Choose the correct option
Question 1
The weight of air on a unit area of the earth:
- weight pressure
- air pressure
- unit pressure
- area pressure
Answer
air pressure
Question 2
Horizontal movement : ............... :: Vertical movement: air current
- conduction
- convection
- winds
- coriolis
Answer
winds
Question 3
The force per unit area exerted against a surface by the weight of the air above that surface:
- Force Pressure
- Area Pressure
- Air Pressure
- Atmospheric Pressure
Answer
Atmospheric Pressure
Question 4
Tha average atmospheric pressure at sea level:
- 1014.5 mb
- 1015.2 mb
- 1013.25 mb
- 1017.75 mb
Answer
1013.25 mb
Question 5
The decrease in the pressure per unit distance in the direction in which the pressure decreases most rapidly.
- Pressure Gradient
- Distance Pressure
- Decreased Pressure
- Unit/Distance Gradient
Answer
Pressure Gradient
Question 6
What are also called the Horse Latitude?
- Equatorial Low Pressure Belts
- Sub-Tropical High Pressure Belts
- Circum-polar Low Pressure Belts
- Polar High Pressure Areas
Answer
Sub-Tropical High Pressure Belts
Question 7
Which pressure belt is also called as Doldrums?
- Equatorial Low Pressure Belts
- Sub-Tropical High Pressure Belts
- Circum-polar Low Pressure Belts
- Polar High Pressure Areas
Answer
Equatorial Low Pressure Belts
Question 8
Horizontal movement of air in the atmosphere.
- Winds
- Currents
- Pressure
- None of the above.
Answer
Winds
Question 9
The steady winds blowing from the Sub-Tropical High Pressure towards the Equatorial Low Pressure:
- High Pressure Winds
- Low Pressure Winds
- Trade Winds
- Steady Winds
Answer
Trade Winds
Question 10
Which amongst the following is NOT a characteristic of Trade Winds?
- They have varying velocity and are irregular
- They are permanent or prevailing winds
- They are called North-East Trades in Northern Hemisphere
- They have fixed velocity and are regular
Answer
They have varying velocity and are irregular
Question 11
Alps : ............... :: Rockies : ...............
- Chinook, Mistral
- Polar Easterlies, Foehn
- Foehn, Mistral
- Chinook, Foehn
Answer
Alps : Foehn :: Rockies : Chinook
Question 12
What is the tropical cyclone over land called?
- Tropical Cyclone
- Temperate Cyclone
- Tornado
- Mistral
Answer
Tornado
Question 13
The concentrated bands of rapid air movement at the tropopause:
- Jet Streams
- Tornado
- Mistral
- Wave Cyclones
Answer
Jet Streams
Question 14
Which of the following is true about Jet streams?
- Forecast weather
- Reduce flight time
- Increase precipitation
- All of the above.
Answer
All of the above
Question 15
Calm region in the centre of the cyclone:
- focus
- eye
- core
- All of the above.
Answer
eye
Question 16
Which of the following is NOT a tropical cyclone?
- hurricane
- typhoons
- mistral
- willy-willies
Answer
mistral
Short Answer Questions
Question 1
Name the four main pressure belts of the earth.
Answer
The four main pressure belts of the earth are-
- Equatorial Low Pressure Belts
- Sub-tropical High Pressure Belts
- Circum-polar Low Pressure Belts
- Polar High Pressure Areas
Question 2
What is the Circum-polar Low Pressure Belt?
Answer
These belts are located between 60° and 70° in each hemisphere. Due to the earth's rotation, the wind surrounding the Polar region blow towards the equator. Centrifugal forces operating in this region create the low pressure belt appropriately called Circum-polar Low Pressure Belt.
Question 3
How does the Coriolis Force vary latitudinally?
Answer
Due to the rotation of the earth on its tilted axis, the wind starts deflecting to its right in the Northern Hemisphere. In the Southern Hemisphere, it starts deflecting to its left from its original path.
Thus, a wind blowing from the north becomes north-easterly in the northern hemisphere and the wind blowing from south becomes south-easterly in the southern hemisphere.
