The Seasons

The cold weather season

the hot weather season

the advancing monsoon

the retreating monsoon

The cold weather season winter

The season begins from mid November and stay till February Northern India

Coldest month are December and January in Northern part of India

The hot weather season summer summer

The hot weather season in India ranges from March to May

Temperature up to 48 degrees celsius are experienced in North India

In Peninsular India temperature remain lower due to the moderating influence of the oceans

Advancing monsoon the rainy season

By early June the trade wind of the southern hemisphere get attracted to the northern hemisphere due to the creation of low pressure condition there

Rainfall in the Ganga Valley decreases from east to west

Rajasthan and part of Gujarat get scanty rainfall

Retreating post monsoon the transition session

During October November the movement of the sun towards south causes the monsoon through in the Northern Plains to become weaker

By early November the low pressure conditions over North Western India get transferred to the Bay of Bengal which caste cyclonic depression

Monsoon as a unifying bond

There is a great diversity in the climatic condition due to location extend and relief feature

This monsoon winds bind the whole country by providing water to set the agricultural activities in motion

Zones of Earth

The earth is divided into three zones torrid zone moderate zone frigid zone and torrentzone most biodiversity lived in torrid zone.

Torrid zone aur hottest zone because the rays of sun is directly to the equator 4 month summer 4 month winter 4 month rain

Moderate is coldest zone because mostly rays reflected the surface 10 month winter 4 month all season

Fridge day is a very coldest zone because all the rays are reflected the surface of earth all month covered by snow no season change

Wind pressure

There are two type of wind pressure high pressure and low pressure

Hot places are low wind pressure and cold places are high wind pressure

Wind are always born high pressure to low pressure to fulfill the space of low pressure is hot and high pressure is cooled because it contains water droplet because it comes in water bodies

So hot wind low pressure always traveled up word and space of hot wind low pressure the cold wind high pressure come and again the hot wind came into the space 2 to cold wind and this cycle process again and again

There is low pressure on the lithosphere and high pressure on the Hydrosphere this happens because water reflected more sun rays on the lithosphere and lithosphere where hot and by this process in low pressure wind become dry and up in the air as water vapour and they mixed into the cloud and rain on the lithosphere and we also so that air flow high pressure to low pressure then high pressure go to lithosphere

The Bay of Bengal Branch

This branch is originally directed towards the coast of Myanmar and part of south east Bangladesh but arakan yoma range along the coast of Myanmar is good enough to deflect a big chunk of this branch enabling it to enter Indian subcontinent

The monsoon therefore enters Bengal and Bangladesh from South and south-east inside of the south westerly direction

Therefore this branch is split into two under the influence of the Mighty Himalayas and the thermal low in North West Indians

The Arabian Sea branch

The Arabian Sea branch of the Southwest monsoon strike Western coast of India in Kerala on 1st June the windward side of Sahyadris receive very heavy rain

Crossing the Ghat they overrun the Deccan Plateau and Madhya Pradesh causing fair amount of rainfall

Thereafter the enter the Ganga Plains and mingle with the Bay of Bengal branch

There are various type of local wind in India these wind are as follows

Loo is the name given to the heart drive in which blue particular Li in the month of May and June in the Northern Plains Lewis common in Uttar Pradesh Punjab Haryana Bihar

Kal Baisakhi in the Bengal the local wind are called kalbaisakhi meaning the ceremony of the month of Baisakhi these local wind are completed by thunderstorm and bring rainfall this rain in the month of April to may is good for tea crops in Assam and jute and rice in Bengal

Mango shower these occur in South India during April May they bring a little rain which is important for mango tea and coffee plant has the name of mango shower is used