A continuous simulation of Holocene effective moisture change in East and Central Asia

Based on a transient climate evolution model, a lake energy balance model and a lake water balance model, the effective moisture change during the Holocene in East and Central Asia is continuously and quantitatively traced by constructing a virtual lake system. Furthermore, according to the changes of precipitation, runoff, evaporation, solar radiation and atmosphere radiation, researchers completed a sensitivity study of effective moisture to climate change.