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Thirty question-and-answer flashcards covering core ideas about India’s climate, monsoons, and related geographic concepts for Grade 10 Geography revision.
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A tropical monsoon climate.
What type of climate prevails over most of India?
(i) India’s location in the tropical belt. (ii) Dominant influence of seasonal monsoon winds confined largely to the tropics.
It is highly seasonal and unequal in distribution; arrival, intensity, and withdrawal are erratic and unreliable.
North (temperate zone) has hot summers and cold winters; South (tropical zone) is generally warmer and lacks a clear-cut winter.
They supply moisture to summer monsoons and moderate temperatures, giving coastal areas an equable climate with heavy rain.
Fast, cold, high-altitude winds that blow in the upper atmosphere and influence weather patterns.
Westerly jet streams bring temperate cyclones to North India in winter; easterly jet streams steer tropical depressions that dictate monsoon rain distribution.
A warm current in the equatorial Pacific that raises sea-surface temperatures and weakens Indian monsoon winds, often causing drought or delayed rains.
Around the first week of June (traditionally 1 June).
The sudden, vigorous onset of heavy Southwest Monsoon rainfall, first felt on the Kerala coast in early June.
Moisture-laden Southwest Monsoon winds blow from sea to land during this period; winter Northeast winds are dry offshore winds.
Southward shift of the sun weakens the Ganga low-pressure trough, which is replaced by high pressure, causing retreat.
They form over warm tropical seas, have higher wind speed and moisture content, producing torrential rain on landfall.
Mumbai’s coastal location moderates winter temperatures, whereas inland Kanpur experiences continental extremes.
Temperate cyclones (Western Disturbances) originating near the Mediterranean that move eastward into North India.
Western Ghats force Arabian Sea branch winds to rise and drop heavy rain on the windward Malabar side; Tamil Nadu lies in the rain-shadow and parallel to the Bay of Bengal branch.
They are far from maritime influence, causing very hot summers and very cold winters.
It lies on the leeward (rain-shadow) side of the Western Ghats, so the Arabian Sea branch loses moisture before reaching it.
Higher altitude (lapse rate ~1 °C per 166 m) makes temperatures fall with elevation.
Kochi’s coastal (marine) climate moderates temperatures; inland Agra has continental extremes.
Varied relief—mountain barriers like the Western Ghats or Aravallis create windward wet zones and leeward dry zones.
The Himalayas block icy Siberian winds, preventing extreme cold from penetrating southward.
Rainfall of the Bay of Bengal branch decreases from southeast to northwest across the Gangetic Plain; Patna lies farther southeast.
Shillong lies on the leeward side of the Khasi Hills, whereas Cherrapunji is on the windward side facing moisture-laden monsoon winds.
They have lower wind speeds and lighter rainfall because they form over land or cooler seas in winter.
Annual Mean Temperature = (Highest monthly mean + Lowest monthly mean) ÷ 2.
Annual Range of Temperature = Highest monthly mean − Lowest monthly mean.
The Northeast Monsoon winds that pick up moisture over the Bay of Bengal.
The Aravallis run parallel to the Arabian Sea monsoon flow and are too low to block the already exhausted Bay of Bengal branch.
About 1 °C drop for every 166 m rise in elevation (≈6.5 °C per 1,000 m).