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:
- Latitude: Temp decreases from Equator to Poles.
- Altitude: Temp decreases as height increases.
- Pressure & Wind System: Depends on lat/altitude. Influences rain.
- Distance from Sea: Moderating influence. Farther = Extreme weather (Continentality).
- Ocean Currents: Warm/Cold currents affect coastal climate.
- 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.
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).
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.
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.
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.
Why houses differ?
• Rajasthan: Thick walls/flat roofs (Insulation).
• Tarai/Goa: Sloping roofs (Heavy rain).
• Assam: Stilts (Floods/Dampness).
• 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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