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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 1 · 25 questions

TOPIC PRACTICE

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  1. Because altitude distance from sea winds and relief also affect it
  2. Because latitude has no relation with temperature
  3. Because climate is formed only by language
  4. Because all places have the same climate
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  1. Because latitude becomes different at both places
  2. Because distance from sea is different
  3. Because the Sun shines only on the coast
  4. Because inland areas have no atmosphere
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  1. When the place is very far from sea
  2. When the place is in a plain
  3. When the place is in a high mountain area
  4. When the place is on the coast
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  1. The sea changes latitude
  2. The Sun is weak on coasts
  3. Wind does not blow on coasts
  4. Sea water heats and cools slowly
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  1. High temperature range in areas far from sea
  2. Low temperature range in coastal areas
  3. Low temperature on high mountains
  4. Direction of ocean currents
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  1. Dry air descends
  2. Moist air rises after striking the mountain
  3. Sea is always absent there
  4. Latitude suddenly changes
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  1. The Sun never rises there
  2. Air pressure is zero there
  3. Air has lost much moisture while crossing the mountain
  4. Ocean current removes the mountain
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  1. Ocean current
  2. Latitude
  3. Distance from sea
  4. Relief
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  1. It helps block cold northern winds
  2. It makes India completely dry
  3. It moves the sea away from India
  4. It measures the angle of Sun rays
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  1. They end latitude
  2. They change wind direction and moisture flow seasonally
  3. They measure mountain height
  4. They stop ocean currents
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  1. Coastal temperature may become relatively lower
  2. Latitude of the coast will change
  3. The sea will disappear
  4. The atmosphere will end
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  1. By always making coast glacial
  2. By raising coastal temperature relatively
  3. By decreasing latitude
  4. By removing mountains
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  1. Rainfall of only one day
  2. Only school timing
  3. Coastal and mountain places having different climates even at same latitude
  4. Same temperature everywhere
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  1. Southern India is surrounded by the Himalaya
  2. Southern India has no latitude
  3. Winds do not blow in southern India
  4. Southern India is surrounded by sea on three sides
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  1. Because language can differ
  2. Because latitude distance from sea and winds also affect climate
  3. Because altitude has no relation with temperature
  4. Because high places have no Sun
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  1. Language distribution
  2. Currency value
  3. Air circulation and moisture transport
  4. Road construction
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  1. In a flat plain without wind
  2. In the middle of sea
  3. In an area without mountains
  4. Mountains stand in the path of moist winds
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  1. Distance from sea and temperature range
  2. Language and air pressure
  3. School and ocean current
  4. Clothes and latitude
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  1. Latitude and solar energy
  2. Altitude and temperature
  3. Relief and rainfall distribution
  4. Language and ocean current
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  1. Rays are more direct at low latitudes and more slanting at high latitudes
  2. Rays are same at every latitude
  3. Latitude only measures rainfall
  4. Latitude is depth of sea
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  1. Look only at distance from sea
  2. Look only at altitude
  3. Look at the combined effect of both controls
  4. Treat climate as chance
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  1. Altitude
  2. Relief
  3. Latitude only
  4. Nearness to sea
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  1. Rainfall
  2. Language
  3. Road width
  4. Currency
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  1. More rainfall on western coast and less rainfall in leeward areas
  2. Equal rainfall across India
  3. Complete end of monsoon
  4. Only cooling of sea
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  1. Very high maritime influence
  2. Distance from sea and dryness
  3. Permanent glaciers
  4. Dense maritime moisture

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