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Summer precipitation and black carbon emission characteristics. a The spatial pattern of summer precipitation using the Climatic Research Unit (CRU) dataset overlain with summer 500 hPa wind fields for the period 2001–2016, using the ERA-Interim dataset over the Tibetan plateau (TP) and South Asia (denoted by red polygon). NTP and STP delineate the northern and southern Tibetan plateau boundaries.

South Asian black carbon causes glacier loss on Tibetan Plateau

Tibetan Plateau

Tibetan plateau rose later than we thought

Data mining finds more than expected beneath Andean Plateau

Strength of tectonic plates may explain shape of the Tibetan Plateau

Rapid uplift of Southern Tibet

Research sheds new light on high-altitude settlement in Tibet

Satellites peer into rock 50 miles beneath Tibetan Plateau

Science Investigates Lithosphere of the Central Iranian Plateau

Snail shells show high-rise plateau is much lower than it used...

Snails Tell of the Rise and Fall of the Tibetan Plateau

Tibetan Plateau was larger than previously thought, geologists say

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