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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 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 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 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 Eastern Himalayan subalpine conifer forests is a temperate coniferous forests ecoregion which is found in the middle and upper elevations of the eastern Middle Himalayas, in western Nepal, Bhutan, northern Indian states including Arunachal Pradesh and Sikkim and adjacent Myanmar and China.
The British explorer John Wood, writing in 1838, described Bam-i-Duniah (Roof of the World) as a "native expression" (presumably Wakhi), [1] and it was generally used for the Pamirs in Victorian times: In 1876, another British traveler, Sir Thomas Edward Gordon, employed it as the title of a book [2] and wrote in Chapter IX:
The Nicobar Islands consist of 22 islands, of which 13 are inhabited. The islands extend about 260 km from north and south, and form three groups. The northern group is composed of Car Nicobar, the northernmost island, and Batti Malv. The central group includes Nancowry, Katchal, Kamorta, Teressa, Chowra, Tillangchong, and several smaller islets.
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.