G. Ramstein et al., EFFECT OF OROGENY, PLATE MOTION AND LAND SEA DISTRIBUTION ON EURASIANCLIMATE-CHANGE OVER THE PAST 30 MILLION YEARS, Nature, 386(6627), 1997, pp. 788-795
The Eurasian climates of today, 10 million and 30 million years ago ar
e simulated using an atmospheric general circulation model that incorp
orates realistic continental geography and epicontinental sea distribu
tions. The resulting climates compare well with various palaeoclimate
records. The retreat of the Paratethys-an epicontinental sea-shifts th
e central Asian climate from temperate to continental conditions, and
plays as important a role as uplift, of the Himalayan/Tibetan plateau
in driving the Asian monsoon changes.