
The climate of India is mainly tropical because _____________.
(A) Of the location of Himalayas in its north
(B) Major part of India lies within the tropics
(C) Of the overpowering influence of Indian Ocean
(D) Of the season influence of jet streams
Answer
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Hint: It is a mountain range in Asia isolating the fields of the Indian subcontinent from the Tibetan Plateau. The range has a significant number of Earth's highest pinnacles, including the most popular, Mount Everest, at the outskirts of Nepal and China.
Complete step-by-step solution:
The atmosphere of India is principally tropical in light of the area of the Himalayas in its North. India is home to a remarkable assortment of climatic districts, going from tropical in the south to temperate and alpine in the Himalayan north, where raised areas get supported winter snowfall. The country's atmosphere is affected by the Himalayas and the Thar Desert.
A tropical rainy atmosphere administers districts encountering industrious warm or high temperatures, which ordinarily don't fall under\[18^\circ {\text{C}}\] ($64^\circ {\text{F}}$).
The most humid is the tropical wet atmosphere—otherwise called tropical rainstorm atmosphere—that covers a portion of southwestern swamps adjoining the Malabar Coast, the Western Ghats, and southern Assam. India's two island domains, Lakshadweep and the Andaman and Nicobar Islands are likewise dependent upon this atmosphere. Portrayed by moderate to high all year temperatures, even in the lower regions, its precipitation is occasional however weighty—commonly over 2,000 mm (79 in) every year. Most precipitation happens between May and November; this dampness is sufficient to support lavish woods and other vegetation for the remainder of the principally dry year. December to March are the driest months when days with precipitation are uncommon. The substantial storm downpours are liable for the remarkable biodiversity of tropical wet backwoods in pieces of these areas.
In India, a tropical wet and dry atmosphere is more normal. Perceptibly drier than regions with a tropical storm atmosphere, it beats the greater part of inland peninsular India aside from a semi bone-dry downpour shadow east of the Western Ghats. Winter and late-spring are long and dry periods with temperatures averaging over \[18^\circ {\text{C}}\] ($64^\circ {\text{F}}$). Summer is blistering; temperatures in low-lying zones may surpass $50^\circ {\text{C}}$ ($122^\circ {\text{F}}$) during May, prompting heat waves that can each murder many Indians.
Thus, option (A) is correct.
Note: The rainy season endures from June to September; yearly precipitation midpoints between 750–1,500 mm (30–59 in) across the locale. When the dry upper east storm starts in September, most precipitation in India falls on Tamil Nadu, leaving different states similarly dry.
Complete step-by-step solution:
The atmosphere of India is principally tropical in light of the area of the Himalayas in its North. India is home to a remarkable assortment of climatic districts, going from tropical in the south to temperate and alpine in the Himalayan north, where raised areas get supported winter snowfall. The country's atmosphere is affected by the Himalayas and the Thar Desert.
A tropical rainy atmosphere administers districts encountering industrious warm or high temperatures, which ordinarily don't fall under\[18^\circ {\text{C}}\] ($64^\circ {\text{F}}$).
The most humid is the tropical wet atmosphere—otherwise called tropical rainstorm atmosphere—that covers a portion of southwestern swamps adjoining the Malabar Coast, the Western Ghats, and southern Assam. India's two island domains, Lakshadweep and the Andaman and Nicobar Islands are likewise dependent upon this atmosphere. Portrayed by moderate to high all year temperatures, even in the lower regions, its precipitation is occasional however weighty—commonly over 2,000 mm (79 in) every year. Most precipitation happens between May and November; this dampness is sufficient to support lavish woods and other vegetation for the remainder of the principally dry year. December to March are the driest months when days with precipitation are uncommon. The substantial storm downpours are liable for the remarkable biodiversity of tropical wet backwoods in pieces of these areas.
In India, a tropical wet and dry atmosphere is more normal. Perceptibly drier than regions with a tropical storm atmosphere, it beats the greater part of inland peninsular India aside from a semi bone-dry downpour shadow east of the Western Ghats. Winter and late-spring are long and dry periods with temperatures averaging over \[18^\circ {\text{C}}\] ($64^\circ {\text{F}}$). Summer is blistering; temperatures in low-lying zones may surpass $50^\circ {\text{C}}$ ($122^\circ {\text{F}}$) during May, prompting heat waves that can each murder many Indians.
Thus, option (A) is correct.
Note: The rainy season endures from June to September; yearly precipitation midpoints between 750–1,500 mm (30–59 in) across the locale. When the dry upper east storm starts in September, most precipitation in India falls on Tamil Nadu, leaving different states similarly dry.
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