The Coriolis effects is greatest near the poles and zero at the equator because of the earths spherical shape. It is proportional to the angle of the latitude.
Question 4
Name the three chief types of wind.
Answer
The three chief types of wind are-
- Permanent or Planetary winds
- Periodic winds
- Local winds
Question 5
What are periodic winds?
Answer
Certain winds reverse their direction periodically with season and are called periodic winds. These winds blow at regular intervals or in regular cycles. They are winds that result from localised differences in pressure and temperature.
Question 6
What are local winds? Name any two local winds.
Answer
There are certain winds in different parts of the world which flow in comparatively small area and have special characteristics. These are called local winds.
Two local winds are Loo and Mistral.
Question 7
Name two types of variable winds. Why are they so called?
Answer
Two types of variable winds are-
- Cyclones
- Anticyclones
They are called variable winds because they do not blow in any definite direction and their direction varies with the movement of the pressure system. Their speed also depends on the intensity of the depression.
Question 8
Why are cyclones frequent in summer in the tropical region?
Answer
Cyclones require a sea surface temperature of about 26°C to develop and maintain their strength. They also need a high relative humidity. These conditions are only found in the tropical oceans during summer. Therefore, cyclones are frequent in summer in the tropical regions.
Question 9
Mention any two differences between Tropical Cyclones and Temperate Cyclones.
Answer
Tropical Cyclones | Temperate Cyclones |
---|---|
These cyclones generally originate in the tropical region between 8° and 20° N and S. | These cyclones are active over mid-latitudinal region between 35° and 65° N and S. |
Tropical cyclones usually travel from east to west. | Temperate cyclones usually travel from west to east. |
Question 10
How are cyclones named differently in different parts of the world?
Answer
Cyclones are called tornadoes in North America, hurricanes in south-east Caribbean region, typhoons in eastern China, Japan and Philippines islands and cyclones in the Bay of Bengal and Arabian sea.
Question 11
What are two chief characteristics of anticyclones?
Answer
Two chief characteristics of anticyclones are-
- There is high pressure in the core and low pressure around it. Winds blow gently outwards.
- These winds are clockwise in northern hemisphere and anticlockwise in the southern hemisphere.
Define the following terms
Question 1
Pressure Gradient
Answer
Pressure gradient is defined as the decrease in pressure per unit distance in the direction in which the pressure decreases most rapidly.
Question 2
Winds
Answer
Contrasts in temperature cause changes in air density, which are responsible for variations in pressure. These variations cause horizontal movements of air called winds.
Question 3
Coriolis force
Answer
Coriolis force is the force generated due to rotation of the Earth on its inclined axis. Due to Coriolis force, moving objects (winds and water currents) tend to deflect to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. The deflection is least at the Equator and greatest at the poles.
Question 4
Altitude
Answer
Altitude refers to the height of a place in relation to sea level or ground level.
Question 5
Monsoons
Answer
Monsoons are periodic seasonal winds blowing in the regions of South East Asia and Northern Australia. They develop because of differences in heating conditions of the continent and the oceans.
Distinguish between the following
Question 1
Cyclones and Anticyclones
Answer
Cyclones | Anticyclones |
---|---|
There is low pressure in the centre and high pressure around it. | There is high pressure at the core and low pressure around it. |
Winds blow inwards. | Winds blow gently outwards. |
These winds are anti-clockwise in northern hemisphere and clockwise in the southern hemisphere. | These winds are clockwise in northern hemisphere and anticlockwise in the southern hemisphere. |
Question 2
Permanent and Periodic Winds
Answer
Permanent Winds | Periodic Winds |
---|---|
Permanent winds blow throughout the year from one latitude to the other in response to the latitudinal differences in the air pressure. | Certain winds reverse their direction periodically with season and are called periodic winds. They blow at regular intervals or in regular cycles. |
For example- trade winds, the Westerlies, the Polar Easterlies. | For example- land and sea breezes and the seasonal winds. |
Question 3
Summer and Winter Monsoons
Answer
Summer Monsoons | Winter Monsoons |
---|---|
Summer monsoon usually begins in April and lasts till the month of September. | The monsoon usually begins in October and lasts till March. |
These are brought by cooler, denser and high-pressure winds over the Indian Ocean, to the low-pressure area over the landmass. | These winds blows from the high pressure over the land mass to the oceans which have lower pressure developed over them. |
The rainfall can be very intense as these winds travel from water bodies to land and thus, carry a lot of moisture. | Winter monsoons are mostly less powerful and less destructive than summer monsoons as they are dry winds and do not contain enough moisture to cause heavy rains. |
They are also called South-west monsoon. | They are also called receding monsoon. |
Structured Questions
Question 1(a)
What is meant by the term 'Atmospheric Pressure'?
