Chapter 4- Climate(Geography) Class -9 Subject- Social Science
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Latitude – Tropic of Cancer divides India into tropical and subtropical zones.
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Altitude – Mountains like Himalayas keep cold winds out; high places are cooler.
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Pressure and Winds – Seasonal winds like monsoon and western disturbances affect climate.
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Distance from the sea – Coastal areas have moderate climate; interior areas are extreme.
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Ocean currents – Warm or cold currents influence coastal temperatures.
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Relief features – Mountains cause rain on one side and dry conditions on the other (rain shadow).
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India experiences a seasonal reversal of winds due to pressure changes.
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In summer, low pressure develops over land and winds come from sea – bringing rain.
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In winter, winds blow from land to sea – making it dry.
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This change causes the monsoon type of climate.
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Most of the rainfall occurs in four months (June to September).
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The Thar Desert in Rajasthan has the highest diurnal range.
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This is because days are extremely hot and nights are very cool due to lack of moisture and vegetation.
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The Southwest monsoon winds cause heavy rainfall along the Malabar Coast.
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These winds come from the Arabian Sea and hit the Western Ghats.
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Seasonal winds that reverse direction with season changes.
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Bring most of India’s rainfall.
Break in monsoon:
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Gaps or pauses in rainfall during the rainy season.
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There are wet and dry spells, not continuous rain.
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Monsoons bring rain that is essential for agriculture in all parts of India.
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Despite different climates, all regions wait for monsoon rains.
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Festivals, crops, and people's lives revolve around monsoon.
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It creates a seasonal rhythm across the country.
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It connects India from north to south and east to west through its impact.
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Monsoon winds enter India from the Bay of Bengal in the east.
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They move towards the north-west after dropping most of their moisture.
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Eastern states like West Bengal and Bihar get more rain.
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By the time winds reach Punjab and Rajasthan, they have less moisture.
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This results in decreasing rainfall from east to west in Northern India.
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Due to changes in temperature and pressure over land and sea.
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In summer: land heats → low pressure → winds come from sea (rainy).
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In winter: land cools → high pressure → winds blow to sea (dry).
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Most rain is caused by southwest monsoon winds.
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These winds come only during June to September.
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Due to northeast monsoon winds blowing from Bay of Bengal to land.
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These pick moisture and bring rain to Tamil Nadu in October–November.
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Cyclones form in the Bay of Bengal during the retreating monsoon.
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These move towards the east coast, hitting deltas of Krishna, Godavari, Kaveri.
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These regions are either far from the monsoon path or in the rain shadow area.
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They receive less than 60 cm of rainfall annually.
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Temperature differences: Rajasthan may reach 50°C in summer, while Drass in J&K goes below –45°C in winter.
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Rainfall variation: Mawsynram receives over 400 cm of rainfall; Jaisalmer gets less than 10 cm.
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Day-night difference: Thar Desert has large difference; Kerala and Andaman have uniform temperature.
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Season length: Winters are long in north India, but barely noticeable in south India.
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Relief impact: Mountains like the Western Ghats get rain, but areas behind them are dry.
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Occurs from mid-November to February; December–January are coldest months.
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Northeast trade winds blow from land to sea – dry in most parts.
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Rainfall in Tamil Nadu due to these winds from Bay of Bengal.
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Western disturbances bring winter rain to north India – good for rabi crops.
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Weather: clear skies, low temperature, low humidity, and frost in north.
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Brings most of the annual rainfall between June and September.
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Rainfall is unevenly distributed – floods in some areas, drought in others.
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Monsoon is uncertain – arrival and amount vary every year.
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Important for agriculture, as most farmers depend on it.
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Monsoon influences festivals, crops, economy, and daily life in India.
Cahpter 1- What is Democracy? Why Democracy?
Chapter 2- Constitutional Design
Chapter 3- Electoral Politics
Chapter 4- Working of Institutions
Class 9- Economics
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