A. Zhisheng et al., Evolution of Asian monsoons and phased uplift of the Himalayan Tibetan plateau since Late Miocene times, NATURE, 411(6833), 2001, pp. 62-66
The climates of Asia are affected significantly by the extent and height of
the Himalayan mountains and the Tibetan plateau(1-4). Uplift of this regio
n began about 50 Myr ago, and further significant increases in altitude of
the Tibetan plateau are thought to have occurred about 10-8 Myr ago(4,5), o
r more recently. However, the climatic consequences of this uplift remain u
nclear. Here we use records of aeolian sediments from China(6,7) and marine
sediments from the Indian(8-10) and North Pacific oceans(11) to identify t
hree stages of evolution of Asian climates: first, enhanced aridity in the
Asian interior and onset of the Indian and east Asian monsoons, about 9-8 M
yr ago; next, continued intensification of the east Asian summer and winter
monsoons, together with increased dust transport to the North Pacirc Ocean
(11), about 3.6-2.6 Myr ago; and last, increased variability and possible w
eakening of the Indian and east Asian summer monsoons and continued strengt
hening of the east Asian winter monsoon since about 2.6 Myr ago. The result
s of a numerical climate-model experiment, using idealized stepwise increas
es of mountain-plateau elevation, support the argument that the stages in e
volution of Asian monsoons are linked to phases of Himalaya-Tibetan plateau
uplift and to Northern Hemisphere glaciation.