Answer
Atmospheric pressure refers to the force per unit area exerted against a surface by the weight of the air above that surface.
Question 1(b)
Explain briefly the factors that affect Atmospheric Pressure.
Answer
The factors that affect Atmospheric Pressure are:
- Altitude — Atmospheric Pressure decreases with increase in altitude at rate of 1 cm of mercury for every 110 m of ascent. Atmospheric Pressure is highest at sea level.
- Temperature — Atmospheric Pressure decreases with increase in temperature.
- Water Vapour — Water Vapour concentration affects atmospheric pressure because molecular weight of water (18 g/mol) is less than the average molecular weight of air (about 29 g/mol). Therefore, humid air is less dense and exerts less pressure than dry air.
- Rotation of the Earth — Due to rotation of earth, bulk of the air at the poles is thrown away towards the Equator. This creates low pressure in Equatorial regions as they are hot whereas at the poles, the cold heavy air sinks down and creates high pressure. In fact, temperature and rotation of the earth together contribute to the formation of world pressure belts.
Question 1(c)
Give a geographical reason for each of the following:
(i) The Westerlies in the Southern Hemisphere blow with greater force than those in the Northern Hemisphere.
(ii) There is a seasonal shifting in pressure belts.
(iii) As we go higher, the atmospheric pressure decreases.
Answer
(i) The Westerlies in the Southern Hemisphere blow with greater force than those in the Northern Hemisphere because there is absence of landmass in the southern hemisphere.
(ii) The causes of shifting of pressure belts are inclination of Earth's axis and change in relative position of Earth with respect to the Sun -
- At the time of Summer solstice the Sun is vertical over the Tropic of Cancer and therefore, all the pressure belts except the northern polar high pressure belt shift northward.
- After Autumn Equinox, there is southward migration of the Sun which becomes vertically over the Tropic of Capricorn at the time of Winter Solstice and therefore the pressure belt shifts southward except in the southern polar high pressure belt.
- The Sun is overhead over the Equator at the time of Spring Equinox and Autumn Equinox and hence all the pressure belts occupy their normal positions.
(iii) As we go higher upwards, the atmospheric pressure decreases at an average rate of 34 millibars per 300 metres of latitude. It is because the air in the lower layer of the atmosphere is denser than at higher level. The air is denser in lower layer because of gravitational pull of earth and also because the lower layers are compressed under upper layers of atmosphere.
Question 1(d)
Draw a well labelled diagram showing the pressure and wind belts of the earth.
Answer
Below labelled diagram shows the pressure and wind belts of the earth:
Question 2(a)
Briefly explain the three chief types of winds.
Answer
The three chief types of winds are-
Permanent / Prevailing / Planetary Winds — Permanent winds blow throughout the year from one latitude to the other in response to the latitudinal differences in the air pressure. For example, Trade winds, the Westerlies and the Polar Easterlies.
Periodic Winds — Certain winds reverse their direction periodically with season and are called periodic winds. For example, Land breeze and sea breeze, summer monsoon and winter monsoon.
Local winds — There are certain winds in different parts of the world which flow in comparatively small area and have special characteristics. These winds are called local winds. For example, loo, foehn and chinook and mistral.
Question 2(b)
Describe some of the important types of local winds.
Answer
Some of the important types of local winds are-
Loo — In the northern plains of India and Pakistan, a very hot and dry wind blows from the west in summer in the afternoons, known as loo. Its temperature invariably ranges between 45°C and 50°C. It may cause sunstroke to people.
