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Indian rhinoceros in the Terai. Above the alluvial plain lies the Terai strip, a seasonally marshy zone of sand and clay soils. The Terai has higher rainfall than the plains, and the downward-rushing rivers of the Himalaya slow down and spread out in the flatter Terai zone, depositing fertile silt during the monsoon season and receding in the dry season.
The climate of Asia is dry across its southwestern region. Some of the largest daily temperature ranges on Earth occur in the western part of Asia . The monsoon circulation dominates across the southern and eastern regions, due to the Himalayas forcing the formation of a thermal low which draws in moisture during the summer.
The climate of the Eastern Himalayas is of a tropical montane ecosystem. The tropical rainforest climate is hot and wet all year round, with no dry season in the foothills in Köppen Climate Classification System , and chilly winters mainly on higher elevations. The hot season commences around the middle of April reaching its maximum ...
The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents.
The subtropical climate zone from 1,000 to 2,000 meters (3,300 to 6,600 ft) occupies 22% of Nepal's land area and is the most prevalent climate of the Middle Hills above river valleys. It experiences frost up to 53 days per year, however, this varies greatly with elevation, proximity to high mountains and terrain either draining or ponding cold ...
The Third Pole, also known as the Hindu Kush-Karakoram-Himalayan system (HKKH), is a mountainous region located in the west and south of the Tibetan Plateau.Part of High-Mountain Asia, it spreads over an area of more than 4.2 million square kilometres (1.6 million square miles) across nine countries, i.e. Afghanistan, Bangladesh, Bhutan, China, India, Myanmar, Nepal, Pakistan and Tajikistan ...
The Transhimalays generally have a cold, arid montane climate. For example, the Spiti region of Himachal Pradesh , India, has an annual rainfall of about 170 mm. [ 2 ] However, studies in Mustang District , Nepal, indicate that climate change is warming the Transhimalayas at a rate of about 0.13 degrees a year.
The Himalayas have three biogeographical provinces – Northwest Himalayas, West Himalayas, Central Himalayas and East Himalayas, which together constitute about 6.4% of the country's area. [2] [13] Tropical rainforests predominate in the Eastern Himalayas while dense subtropical and alpine forests are typical in the Central and Western Himalayas.