Tibetic languages

The Tibetic languages form a well-defined group of languages descended from Old Tibetan (7th to 9th centuries). According to Tournadre (2014), there are 50 languages, which split into over 200 dialects or could be grouped into 8 dialect continua. These languages are spoken in the Tibetan Plateau and in the Himalayas in Gilgit-Baltistan, Aksai Chin, Ladakh, Nepal, Himachal Pradesh, Uttarakhand, and Bhutan. Classical Tibetan is the major literary language, particularly for its use in Buddhist literature. Tibetan languages are spoken by some 6 million people, not all of whom are Tibetans. With the worldwide spread of Tibetan Buddhism, the Tibetan language has spread into the western world and can be found in many Buddhist publications and prayer materials; with some western students learning the language for translation of Tibetan texts. Outside Lhasa itself, Lhasa Tibetan is spoken by approximately 200,000 exile speakers who have moved from modern-day Tibet to India and other countries. Tibetan is also spoken by groups of ethnic minorities in Tibet who have lived in close proximity to Tibetans for centuries, but nevertheless retain their own languages and cultures. Although some of the Qiang peoples of Kham are classified by China as ethnic Tibetans (see Gyalrongic languages; Gyalrong people are identified as 'Tibetan' in China), the Qiangic languages are not Tibetan, but rather form their own branch of the Tibeto-Burman language family. Classical Tibetan was not a tonal language, but many varieties such as Central and Khams Tibetan have developed tone registers. Amdo and Ladakhi-Balti are without tone. Tibetan morphology can generally be described as agglutinative. Marius Zemp (2018) hypothesizes that Tibetan originated as a pidgin with the West Himalayish language Zhangzhung as its superstratum, and Rgyalrongic as its substratum (both languages are part of the broader Sino-Tibetan family). Similarly, Tamangic also has a West Himalayish superstratum, but its substratum is derived from a different Sino-Tibetan branch.

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Light-absorbing impurities enhance glacier albedo reduction in the southeastern Tibetan plateau

Julia Schmale, Wei Yang, Xinyang Li

Light‐absorbing impurities (LAIs) in snow of the southeastern Tibetan Plateau (TP) and their climatic impacts are of interest not only because this region borders areas affected by the South Asian atmospheric brown clouds but also because the seasonal snow ...

2017

Synchronising EDML and NorthGRIP ice cores using δ18O of atmospheric oxygen (δ18Oatm) and CH4 measurements over MIS5 (80-123 kyr)

Jérôme Chappellaz

An ice core air content record that was recovered from the refrozen-recrystallization ice formation zone in the Dasuopu Glacier was investigated in this work, which showed that the air content in ice performed significant fluctuations both in the seasonal ...

Elsevier BV2010

Ladakh

Ladakh (ləˈdɑːk) is a region administered by India as a union territory and constitutes an eastern portion of the larger Kashmir region that has been the subject of a dispute between India and Pakistan since 1947 and India and China since 1959. Ladakh is bordered by the Tibet Autonomous Region to the east, the Indian state of Himachal Pradesh to the south, both the Indian-administered union territory of Jammu and Kashmir and the Pakistan-administered Gilgit-Baltistan to the west, and the southwest corner of Xinjiang across the Karakoram Pass in the far north.

Tibetan people

The Tibetan people (; ) are an East Asian ethnic group native to Tibet. Their current population is estimated to be around 6.7 million. In addition to the majority living in Tibet Autonomous Region of China, significant numbers of Tibetans live in the Chinese provinces of Gansu, Qinghai, Sichuan, and Yunnan, as well as in India, Nepal, and Bhutan. The Tibetic languages belong to the Tibeto-Burman language group. The traditional or mythological explanation of the Tibetan people's origin is that they are the descendants of the human Pha Trelgen Changchup Sempa and rock ogress Ma Drag Sinmo.

Tibetan Plateau

The Tibetan Plateau (, also known as the Qinghai–Tibet Plateau or the Qing–Zang Plateau () or as the Himalayan Plateau in India, is a vast elevated plateau located at the intersection of Central, South and East Asia covering most of the Tibet Autonomous Region, most of Qinghai, western half of Sichuan, Southern Gansu provinces in Western China, southern Xinjiang, Bhutan, the Indian regions of Ladakh and Lahaul and Spiti (Himachal Pradesh) as well as Gilgit-Baltistan in Pakistan, northwestern Nepal, eastern