Based on the geological evidence that the northern TP (NTP) had an uplift of finite magnitude since the Miocene and the major Asian inland deserts formed in the early Pliocene, Dr. LIU Xiaodong and Dr. SUN Hui, from the Institute of Earth Environment of Chinese Academy of Sciences, and co-authors revealed the influence of uplift of the NTP and Asian inland deserts information on regional climate and environment by using a high resolution regional climate model through paleo-climate modeling of lowering topography of the NTP and removing Asian inland deserts.
The analysis on the boreal summer intraseasonal oscillation over the Tibetan Plateau shows that the dominant intraseasonal signal was the quasi-biweekly oscillation, which could be detected in circulation, precipitation and diabatic heating fields.
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