Foehn and Chinook — Foehn is a dry, hot wind which blows in the valley on the northern slopes of Alps. The temperature of the wind is from 15°C to 20°C. The wind is of use for melting snow and it hastens the ripening of grapes.
Similar kind of wind in the USA and Canada move down the west slopes of the Rockies and are known as Chinook.
- Mistral — Mistral is a local cold wind that blows from the Alps over France towards the Mediterranean Sea. Mistral brings down the temperature below freezing point.
Question 2(c)
Give a geographical reason for each of the following:
(i) The winds are directed to the right of their flow in the Northern Hemisphere.
(ii) Temperature and pressure are inversely related to one another.
(iii) Humid air is lighter than dry air.
Answer
(i) The rotation of the earth produces another force other than the pressure force which is called the Coriolis force. It causes deflection of winds. Thus, the winds are directed to the right of their flow in the Northern Hemisphere due to Coriolis effect.
(ii) Temperature and pressure are inversely related to one another as atmospheric pressure decreases with increase in temperature. This is because when the temperature rises, air expands. The molecules of air move far apart and hence exert less pressure. On the contrary, with decrease in temperature, the air gets compressed and the space between molecules decreases and exerts more pressure on the region.
(iii) Humid air is lighter than dry air because the molecular weight of water is less than the average molecular weight of air. When water evaporates and enters the atmosphere as a gas, the water vapour molecules take the place of other gas molecules in the air. So, the volume of wet air weighs less than an equal volume of dry air.
Question 2(d)
What is Coriollis Effect? How does it affect the planetary winds?
Answer
Coriolis effect or Coriolis force is the force generated due to rotation of the Earth on its inclined axis. Due to Coriolis effect, planetary winds tend to deflect to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. The deflection is least at the Equator and greatest at the poles.
Question 3(a)
Explain the weather conditions associated with tropical and temperate cyclones.
Answer
Tropical cyclones-
- Tropical cyclones are mainly developed over the sea.
- They are usually limited to a small area and usually travel from east to west.
- When there is a tropical cyclone the air is still, but the temperatures and the humidity are high. There is sudden drop in air pressure.
- When the front of the vortex arrives, there are strong winds and thick clouds, then the winds become violent with great speed. Dense clouds and heavy rain reduce visibility.
- The eye of the cyclone heralds a calm condition.
- When the rear of the vortex arrives, there are violent winds, thick clouds and heavy rains. The wind blows in the opposite direction.
Temperate Cyclones-
- Temperate cyclones are produced both on land and on sea.
- They occupy areas measuring a couple of thousands of kilometres and move from west to east.
- In a temperate cyclone, the wind speed is low.
- All sectors of the cyclone have different temperatures.
- There is not a single place where the winds and rains are inactive.
- Direction of winds rapidly change at the front.
- The approach of a temperate cyclone is marked by fall in temperature, fall in the mercury level, wind shifts and a halo around the sun and the moon.
- A light drizzle follows which turns into a heavy downpour.
- They cause light rainfall which continues for many days.
Question 3(b)
What are the Jet Streams? What is the significance of the Jet Streams?
Answer
Jet streams refer to the concentrated bands of rapid air movement found at the tropopause and the stratosphere, located at 10-15 km above the surface of the Earth.
The significance of jet streams is as follows-
- Most weather systems are moved forward with the jet streams. The position and strength of the jet stream then helps meteorologists forecast future weather events.
- The airline industry consistently uses the jet stream for its flights, which reduces the flight time and aids in reduction in fuel consumption.
- Precipitation usually increases in California because the polar jet stream moves farther south and brings more storms with it. In addition, precipitation often increases in Europe because the jet stream is stronger in the Northern Atlantic.
- Whatever the position of the jet stream, it has a significant impact on the world's weather patterns and severe weather events like floods and droughts.
Question 3(c)
Give a geographical reason for each of the following:
(i) Doldrums is a low pressure belt.
(ii) Equatorial regions have low atmospheric pressure throughout the year.
