Published June 1, 2022 | Version v1

Insolation and CO2 impacts on the spatial differences of the MIS-9 and MIS-11 climate between monsoonal China and central Asia

Description

The model outputs we use are those performed in Yin & Berger (2012) where the climate of the last nine interglacials were simulated with the LOVECLIM model. The model outputs for MIS-11 and MIS-9 are used here to study the climate conditions in mid and eastern Asia.

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