Fig. 3From: Evolution and variability of the Asian monsoon and its potential linkage with uplift of the Himalaya and Tibetan PlateauChange in position and intensity of the Siberian High with the uplift of the TP. The figure is based on an AGCM experiment by Liu and Yin (2002). Winter average SLP distributions for a no mountain and b full mountain experiments are shown (unit: hPa). Modified from Liu and Yin (2002)Back to article page