Xinyu Wen

TL;DR: In this article, the authors examined the evolution of the climate and precipitation δ18O for the last 21,000 years in models and observations, and proposed an interpretation of the Chinese ǫ18O record that reconciles its representativeness of the East Asia Summer Monsoon (EASM) and its driving mechanism of upstream depletion.

TL;DR: A series of transient Coupled General Circulation Model simulations forced by changes in greenhouse gasses, orbital forcing, the meltwater discharge and the ice-sheet history throughout the past 21,000 years show an orbitally induced strengthening of ENSO during the Holocene epoch.

TL;DR: Using a set of long-term transient simulations of the climate evolution of the last 21,000 years, it is shown that the EASM and EAWM are positively correlated on the orbital timescale in response to the precessional forcing, but are anti-correlated on millennial timescales in responseto North Atlantic melt water forcing.

TL;DR: In this article, a multi-model set of atmospheric simulations forced by historical sea surface temperature (SST) or SSTs plus Greenhouse gases and aerosol forcing agents for the period of 1950-1999 is studied to identify and understand which components of the Asian-Australian monsoon (A-AM) variability are forced and reproducible.

TL;DR: In this paper, the authors present results from 1 year process analysis and a number of sensitivity simulations using the Community Multiscale Air Quality (CMAQ) modeling system aimed to understand the formation mechanisms of O3 and PM2.5, their impacts on global environment and implications for pollution control policies.