential and heat energies are converted into kinetic energy

in these storms and the restless atmosphere again returns to its stable state.

small-diameter column of violently rotating air developed within a convective

cloud and in contact with the ground

occur most often in association with thunderstorms during the spring and

summer in the mid-latitudes of both the Northern and Southern Hemispheres.

These whirling atmospheric vortices can generate the strongest winds known on

Earth: wind speeds in the range of 500 km (300 miles) per hour

often referred to as twisters or cyclones

Distribution

rare in polar regions and infrequent at latitudes higher than 50° N and 50° S.

The temperate and tropical regions are the most prone to thunderstorms.

Tornadoes have been reported on all continents except Antarctica

United States has the most violent tornadoes

Canada reports the second largest number of tornadoes

at any moment there are approximately 1,800 thunderstorms in progress

throughout the world.

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Waterspout

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waterspout is an intense columnar vortex (usually appearing as a funnel-shaped

cloud) that occurs over a body of water

They are connected to a towering cumuliform cloud or a cumulonimbus cloud

weaker than most of its land counterparts

Most waterspouts do not suck up water; they are small and weak rotating columns

of air over water

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tornadoes in connection with severe thunderstorms, but simply occurring over

water.

identical to traditional land-based tornadoes in connection with severe

thunderstorms, but simply occurring over water.

Multiple choise questions

Multiple choice questions. (i) If the surface air pressure is 1,000 mb, the air pressure

at 1 km above the surface will be: (a) 700 mb (c) 900 mb (b) 1,100 mb (d) 1,300 mb

The Inter Tropical Convergence Zone normally occurs: (a) near the Equator (b) near the

Tropic of Cancer (c) near the Tropic of Capricorn (d) near the Arctic Circle

The direction of wind around a low pressure in northern hemisphere is: (a) clockwise

(c) anti-clock wise (b) perpendicular to isobars (d) parallel to isobars

Which one of the following is the source region for the formation of air masses? (a) the

Equatorial forest (c) the Siberian Plain (b) the Himalayas (d) the Deccan Plateau

30 words

While the pressure gradient force is from north to south, i.e. from the subtropical high

pressure to the equator in the northern hemisphere, why are the winds north easterlies

in the tropics.

What are the geotrophic winds?

Explain the land and sea breezes.

150 words

Discuss the factors affecting the speed and direction of wind.

Draw a simplified diagram to show the general circulation of the atmosphere over the

globe. What are the possible reasons for the formation of subtropical high pressure over

30° N and S latitudes?

Why does tropical cyclone originate over the seas? In which part of the tropical cyclone

do torrential rains and high velocity winds blow and why?

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