(iii) Low atmospheric pressure prevails over the Circum-polar region.
Answer
(i) Doldrums extend from 0 to 5° North and South of Equator. Due to the vertical rays of the sun here, there is intense heating. The air expands and rises as convection current, causing a low pressure to develop here. Hence, Doldrums is a low pressure belt.
(ii) Equatorial regions have low atmospheric pressure throughout the year because atmospheric pressure decreases with increase in temperature. This is because when the temperature rises, air expands. The molecules of air move far apart and hence exert less pressure. On the contrary, with decrease in temperature, the air gets compressed and the space between molecules decreases and exerts more pressure on the region.
(iii) In the sub-tropical region the descending air gets divided into two parts. One part blows towards the Equatorial Low Pressure Belt. The other part blows towards the Circum-Polar Low Pressure Belt. This zone is marked by ascent of warm Sub-Tropical air over cold polar air blowing from poles. Due to earth's rotation, the winds surrounding the Polar region blow towards the Equator. Centrifugal forces operating in this region create the low pressure belt, known as Circum-polar low pressure belt.
Question 3(d)
Draw a well labelled diagram showing a cyclone in the Northern Hemisphere.
Answer
Below labelled diagram shows a cyclone in the Northern Hemisphere:
Thinking Skills
Question 1
State two situations when you physically felt the effect of the atmospheric pressure. Give reasons to support your answer.
Answer
Two situations when I physically felt the effect of the atmospheric pressure are:
- I felt discomfort when I travelled by plane for a vacation. It happened because when travelling in a plane, changes in altitude cause variations in atmospheric pressure. The pressure inside the cabin differs from the pressure at ground level. These pressure differences can lead to discomfort, particularly in the ears, sinuses, and other air-filled cavities, which can be alleviated by equalizing the pressure.
- On the vacation, I visited Ladakh. There my nose started bleeding due to decrease in atmospheric pressure at high altitude. As blood pressure exceeded the atmospheric pressure, it resulted in nose bleeding.
Question 2
You must have read in newspapers or seen on TV channels, the news of cyclonic storms like Amphan, Nisarga, Fani, Yaas, Tauktae, Guiab, etc. affecting different parts of the country. Find out the origin and effects of atleast three of these cyclonic storms.
Answer
Cyclone Fani
Origin — Cyclone Fani originated from a low-pressure system that formed in the Bay of Bengal in late April 2019. It intensified into a severe cyclonic storm and made landfall near Puri, Odisha, India, on May 3, 2019.
Effects — Cyclone Fani caused widespread destruction in Odisha and parts of West Bengal. It resulted in heavy rainfall, strong winds and storm surges, causing significant damage to infrastructure, including buildings, roads and power lines. The storm led to the evacuation of millions of people from coastal areas, minimizing the loss of life. However, there were still casualties and extensive damage to property and agriculture.
Cyclone Yaas
Origin — Cyclone Yaas originated from a low-pressure area in the Bay of Bengal in May 2021. It rapidly intensified into a severe cyclonic storm and made landfall near Balasore, Odisha, on May 26, 2021.
Effects — Cyclone Yaas brought heavy rainfall, strong winds, and storm surges to coastal areas of Odisha and West Bengal. It caused significant flooding, damaging houses, infrastructure, and agriculture. The storm led to the evacuation of millions of people from vulnerable regions, minimizing the loss of life. However, there were still reports of casualties and widespread disruption to daily life.
Cyclone Tauktae
Origin — Cyclone Tauktae originated from a depression over the Arabian Sea in May 2021. It rapidly intensified into an extremely severe cyclonic storm and made landfall near Gujarat, India, on May 17, 2021.
Effects — Cyclone Tauktae brought heavy rainfall, strong winds and storm surges to the coastal areas of Gujarat, Maharashtra, Kerala, Karnataka and Goa. The storm caused widespread damage to infrastructure, including buildings, power lines and communication networks. It resulted in casualties and displacement of people along with significant disruptions to transportation and economic activities. The cyclone also affected offshore activities, including fishing and oil drilling operations.