AP Board 10th Class Social Studies Notes Chapter 4 Climate of India

Students can go through AP State Board 10th Class Social Studies Notes Chapter 4 Climate of India to understand and remember the concept easily.

AP State Board Syllabus 10th Class Social Studies Notes Chapter 4 Climate of India

→ What have been the general conditions, year after year over thirty years or more gives us the climate,

→ The elements of weather and climate are temperature, atmospheric pressure, wind, humidity, and precipitation,

→ Climograph shows average monthly values of maximum temperature, minimum temperature, and rainfall for a given place.

→ The factors that affect climate are called climatic controls. These include

  • Latitude
  • Land-water relationship
  • Relief and
  • Upper air circulation.

→ The average temperatures for the year drop as you go further away from the Equator.

→ Darker areas such as heavily vegetated regions tend to be good absorbers; lighter areas, such as snow and ice-covered regions, tend to be good reflectors.

→ The difference between the temperature of day and night and that of summer and winter is not much. This is known as ‘equable climate’.

→ Hills and mountains will have lower temperatures than locations on the plain.

→ The climate of India is affected by the movement of upper air currents in the atmosphere above 12,000 m called ‘Jet Streams’.

→ The temperature in the Indian landmass considerably reduces from Mid-November and this cold season continues till February.

→ During the hot season, as we move from the southern to the northern part of the country, the average temperature increases.

AP Board Solutions AP Board 10th Class Social Studies Notes Chapter 4 Climate of India

→ The monsoon forms in the tropical area approximately between 20eN and 208S latitudes,

→ The bulk of annual rainfall in India is received from the southwest monsoon.

→ The retreat of the monsoon is marked by clear skies and a rise in temperature.

→ As the Earth started to take shape from a fire bail to a planet, many gases were released.

→ These gases did not escape into outer space because of the Earth’s gravitational pull, and it still holds them back.

→ The atmosphere traps a lot of solar energy that reaches the Earth by preventing it from totally escaping back into space. This is called the Greenhouse effect.

→ Much of the warming has been occurring since thelhdfiStrfal Revolution is because of human activities. Hence, the current global warming is Anthropogenic Globed Warming.

→ Methane is said to be even more powerful than carbon dioxide as a greenhouse gas. c& AGW (Anthropogenic Global Warming) is causing many changes in the distribution of heat in the Earth system.

→ One of the human activities that contribute to global warming is deforestation.

→ An international effort to form an agreement whereby all countries try to reduce their emission of greenhouse gases has so far not been achieved.

→ Climograph: Graphs that show average monthly values of maximum temperature, minimum temperature, and rainfall for a given place.

→ Weather: The state of the atmospheric conditions over an area at a particular time.

→ Monsoon: The seasonal reversal of wind system in India.

→ Insolation (IncomIng solar radiation): The heat coming from the Sun to the Earth’s surface In the form of rays.

→ Jet streams: The fast flowing upper air currents in a narrow belt In the upper atmosphere above 12,000 m.

→ Pressure zone: The exertion of force by one body on the surface of another.

→ Global Warming: Atmosphere traps a lot of solar energy that reaches Earth by preventing it from totally escaping into space This is called Global Warming.

AP Board Solutions AP Board 10th Class Social Studies Notes Chapter 4 Climate of India

→ Climate Weather conditions followed a similar general pattern over many years over a large area.

→ Climatic controls The factors that affect climates like latitude, relief, land-water relationship, and upper air circulation.

→ Equable climate: The climatic condition where the differences between the temperatures of day and night and summer and winter are not much

→ Trade winds: Winds blowing from sub4roplcal high-pressure belt to equatorial low-pressure belt by reflecting towards the west are called trade winds.

→ Western disturbances: Cyclone depressions coming from the mediterranean sea.

→ Loo: A dry hot wind that blows In the northern plain of India.

→ Bursting monsoon: The pre-monsoon showers towards the end of the summer season in the Deccan Plateau.

→ Mango showers: The pre-monsoon showers In Andhra Pradesh helping the early ripening of mangoes.

→ The onset of the monsoon: By the beginning of June, the arrival of the Arabian Sea branch and the Bay of Bengal branch in India is called the onset of the monsoon.

→ The onset of the monsoon: By the beginning of June, the arrival of the Arabian Sea branch and the Bay of Bengal branch in India is called the onset of the monsoon.

→ Anthropogenic Global Warming: Global warming that is caused by humans since the Industrial Revolution.

→ October heat: WIth high temperature and humidity, the weather becomes oppressive during the retreat of the monsoon is called October heat.
AP Board 10th Class Social Studies Notes Chapter 4 Climate of India 1
AP Board 10th Class Social Studies Notes Chapter 4 Climate of India 2