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Subjects

Geography

Climatic Controls

In Class 9 Geography, the topic Climatic Controls explains why places experience different temperatures, rainfall, winds and seasons. As part of the chapter Climate, students examine the effects of latitude, altitude, air pressure and wind systems, distance from the sea, ocean currents, and relief features such as mountains. They learn to connect these controls with regional climate patterns and understand why India and other regions show varied climatic conditions.

Hard · Level 3 · 25 questions

TOPIC PRACTICE

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25 questions

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  1. Altitude distance from sea and relief may differ
  2. Latitude has no relation with climate
  3. The Sun does not reach both places
  4. Rainfall is always same at both places
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  1. It decides sea depth
  2. It affects the angle of Sun rays and energy received
  3. It completely stops air
  4. It changes soil texture
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  1. Lower places will always be colder
  2. Both will have exactly same temperature
  3. The higher place can be relatively cooler
  4. Altitude only measures rainfall
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  1. Coastal areas always have maximum range
  2. Distance from sea has no relation with range
  3. Near the sea temperature always remains zero
  4. Places far from sea may have greater temperature range
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  1. Mumbai has more moderate temperature and Delhi has greater range
  2. Delhi is more coastal and Mumbai is inland
  3. Both have equal sea influence
  4. Mumbai has no temperature
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  1. Latitude
  2. Relief
  3. Ocean current
  4. Population density
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  1. Air loses moisture on windward side and descends on leeward side
  2. Sea gives equal moisture everywhere
  3. Sun rays do not come there at all
  4. Latitude is always zero there
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  1. Only latitude
  2. Only warm ocean current
  3. Relief and moist monsoon winds
  4. Very great distance from sea
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  1. They may lie in rain shadow
  2. They are in the middle of sea
  3. Altitude is zero there
  4. Wind never blows there
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  1. Because source region decides moisture and heat properties of wind
  2. Because source region decides river length
  3. Because source region changes latitude
  4. Because source region stops day and night
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  1. When they carry moisture towards land
  2. When they come from completely dry land
  3. When they lose moisture before mountains
  4. When they have no water vapour
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  1. Through language and culture
  2. Through wind direction and air circulation
  3. Through soil thickness
  4. Through rock age
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  1. It helps control rainfall and seasonal pattern
  2. It changes latitude
  3. It stops ocean currents
  4. It reduces altitude
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  1. It blocks cold northern winds and influences monsoon
  2. It turns India into a polar ocean
  3. It ends solar energy
  4. It always stops all winds
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  1. Cold Central Asian winds could have stronger influence
  2. North India would go under the sea
  3. Sunlight would stop
  4. Rainfall would lose relation with climate
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  1. Low latitude and maritime moisture
  2. High altitude and mountain rain shadow
  3. Equable climate and warm current
  4. Coastal location and heavy monsoon
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  1. They can reduce reach of marine moisture and limit rainfall distribution
  2. They cause equal rainfall everywhere
  3. They make the region coastal
  4. They always make temperature zero
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  1. Only due to altitude
  2. Coastal location moist monsoon winds and Western Ghats effect
  3. Due to very great distance from sea
  4. Due to polar winds
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  1. Latitude angle of Sun rays
  2. Altitude effect on temperature
  3. Distance from sea effect on temperature range
  4. Population density natural climatic control
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  1. Altitude as control and temperature as element
  2. Temperature as control and altitude as element
  3. Rainfall as control and latitude as element
  4. Humidity as control and sea distance as element
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  1. Lowering temperature relatively and increasing dryness
  2. Changing latitude
  3. Removing mountains
  4. Ending climatic controls
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  1. Temperature may be relatively lower even though it is coastal
  2. The place will always be very hot
  3. Sea will have no effect
  4. Rainfall will be same every day
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  1. Equable climate has low range and continental climate may have high range
  2. Equable climate is always desert
  3. Continental climate has no temperature
  4. Sea influence is equal in both
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  1. Altitude may cool it and distance may increase temperature range
  2. Both will always make temperature same
  3. Both will increase maritime influence
  4. Both will stop wind
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  1. A high mountain place in tropical region can be cool
  2. Sea at pole will become hot
  3. Inland place will become coastal
  4. Heavy rain will occur everywhere in rain shadow

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