Glacial geology
; Wetting
; Associated mechanism
; Global
; Last Glacial Maximum
; Multi-Model Simulations
; Paleoclimate modelling
; Pleistocene
; Potential evapotranspiration
; Southeastern Africa
; Moisture
; aridity
; climate modeling
; global climate
; Last Glacial Maximum
; moisture
; paleoclimate
; Pleistocene
; potential evapotranspiration
; precipitation (climatology)
; Africa
; Andes
; Australia
; Brazil
; Central America
; Iberian Peninsula
; North America
; South America
; Southeast Asia
Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China; CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, 100101, China; Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science & Technology, Nanjing, 210044, China; University of Chinese Academy of Sciences, Beijing, 100049, China
Recommended Citation:
Liu S.,Jiang D.,Lang X.. A multi-model analysis of moisture changes during the last glacial maximum[J]. Quaternary Science Reviews,2018-01-01,191