Chapter - 4 Climate
Weather:- Weather refers to the day-to-day condition of the atmosphere at a particular place and time. It includes elements like temperature, humidity, rainfall, wind speed, etc. Example: "It is raining today in Delhi."
Climate:- Climate is the average weather pattern of a place over a long period of time (usually 30 years or more). It describes general atmospheric conditions like overall temperature, rainfall, etc., of a region. Example: "India has a monsoon climate."
Climate of India
- India has a monsoon type climate.
- Influenced by latitude, altitude, and relief features.
3. Factors Affecting India’s Climate
Latitude
- The Tropic of Cancer (23.5°N) passes almost through the middle of India.
- It divides the country into two climate zones:
- Tropical zone (south of the Tropic): Hot throughout the year with less seasonal variation.
- Example: Chennai – remains warm even in winter.
- Subtropical zone (north of the Tropic): Has hot summers and cold winters.
- Example: Delhi – very hot in summer and cold in winter.
Altitude
- Temperature decreases as we go higher above sea level.
- Example: Shimla (in the hills) is cooler than Delhi, even though both are in the north.
- Pressure and Winds – Includes monsoon winds, jet streams, and western disturbances.
- Distance from the Sea – Coastal areas have moderate climate; interiors are extreme.
- Relief – Hills and mountains affect temperature and rainfall patterns.
Pressure and Winds:- Atmospheric pressure and winds play a major role in deciding the climate of India. The movement of air from high-pressure to low-pressure areas causes winds, which bring changes in temperature and rainfall.
Coriolis Force:- The Coriolis Force is a force caused by the rotation of the Earth. It affects the direction of winds and ocean currents.
- It deflects moving air (winds) and water to the right in the Northern Hemisphere and to the left in the Southern Hemisphere.
- Because India is in the Northern Hemisphere, winds here get deflected to the right.
- It carry moisture and bring rain.
Indian Monsoon
- Monsoon: Seasonal reversal of winds bringing rainfall.
- Summer Monsoon (June–Sept): Moist winds from the sea to land → rainfall.
- Winter Monsoon (Oct–Feb): Dry winds from land to sea → less rain (except east coast).
- Retreating Monsoon (Oct–Nov): Withdrawal of monsoon; causes cyclones in Bay of Bengal.
Key Features:
- Cool Temperatures:
- The northern plains become very cold, especially in January.
- Example: Delhi, Amritsar, and Srinagar experience low temperatures.
- The southern parts of India (like Chennai and Kochi) remain warm.
- Clear Skies and Dry Weather:
- The weather is mostly clear with little rainfall in most areas.
- Humidity is low.
- Western Disturbances:
- These are winds that come from the Mediterranean Sea.
- They bring light rain to north and northwest India, especially Punjab and Haryana.
- Mahawat:- Winter rainfall locally known as "Mahawat".
- This rain is important for the rabi crops like wheat.
- High Pressure Over Land:
- A high-pressure area forms over north India.
- Winds blow from the land to the sea, which makes the season dry.
- Temperatures rise steadily throughout the country.
- Example: Northern plains like Delhi, Jaipur, and Lucknow often see temperatures above 40°C in May.
- Central India becomes extremely hot, especially in areas like Nagpur.
- Due to the intense heat, a low-pressure area develops over northwestern India.
- This low pressure attracts moist winds from the sea, which later helps bring the monsoon.
- In northern India, hot, dry winds called Loo blow in the afternoons during May and June.
- These winds can cause heatstroke and are dangerous.
- In eastern India, especially in West Bengal and Assam, strong winds with rain and thunderstorms occur.
- These storms are called "Kalbaisakhi" or Nor’westers.
- They help cool down the region and are useful for early crops.
- The Southwest Monsoon winds begin to blow from the sea toward the land.
- These winds carry a lot of moisture from the Arabian Sea and Bay of Bengal.
- First hits Kerala around June 1, then spreads across the country.
- These winds bring heavy rainfall to most parts of India.
- Western Ghats, Northeast India, and coastal areas receive very high rainfall.
- Example: Mawsynram in Meghalaya gets the highest rainfall in the world.
- Arabian Sea Branch: Hits the Western Ghats, giving heavy rain to Kerala, Karnataka, Maharashtra.
- Bay of Bengal Branch: Moves towards northeast India, then towards the north and northwest.
- The Southwest Monsoon starts retreating from northwestern India by early October.
- It gradually moves out of the country by mid-November.
- After the rain stops, skies become clear.
- The temperature remains high during the day, especially in southern India.
- This hot and humid weather in October is called “October Heat.”
- The low-pressure area shifts to the Bay of Bengal.
- Winds change direction and start blowing from land to sea.
- The Northeast Monsoon winds pick up moisture from the Bay of Bengal.
- These bring rainfall to Tamil Nadu, southern Andhra Pradesh, and parts of Kerala.
- This season is also known for cyclonic storms in the Bay of Bengal.
- These can cause heavy damage, especially along the eastern coast.
1. Areas of High Rainfall (More than 200 cm per year):- Found in the Western Ghats, Northeast India, and Himalayan foothills. Example:
- Mawsynram (Meghalaya) – highest rainfall in the world.
- Western coast – Kerala, Karnataka, and Goa.
- Assam and Arunachal Pradesh.
Found in most of the northern plains, eastern Rajasthan, Madhya Pradesh, and parts of the Deccan Plateau. Examples:- West Bengal, Uttar Pradesh, Maharashtra (some parts).
3. Areas of Low Rainfall (50–100 cm per year):- Includes interior Deccan, central Rajasthan, Punjab, and Haryana. Rainfall is less but still enough for some crops.
4. Areas of Very Low Rainfall (Below 50 cm per year):- Found in desert and semi-desert areas. Examples:- Western Rajasthan (like Jaisalmer), Parts of Ladakh.
- Himalayas protect the subcontinent from extermely cold winds from central asia. Northen India to have uniformly higher temperatures compared to other areas on same latitudes.
- Peninsular Plateau:- Under the influence of the sea from three sides, has moderate temeperatures.
- The arrival of monsoon is celebrated across regions in different ways, showing its emotional and cultural importance.
- A large part of India’s population depends on farming, and most crops need monsoon rain.
- Example: Crops like rice, sugarcane, and cotton are mainly grown with monsoon water.
- So, farmers across India share the same hope and concern for good rainfall.