Climate of India
The principal area of the area of India ( *indian visa online application form) is in the sub equatorial region. The primary characteristic of this region is tropical monsoons. Summer monsoon from the Indian Ocean provides rains to India. They heighten at the begining of June on the west coast and in mid-June on the east coast. Whenever passing over the Arabian Sea and the Bay of Bengal, the monsoons are saturating with moisture and also move in a northwest way.
Rising above the Western Ghats and Assam Mountains, monsoons move at a pace of 5-7 m/s, leading to heavy rain. Thunder or wind storms fall on the hills of the hills in June. However later they calm down, and through the period from late September to mid-October rain falls typically, stop. From November to March, the dry northeastern monsoon blows through the land side. It makes the climate cold and sun-drenched.
Based on data on thermal conditions, precipitation, and also winds, we can separate the calendar year in 3 main climatic seasons.
In November – February, if the northeastern monsoon dominates, it is cold and sunshiny. In March, the temperature slowly goes up.The dry season lasts from the end of March to June. By the end of June, the humidity rises. And also the weather condition of Indian plains becomes rainy.The time from July to mid-September will be the summer monsoon time. It is a time of wet tropical climate. The south-westerly winds blend with high temperatures.October is a transitional time. The air humidity is high due to evaporation through the surface of the fields. However the rains stop.
There are actually differences in temperature as well as weather in various areas of India. The nation covers a big location, and every location has yet another terrain. Hence, in the Thardesert, the annual precipitation does not go over 100 mm. At Cherapun jistation in the Khashi Mountains, it is around 10 770 mm of rainfall per year. It is among the wettest spots on Earth.
The monsoon climate is characteristic of the coast of the Arabian Sea. The very coldest period of time is from December to February. Simultaneously, there is fewer rain. The hottest time is from May to June. Yet even great heat are tolerated very easily since air is dried, relative humidity, even in the morning, doesn’t surpass 60%. Winds raise clouds of dust and turn the horizon a dirty yellow.
The onset of the monsoon in June commences with the greater wind and cloud cover. The time can last until September. During most days of the month, it rains frequently and lightly. The monthly rainfall in the wettest month – July exceeds 600 mm. Cloudy weather decreases the temperature by 3-5 degrees.
In the mountains of the Himalayas, the climate will depend on the height above sea level. Soat altitudes through 1500 to 2300 meters, from December to February, the average minimum temp is from 0 to -3C (25 to 32F), and the average maximum temperature is +4 to +8C (40 to 45F).
The hottest time of the year lasts from June to August: the average minimum temperatureis +14 to +18C (55 to 65F), the average optimum temperatureis +29 to +30C (84 to 86F). Summer time monsoon does not appear here. The smallest amount of rainfall is from September to November (25-35 mm per month), the highest in March (about 100 mm). As you will see, the climate of India varies depending on the location, its distance from the Ocean, as well as its altitude. We could not compare Himalayan climate to other portions of India. These hills are really high and also have a unique climate.