Climate of India

Climate of India 

The sum of the long-term average conditions of the atmosphere is known as climatic conditions.
 The yoga of a similar state living in an end time period is called the weather which changes in the short term.
 The climate of India is called monsoon climate. Monsoon is derived from the Arabic word Mohsin, which means the change in the wind is due to the Indian climate.
Position and latitudinal expansion North Mountain range Distance from the ocean Distance from the ocean bottom
 Topography Because of the sum of all the reasons, the climate of India is called the tropical monsoon climate.
    Indian climate is divided into four seasons summer autumn winter season rainy season

summer season - Summer is found in India between March to June. In this season, the temperature remains high and excessive hot air moves, which is called Lu, because after sunset in the northern part of the Northern Hemisphere, after 23 March, Is found and winter is found in the southern hemisphere

 Winter season-
From September to November, autumn is observed in India, the sun gets dakshin after 23rd September and the temperature decreases in the Indian subcontinent and high air pressure is found in place of low barrage and air is from south east to southwest. Water moves from the ground to the water department

 winter season -
In the Indian region there is cold winter in the month of November till January. In this season, there is cold winter in India and in southern India the temperature remains normal, the winds in the north 3: 30 degrees North latitudes Who are called cold-blooded

 Rainy Season -
There is excessive rainfall in different regions of India between June and September, due to this, the time of rainy season is considered as due to the attraction of southern western monsoon winds in the second fortnight of June, rainy season starts in southern India in the Indian subcontinent. The southwest monsoon is active and heavy rainfall causes these monsoon rains to 75% of the annual rainfall annually in India. Southwest monsoon wind is divided into two parts


1. Arabian Sea Monsoon Sections
 The monsoon stream of the Arabian Sea reaches the shores of India and the essay is dissolved in three parts.
1 First branch heavy rainfall on Western Ghats
2 The second branch rains in the valleys of Narmada and Tapti
3 The third branch is parallel to Aravali, but also reaches central India.

 Bay of Bengal's monsoon stream
     The monsoon of the Bay of Bengal Dharavi is divided into two parts.
1 First branch grows heavy in the Gangetic plains and in the hills of Garo Khasi Jaintia
 And this is also the location of the highest rainfall in the world.
2 and the other in the areas of Himachal Pradesh, Jammu and Kashmir, colliding with the Himalayan Mountains.
 Heavy rain

 The line joining the equinox line with the same atmospheric pressure is   called the equilateral line
 it is said. A line joining similar salinity places is called the salinity line.

 The line joining the contour line equal elevation is called.

 A similar speed line is called the line measuring the velocity of the same air.