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Subjects

Geography

Distribution of Rainfall

In Class 9 Geography, under the chapter Climate, students study the distribution of rainfall across India. The topic explains how rainfall varies from region to region, identifies areas receiving very heavy, moderate, or low rainfall, and relates these patterns to factors such as relief features, monsoon winds, and distance from the sea.

Hard · Level 5 · 25 questions

TOPIC PRACTICE

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25 questions

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  1. Because wind direction relief distance from sea and local factors also affect it
  2. Because monsoon gives no rainfall in India
  3. Because rainfall is equal in every region
  4. Because rainfall occurs only in Himalayas
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  1. Sandy soil and hot wind
  2. Moist Bay of Bengal winds and hill barriers
  3. Ladakh rain shadow
  4. Parallel direction of Aravalli
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  1. Low moisture and Aravalli direction parallel to winds
  2. Strong uplift by Khasi Hills
  3. Windward slope of Western Ghats
  4. Very high coastal humidity
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  1. Rain shadow effect
  2. Sea tide
  3. Loo effect
  4. Cold wave
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  1. Waterlogging and flood
  2. Permanent drought
  3. Complete absence of moisture
  4. Desert expansion only
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  1. Moisture decreases in monsoon winds from east to west
  2. The Bay of Bengal is in the west
  3. Delhi is on the sea coast
  4. Eastern part is in rain shadow
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  1. Strong regional unevenness of rainfall in India
  2. Equal rainfall everywhere in India
  3. Only snowfall in India
  4. No relation of rainfall with relief
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  1. Because it receives important rainfall from retreating monsoon
  2. Because it never receives rainfall
  3. Because it is located in Ladakh
  4. Because it is part of Thar Desert
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  1. Sharp contrast of orographic rain and rain shadow could reduce
  2. Deccan would never receive rain
  3. Western coast would surely become desert
  4. Meghalaya rainfall would stop
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  1. Because limited rainfall can be saved for future use
  2. Because it completely stops rainfall
  3. Because it destroys moisture
  4. Because it is useful only in flood areas
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  1. Meghalaya very heavy rainfall
  2. Ladakh humid coastal area
  3. Western Rajasthan very heavy rainfall
  4. Rain shadow Deccan dense rainforest
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  1. Himalayan rain shadow
  2. Direct moisture of Arabian Sea
  3. Barrier of Khasi Hills
  4. Western coastal location
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  1. Uneven rain can increase drought risk in some areas and flood risk in others
  2. Risk ends everywhere
  3. Rainfall has no relation with farming
  4. Only cities are affected
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  1. Western Coast and Western Ghats
  2. Cold desert of Ladakh
  3. Interior Thar
  4. Dry western Rajasthan
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  1. Meghalaya and North-Eastern India
  2. Western Rajasthan
  3. Ladakh
  4. Rann of Kachchh
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  1. Because intense short rainfall can increase runoff and flooding
  2. Because intensity has no effect
  3. Because amount is always wrong
  4. Because rainfall happens only at night
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  1. Winter rainfall in north-west India
  2. Summer extreme rainfall in Meghalaya
  3. South-western flood in Thar
  4. Daily rainfall on Coromandel Coast
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  1. Kharif farming and water availability
  2. Height of Himalayas
  3. Sea salt production only
  4. Map colour scheme
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  1. Where rainfall is uneven water availability also varies by region
  2. Rainfall and water resources are unrelated
  3. Low rainfall always gives more groundwater
  4. High rainfall always creates water scarcity
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  1. Local hills valleys and wind direction
  2. Complete absence of sea
  3. Non arrival of monsoon
  4. Desert sand only
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  1. Western slope of Western Ghats and interior Deccan
  2. Meghalaya and Assam only
  3. Population of Delhi and Kolkata
  4. Soil of Kachchh and Thar
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  1. Coastal areas may have more moisture and some interior areas less moisture
  2. Distance from sea has no relation with moisture
  3. All interior areas receive highest rainfall
  4. All coastal areas are dry deserts
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  1. If storage distribution and management are weak
  2. Because rainwater is never useful
  3. Because high rainfall produces no water
  4. Because rivers always disappear
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  1. Ladakh
  2. Malabar Coast
  3. Mawsynram
  4. Konkan
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  1. Wrong conclusions about regional climate and water planning
  2. Mountains will change immediately
  3. Rainfall will stop
  4. Sea will dry up

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