Class 9 Climate

Climate of India – Topper Notes

Climate (जलवायु)

1. Introduction

  • Climate: Sum total of weather conditions & variations over a large area for a long period (>30 years).
  • Weather: State of atmosphere over an area at any point of time.
  • Elements: Temperature, Atmospheric Pressure, Wind, Humidity, Precipitation.
  • Monsoon: Seasonal reversal in wind direction during a year. (Arabic ‘Mausim’ = Season).

2. Climatic Controls (जलवायु नियंत्रण)

There are 6 major controls of climate:

  1. Latitude: Temp decreases from Equator to Poles.
  2. Altitude: Temp decreases as height increases.
  3. Pressure & Wind System: Depends on lat/altitude. Influences rain.
  4. Distance from Sea: Moderating influence. Farther = Extreme weather (Continentality).
  5. Ocean Currents: Warm/Cold currents affect coastal climate.
  6. Relief: Mts act as barriers (Rain shadow vs Windward side).

3. Factors Affecting India’s Climate

  • Latitude: Tropic of Cancer divides India into Tropical (South) & Sub-tropical (North).
  • Altitude: Himalayas prevent cold winds from Central Asia → Milder winters.
  • Winds: India lies in NE Trade Winds region.
Equator Right Deflection (NH) Left Deflection (SH)
Fig: Coriolis Force
★ Coriolis Force:
Apparent force caused by earth’s rotation. Deflects winds to Right in Northern Hemisphere and Left in Southern Hemisphere. (Ferrel’s Law).
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The Seasons (ऋतुएँ)

4. The Cold Weather Season (Winter)

  • Duration: Mid-November to February.
  • Coldest Months: December & January.
  • Temp decreases from South to North.
  • Winds: NE Trade winds prevail (Land to Sea → Dry).
  • Tamil Nadu coast gets rain (Sea to Land winds).
  • Western Cyclonic Disturbances: From Mediterranean Sea. Cause winter rain (Mahawat) → Good for Rabi crops.

5. The Hot Weather Season (Summer)

  • Duration: March to May.
  • Heat belt shifts northwards. Temp rises to 45°C in NW India.
  • Loo: Strong, gusty, hot, dry winds (daytime).
  • Kaal Baisakhi: Localized thunderstorms in West Bengal.
  • Mango Showers: Pre-monsoon showers in Kerala/Karnataka (help mangoes ripen).

6. Advancing Monsoon (Rainy Season)

  • Duration: Early June to September.
  • Low pressure over Northern Plains attracts SE Trade Winds from S. Hemisphere.
  • Cross equator → Turn right → SW Monsoon.
  • Breaks in Monsoon: Wet & dry spells interspersed.
  • Mawsynram: Highest average rainfall in the world.
Arabian Sea Branch Bay of Bengal Branch
Fig: Advancing Monsoon
El Niño:
Warm ocean current along Peru coast. Replaces cold Peruvian current. Leads to increase in sea-surface temperature & weakening of monsoon.
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Retreating Monsoon (लौटता मानसून)

7. Retreating Monsoon (Transition)

  • Duration: October – November.
  • Monsoon trough weakens → replaced by high pressure.
  • Clear skies + Rise in temperature.
  • October Heat: Oppressive weather due to high temp & humidity.
  • Cyclones shift to Bay of Bengal → Hit East Coast (Godavari/Krishna/Kaveri deltas).
  • Bulk of rainfall on Coromandel Coast occurs now.

8. Distribution of Rainfall

  • High (>400 cm): West Coast & NE India.
  • Low (<60 cm): W. Rajasthan, Gujarat, Haryana, Punjab, Leh.
  • Rest of country: Moderate.
  • Snowfall: Himalayan region.

9. Monsoon as Unifying Bond

Despite regional variations, the monsoon provides a rhythmic cycle of seasons.

  • Indian landscape, animal/plant life, agricultural calendar, and festivals revolve around it.
  • Binds the whole country by providing water for agriculture.
  • River valleys act as single units.
Meghalaya Rajasthan Rainfall Variability
Why houses differ?
Rajasthan: Thick walls/flat roofs (Insulation).
Tarai/Goa: Sloping roofs (Heavy rain).
Assam: Stilts (Floods/Dampness).
Key Terms:
  • Jet Streams: Fast flowing air currents in upper atmosphere.
  • ITCZ: Inter Tropical Convergence Zone (Low pressure trough).

“Climate dictates our Lifestyle!” ☁☀☔

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