The Bay of Bengal branch is the most active one in the monsoon season. This branch strikes the coast of Myanmar and part of Bangladesh. The Arakan Hills, however, deflect a big portion of this branch towards India. The monsoon, therefore, enters West Bengal and Bangladesh from south and southeast instead of from the south-westerly […]
Over the Arabian Sea, monsoon winds alternately blow from the northeast and the southwest, reversing their dominant direction with the seasons. In the winter, the winds blow from Southwest Asia toward the sea. The monsoon winds originating over the Arabian Sea further split into three branches: It’s one branch is obstructed by the Western Ghats.
The southwest monsoon season is considered the most critical and significant season of the year to the people of India. This is because it brings relief from the scorching heat of the hot summer. Increase of temperature in May over the northwestern plains, the low pressure conditions over there get further intensified. By early June,
They are highly known for their wide range of extreme weather conditions. It can be both chilly and chilly like the winters or it could be completely hot like in summers. Hot weather season is usually accompanied by dust storms that pick up pace as winds blow. They move at an incredible speed causing huge
November is the beginning of the cold weather season of north India. December and January are considered to be the coldest months in the northern plain. The temperature usually dips below freezing point in these two months. There are three main reasons for the excessive cold in north India during this season: States like Punjab,
The different climatic conditions prevalent in India are basically dependent on the seasonal changes in the temperature, rainfall, humidity etc. The climatic conditions of India can best be described in terms of an annual cycle of seasons. The climatic conditions of India can best be described in terms of an annual cycle of seasons. The
Monsoon refers to a seasonal change of winds, characterized by heavy rains. A monsoon’s season is triggered towards the end of the summer due to the difference between hot and cold air masses. The warm air mass lands on India from tropical landmasses over the Indian Ocean. Once the warm winds hit the continental land,
SOLANKI SCHOOL In the North-western part of India including Gujarat and Rajasthan, this school developed under the patronage of the Solanki ruler. Temples walls devoid of any carvings. Gharbhagriha connected with Mandapa both internally as well as externally. Porticos have decorative arched gateways known as Torans. Unique feature is the presence of step-tank. Variety of
SOLANKI SCHOOL – UPSC Daily Important Topic | 9 October 2021 Read More »
Scientists and meteorologists continue to study and predict the effects of EI-Nino. However, for people living in areas that are vulnerable to the yearly monsoon, this represents a major challenge, particularly in India where there is a long history of devastating floods and droughts affecting the lives and livelihoods of many. What is EI-Nino? EI-Nino
The monsoon is one of the major climatic features of India, and has a profound influence on the economy of the country. The distribution and characteristics of rainfall during the South West Monsoon (SWM) season in India is well documented by meteorological elements and in literature. There seem to be two rain-bearing systems in India.
